Chapter 5 Rights | class 11th | Political Theory NCERT Important MCQs for Political Science

MCQ Questions for Class 11 Political Science: Ch 5 Rights

1. In a state, it is also the duty of the citizens to

(a) Ensure sustainable development.

(b) Protect the atmosphere.

(c) Pollute air and water.

(d) Live in peace.

► (a) Ensure sustainable development.

2. A Bill of Rights is enshrined in the

(a) Preamble of the UNO.

(b) Constitution of many countries.

(c) Human rights of UNESCO.

(d) Government documents of few countries.

► (b) Constitution of many countries.

3. Natural Rights are those which are given to us by:

(a) Constitution

(b) Parliament

(c) God or Nature

(d) King

► (c) God or Nature

4. Human rights, traditionally are divided into

(a) Political and economic rights.

(b) Political and social rights on one hand and cultural rights on the other.

(c) Civil and political rights.

(d) Civil and political rights on one hand and the right to development on the other.

► (c) Civil and political rights.

5. Who said “Rights are those conditions of social life without which no man can seek to be himself at his best ?”

(a) Austin

(b) Wilde

(c) Green

(d) Laski

► (d) Laski

6. The political right is the right to

(a) Shelter.

(b) Sustainable development.

(c) Livelihood.

(d) Form political parties.

► (d) Form political parties.

7. Civil liberties and political rights form the basis of a

(a) Democratic government.

(b) Monarchical rule.

(c) Totalitarian government.

(d) Dictator rule.

► (a) Democratic government.

8. Right to franchise is a

(a) Customary rights.

(b) Political right.

(c) Moral rights.

(d) Cultural right.

► (b) Political right.

9. The natural right that was not advocated by the political theorists of 17th and 18th centuries was right to

(a) Life.

(b) Liberty.

(c) Information.

(d) Property.

► (c) Information.

10. Civil Rights are given to the Individual by:

(a) Nature

(b) God

(c) The state

(d) The people

► (c) The state

11. Freedom of expression is important for

(a) A state.

(b) A democratic government.

(c) Communist society.

(d) An individual livelihood.

► (b) A democratic government.

12. According to the German philosopher Immanuel Kant, human beings unlike other objects are:

(a) Useful.

(b) Valuable.

(c) Selfish.

(d) Independent.

► (b) Valuable.

13. What is the force behind Legal Rights ?

(a) Force of public opinion

(b) Force of morality

(c) Force of law

(d) Force of nature

► (c) Force of law

14. The provision to abolish untouchability is reflected in the Indian constitution under

(a) Article 14.

(b) Article 15.

(c) Article 16.

(d) Article 17.

► (d) Article 17.

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Chapter 4 Social Justice | class 11th | Political Theory NCERT Important MCQs for Political Science

MCQ Questions for Class 11 Political Science: Ch 4 Social Justice

1. The famous quote “In a country well governed, poverty is something to be ashamed of. In a country badly governed, wealth is something to be ashamed of.” is given by

(a) J.S.Mill.

(b) Plato.

(c) Aristotle.

(d) Confucius.

► (d) Confucius.

2. Choose the type of stages of equality advocated by John Rawls.

(a) Two

(b) Three

(c) Four

(d) Five

► (b) Three

3. Identify stage of equality which rejects formal institutions of inequalities.

(a) Liberal Equality

(b) Natural Liberty

(c) Democratic Equality

(d) Economic Equality

► (b) Natural Liberty

4. Which one of the following in not the fundamental postulate of Justice?

(a) Truth

(b) Equality before law

(c) Freedom

(d) Property

► (d) Property

5. An international institution that work for justice is

(a) International Court of justice.

(b) Civil services.

(c) IMF.

(d) WTO.

► (a) International Court of justice.

6. Justice is administered by:

(a) Executive

(b) Judiciary

(c) Legislature

(d) Political parties

► (b) Judiciary

7. The essential principles of modern justice is that

(a) Judges should be part of executive.

(b) Judges should be under the control of the Head of the State.

(c) There should be independence of judiciary.

(d) Judges should be under the control of the electorate.

► (c) There should be independence of judiciary.

8. Free market is a product of

(a) Socialism.

(b) Feminism.

(c) Neo-liberalism.

(d) Patriarchy.

► (c) Neo-liberalism.

9. People get proper justice in:

(a) Dictatorship

(b) Totalitarian state

(c) Monarchy

(d) Democracy

► (d) Democracy

10. State’s failure to provide individuals with basic necessities of life such as; food and housing is an example of

(a) Political Injustice

(b) Economic Injustice

(c) Social discrimination

(d) Gender inequality

► (b) Economic Injustice

11. Choose the ministry that is entrusted with the welfare, social justice and empowerment of disadvantaged and marginalized sections of the society in India.

(a) Ministry of welfare

(b) Ministry of social justice and empowerment

(c) Ministry of social defense

(d) Ministry of Education

► (b) Ministry of social justice and empowerment

12. Our political rights and participation are insured only when our

(a) Social needs are being taken care of.

(b) Basic needs

(c) Cultural needs

(d) Security needs

► (b) Basic needs

13. The term “justice’ is derived from the word ‘Jus’ which is a word from:

(a) Latin language

(b) Greek language

(c) English language

(d) French language

► (a) Latin language

14. Justice is essentially a:

(a) Legal concept

(b) Moral concept

(c) Social concept

(d) All of the above

► (d) All of the above

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Chapter 14 सुमित्रानंदन पंत | class 11th | Ncert solution for Hindi Antra

NCERT Solutions for Class 11th: पाठ 14 -सुमित्रानंदन पंत

प्रश्न-अभ्यास

1. संध्या के समय प्रकृति में क्या-क्या परिवर्तन होते हैं, कविता के आधार पर लिखिए।

उत्तर

संध्या के समय सूर्य का प्रकाश लाल आभा लिए हो जाता है और झरनों से बहनेवाले जल का वर्ण स्वर्णिम हो जाता है। ये किरणें गंगाजल को स्वर्णिम करती हुई उसके किनारे की रेत पर धूपछाँही बना देती है। जैसे-जैसे सूर्य डूबता जाता है वैसे-वैसे प्राकृतिक परिवेश बदलता रहता है। तांबाई से स्वर्णिम, फिर सुरमई और सूर्य के डूबते ही अँधेरा छा जाता है।

2. पंत जी ने नदी के तट का जो वर्णन किया है, उसे अपने शब्दों में लिखिए।

उत्तर

नदी के तट पर ध्यान में मगन वृद्ध औरतें ऐसे प्रतीत हो रही हैं, मानो शिकार करने के लिए नदी किनारे खड़े बगुलें हों। पंत जी ने कविता में वृद्ध औरतों की बहुत सुंदर उपमा दी है। उनके दुख को भी बहुत सुंदर ढंग से प्रस्तुत किया है। नदी की मंथर धारा को वृद्ध औरतों के मन में बहने वाले दुख के समान बताया गया है। इस तरह से वृद्ध औरतें और बगुले दोनों ही नदी किनारे में मिलते हैं। उनके सफेद रंग के कारण कवि ने बहुत सुंदर उपमा देकर दोनों को एक कर दिया है।

3. बस्ती के छोटे से गाँव के अवसाद को किन-किन उपकरणों द्वारा अभिव्यक्त किया गया है?

उत्तर

शाम होते ही कृषक, उनकी गाएँ तथा पक्षी घर की और लौट पड़ते हैं।

4. लाला के मन में उठनेवाली दुविधा को अपने शब्दों में लिखिए।

उत्तर

लाला अपनी छोटी एवं संकुचित दुकान को देखकर वह स्वयं को दयनीय, दुखी और अपमानित अनुभव करता है। जीवन-भर अपनी दुकान की गद्दी पर बैठा हुआ उसे ऐसा लगता है जैसे किसी निर्जीव और बेकार अनाज का ढेर हो। वह सोचता था कि शहर में रहने वाले बनियों के समान वह उठ क्यों नहीं पाता? वह थोड़ी-सी आय के लिए बात-बात में झूठ बोलता है तथा अपने ही वर्ग के साथ प्रतिस्पर्धा के कारण अपने जीवन को तबाह कर रहा है।

5. सामाजिक समानता की छवि की कल्पना किस तरह अभिव्यक्त हुई है?

उत्तर

सामाजिक समानता की छवि की कल्पना इस प्रकार अभिव्यक्त हुई है-
• कर्म तथा गुण के समान ही सकल आय-व्यय का वितरण होना चाहिए।
• सामूहिक जीवन का निर्माण किया जाए।
• सब मिलकर नए संसार का निर्माण करें।
• सब मिलकर सभी प्रकार की सुख-सुविधाओं का भोग करें।
• समाज को धन का उत्तराधिकारी बनाया जाए।
• सभी व्याप्त वस्त्र, भोजन तथा आवास के अधिकारी हों।
• श्रम सबमें समान रूप से बँटें।

6. ‘कर्म और गुण के समान..”हो वितरण’ पंक्ति के माध्यम से कवि कैसे समाज की ओर संकेत कर रहा है?

उत्तर

इस पंक्ति में कवि ऐसे समाज की कल्पना कर रहा है, जहाँ का वितरण मनुष्य के कर्म और गुणों के आधार पर होना चाहिए। ऐसे में प्रत्येक मनुष्य को उसके गुणों और कार्य करने की क्षमता के आधार पर कार्य मिलेगा, इससे आय का सही प्रकार से बँटवारा हो सकेगा। ये समाजवाद के गुण हैं, जिसमें किसी एक वर्ग का आय-व्यय पर अधिकार नहीं होता है। सबको समान अधिकार प्राप्त होते हैं।

7. निम्नलिखित पंक्तियों का काव्य-सौंदर्य स्पष्ट कीजिए-
(क) तट पर बगुलों-सी वृद्धाएँ
विधवाएँ जप ध्यान में मगन, मंथर धारा में बहता
जिनका अदृश्य, गति अंतर-रोदन!

उत्तर

प्रस्तुत पंक्तियां कविवर सुमित्रानंदन की कविता ‘संध्या के बाद’ से ली गयी हैं जिसमें कवि ने बहुत ही सुंदर और मार्मिक रूप में प्रकृति का चित्रण किया है। कवि ने सांध्यकालीन वातावरण में नदी के तट पर बैठी बूढ़ी स्त्रियों और विधवाओं की दशा का वर्णन किया है जो ऐसे ध्यान मग्न होकर परमात्मा का नाम जप रही हैं जैसे बगुले ध्यानपूर्वक पानी देख रहे हों| उनके हृदय में दुख की मंथन धारा बह रही है। इस काव्यांश की प्रत्येक पंक्ति में काव्य सौंदर्य अद्भुत जान पड़ता है। पहली पंक्ति में ‘बगुलों-सी वृद्धाएँ’ में उपमा अलंकार है। कवि ने तत्सम शब्दों का प्रयोग करके अपनी बात को बहुत सुंदर रूप में चित्रित किया है।

8. आशय स्पष्ट कीजिए-

(क) ताम्रपर्ण, पीपल से, शतमुख/ झरते चंचल स्वर्णिम निर्झर!

उत्तर

पीपल के सूखे पत्ते ऐसे लग रहे हैं मानो ताँबे धातु से बने हों। वह पेड़ से गिरते हुए ऐसे लग रहे हैं मानो सैंकड़ों मुँह वाले झरनों से सुनहरे रंग की धाराएँ गिर रही हों।

(ख) दीप शिखा-सा ज्वलित कलश/नभ में उठकर करता नीराजन!

उत्तर

मंदिर के शिखर पर लगा कलश सूर्य की रोशनी के प्रभाव से दीपक की जलती लौ के समान लग रहा है। ऐसा लग रहा है मानो संध्या आरती में वह भी लोगों के समान आरती कर रहा है।

(ग) सोन खगों की पाँति/आर्द्र ध्वनि से नीरव नभ करती मुखरित!

उत्तर

आकाश में व्याप्त खग नामक पक्षी पंक्ति में उड़ रहे हैं। उनकी गुंजार शांत आकाश को गुंजार से भर देती है।

(घ) मन से कढ़ अवसाद श्राति / आँखों के आगे बुनती जाला!

उत्तर

मनुष्य के मन में व्याप्त दुख तथा कष्ट उसकी आँखों में यादों के रूप में उभर आते हैं।

(ङ) क्षीण ज्योति ने चुपके ज्यों / गोपन मन को दे दी हो भाषा!

उत्तर

घरों में विद्यमान दीपक जल उठे हैं। इस अंधकार में उसकी रोशनी अवश्य कमज़ोर है। उस कमज़ोर ज्योति ने लगता है गोपों के मन को एक आशा दे दी है।

(च) बिना आय की क्लाति बन रही/ उसके जीवन की परिभाषा!

उत्तर

गाँव में लोगों के पास आय का साधन विद्यमान नहीं है। अतः उसके जीवन में बहुत दुख विद्यमान हैं। ऐसा लगता है कि मानो यह अभाव उसकी कहानी बनकर रह जाएँगे।

(छ) व्यक्ति नहीं, जग की परिपाटी/ दोषी जन के दुःख क्लेश की।

उत्तर

दोष से युक्त सामाजिक व्यवस्था ही मनुष्य के दुख का कारण है। धन के असमान बँटवारे के कारण ही समाज में अंतर व्याप्त है।

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Chapter 3 Matrices | class 12th | quick revision notes maths

Class 12 Maths Notes Chapter 3 Matrices

Matrix: A matrix is an ordered rectangular array of numbers or functions. The numbers or functions are called the elements or the entries of the matrix.

Order of a Matrix: If a matrix has m rows and n columns, then its order is written as m × n. If a matrix has order m × n, then it has mn elements.

In general, am×n matrix has the following rectangular array:
Matrices Class 12 Notes Maths Chapter 3 1
Note: We shall consider only those matrices, whose elements are real numbers or functions taking real values.

Types of Matrices
Column Matrix: A matrix which has only one column, is called a column matrix.
e.g. \(\left[ \begin{matrix} 1 \\ 0 \\ -5 \end{matrix} \right]\)
In general, A = [aij]m×1 is a column matrix of order m × 1.

Row Matrix: A matrix which has only one row, is called a row matrix,
e.g. \(\left[ \begin{matrix} 1 & 5 & 9 \end{matrix} \right]\)
In general, A = [aij]1×n is a row matrix of order 1 x n

Square Matrix: A matrix which has equal number of rows and columns, is called a square matrix
e.g. \(\begin{bmatrix} 3 & -1 \\ 5 & 2 \end{bmatrix}\)
In general, A = [aij]m x m is a square matrix of order m.
Note: If A = [aij] is a square matrix of order n, then elements a11, a22, a33,…, ann is said to constitute the diagonal of the matrix A.

Diagonal Matrix: A square matrix whose all the elements except the diagonal elements are zeroes, is called a diagonal matrix,
e.g. \(\left[ \begin{matrix} 3 & 0 & 0 \\ 0 & -3 & 0 \\ 0 & 0 & -8 \end{matrix} \right]\)
In general, A = [aij]m×m is a diagonal matrix, if aij = 0, when i ≠ j.

Scalar Matrix: A diagonal matrix whose all diagonal elements are same (non-zero), is called a scalar matrix,
e.g. \(\left[ \begin{matrix} 2 & 0 & 0 \\ 0 & 2 & 0 \\ 0 & 0 & 2 \end{matrix} \right]\)
In general, A = [aij]n×n is a scalar matrix, if aij = 0, when i ≠ j, aij = k (constant), when i = j.
Note: A scalar matrix is a diagonal matrix but a diagonal matrix may or may not be a scalar matrix.

Unit or Identity Matrix: A diagonal matrix in which all diagonal elements are ‘1’ and all non-diagonal elements are zero, is called an identity matrix. It is denoted by I.
e.g. \(\left[ \begin{matrix} 1 & 0 & 0 \\ 0 & 1 & 0 \\ 0 & 0 & 1 \end{matrix} \right]\)
In general, A = [aij]n×n is an identity matrix, if aij = 1, when i = j and aij = 0, when i ≠ j.

Zero or Null Matrix: A matrix is said to be a zero or null matrix, if its all elements are zer0
e.g. \(\begin{bmatrix} 0 & 0 \\ 0 & 0 \end{bmatrix}\)

Equality of Matrices: Two matrices A and B are said to be equal, if
(i) order of A and B are same.
(ii) corresponding elements of A and B are same i.e. aij = bij, ∀ i and j.
e.g. \(\begin{bmatrix} 2 & 1 \\ 0 & 3 \end{bmatrix}\) and \(\begin{bmatrix} 2 & 1 \\ 0 & 3 \end{bmatrix}\) are equal matrices, but \(\begin{bmatrix} 3 & 2 \\ 0 & 1 \end{bmatrix}\) and \(\begin{bmatrix} 2 & 3 \\ 0 & 1 \end{bmatrix}\) are not equal matrices.

Operations on Matrices
Between two or more than two matrices, the following operations are defined below:
Addition and Subtraction of Matrices: Addition and subtraction of two matrices are defined in an order of both the matrices are same.
Addition of Matrix
If A = [aij]m×n and B = [yij]m×n, then A + B = [aij +bij]m×n, 1 ≤ i ≤ m, 1 ≤ j ≤ n
Subtraction of Matrix
If A = [aij]m×n and B = [bij]m×n, then A – B = [aij – bij]m×n, 1 ≤ i ≤ m, 1 ≤ j ≤ n

Properties of Addition of Matrices
(a) Commutative If A = [aij] and B = [bij] are matrices of the same order say m x n then A + B = B + A,
(b) Associative for any three matrices A = [aij], B = [bij], C = [cij] of the same order say m x n, A + (B + C) = (A + B) + C.
(c) Existence of additive identity Let A = [aij] be amxn matrix and O be amxn zero matrix, then A + O = O + A = A. In other words, O is the additive identity for matrix addition.
(d) Existence of additive inverse Let A = [aij]m×n be any matrix, then we have another matrix as -A = [-aij]m×n such that A + (-A) = (-A + A) = O. So, matrix (-A) is called additive inverse of A or negative of A.

Note
(i) If A and B are not of the same order, then A + B is not defined.
(ii) Addition of matrices is an example of a binary operation on the set of matrices of the same order.

Multiplication of a matrix by scalar number: Let A = [aij]m×n be a matrix and k is scalar, then kA is another matrix obtained by multiplying each element of A by the scalar k, i.e. if A = [aij]m×n, then kA = [kaij]m×n.
Matrices Class 12 Notes Maths Chapter 3 2

Properties of Scalar Multiplication of a Matrix
Let A = [aij] and B = [bij]be two matrices of the same order say m × n, then
(a) k(A + B) = kA + kB, where k is a scalar.
(b) (k + l)A = kA + lA, where k and l are scalars.

Multiplication of Matrices: Let A and B be two matrices. Then, their product AB is defined, if the number of columns in matrix A is equal to the number of rows in matrix B.
Matrices Class 12 Notes Maths Chapter 3 3

Properties of Multiplication of Matrices
(a) Non-commutativity Matrix multiplication is not commutative i.e. if AB and BA are both defined, then it is not necessary that AB ≠ BA.
(b) Associative law For three matrices A, B, and C, if multiplication is defined, then A (BC) = (AB) C.
(c) Multiplicative identity For every square matrix A, there exists an identity matrix of the same order such that IA = AI = A.
Note: For Amxm, there is only one multiplicative identity Im.
(d) Distributive law For three matrices A, B, and C,
A(B + C) = AB + AC
(A + B)C = AC + BC
whenever both sides of the equality are defined.

Note: If A and B are two non-zero matrices, then their product may be a zero matrix.
e.g. Suppose A = \(\begin{bmatrix} 0 & -1 \\ 0 & 2 \end{bmatrix}\) and B = \(\begin{bmatrix} 3 & 5 \\ 0 & 0 \end{bmatrix}\), then AB = \(\begin{bmatrix} 0 & 0 \\ 0 & 0 \end{bmatrix}\).

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Chapter 2 Map Scale | Class 11th Practical Work in Geography revision notes

What is a Map Scale?

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Map scales are useful to understand the sizes of objects and distances between objects (their relative sizes) in comparison to the actual sizes of objects and distances between them. This means that on a map it is not possible to denote the actual distances between objects or their sizes since then the map would need to be as big as the objects being measured. This would defeat the purpose of having a map in the first place. 

This is what it means when it is said that maps are drawn to scale. Scales are always mentioned on the maps so that whoever looks at them can get an idea of how to navigate through them. The scale represents how much the area on the map corresponds to the actual area on the ground that it shows. For example, if a map is drawn to a scale of one inch to one kilometre, it would mean that one inch on the map is equivalent to one kilometre on the ground. 

Classification of Maps

To understand what a map scale is, let us go through a few classifications of maps and map scales first. As per the common classification of maps, there are about five types of maps – thematic maps, general maps, navigation charts, topographic maps, series maps, cadastral, and plans. The types of map scale representations are discussed below. The basic type of representation of actual distance on maps is done by bar scales and lexical scales. In the bar scales used in maps, the distance ratio is expressed visually whereas, in lexical scales, the ratio is stated in words. 

There are 3 ways of representing the scale of a map, namely, representative fraction, verbal, and graphic. Out of these three, the representative fraction is the most commonly used scale. For example, the topographic maps help to understand the contour and general landforms of an area and most have the scale stated in representative fraction. In topographic maps, various colours are used to represent the contour of landforms, water bodies, settlements. 

Map Projections

Map projections are used to draw the parallels and meridians of the Earth systematically, on a flat surface. Various map projections are used to represent the landforms on maps. There are certain map projections that have equal-area properties. Also, projections that have the feature of conformal delineations are devised to represent the landforms on maps. 

In certain cases, the outlined shape of very small regions is nearly represented in the same way on the map as it is on the ground. It is not possible to completely avoid distortions of shapes of land areas on large-scale maps. The only way to reduce the distortions is to devise the most suitable for the purpose of the particular map. 

In general, the Mercator projection is devised on the navigational charts. The charts for the polar regions and the great circle charts do not devise the ordinary Mercator projections. The Great Circle charts that represent large map areas are generally depicted on quite small scales devising gnomonic projection. For example, the navigational chart for the Pacific Ocean. The navigators use these charts to lay a track between two ports and calculate the shortest distance between the ports.         

Symbolization

Symbols are the graphical representations of landforms, water bodies, winds, ocean currents, settlements, transport, and communication systems for maps. It may be said that symbols make a graphical language for maps and charts. The symbols were originally ordinary pictograms, which have now developed into conventional signs and symbols for the representation and interpretation of maps.

Standardization of symbols has been brought about by the joint efforts of the UN, NATO, International Map of the World agreements, and the international technical societies. It helped to reduce the confusion that used to arise in the interpretation of maps. The symbols can be classified as hypsographic and planimetric. These symbols can also be grouped based on conventional colours. 

For example, the blue colour is used to represent water bodies, black colour is used to represent occupation, cultures, and names of population, green colour is used to depict vegetation, brown colour is used to depict relief features, and red colour is used to depict types of roads and other special information. This is the standard use of colours, but there may be variations for geologic and soil maps. Planimetric features are used to represent the slopes, heights, and shapes of the land, on a map.

Nomenclature

To enhance the utility of maps, all the possible features and places are identified and labelled on a map. However, for the small-scale maps, only the important features and places are labelled, to enhance legibility. The nomenclature of maps has various parts. The geographic names are among the most troublesome parts of map nomenclature. The large-scale maps permit the naming of the minor features like streams, hilltops, ridges, etc. While making a topographic map, extensive research and documentation are carried out. 

Also, the local records are referred to for identifying and labelling all the parts of the area under concern. When a topographical map is published and distributed, it is used as an official document that eliminates confusion regarding the nomenclature of the local areas. The basic types of lettering that are used in the maps are Roman style, Italic, and Gothic style. 

What is the Significance of the Map Scale?

Map scales give people an accurate idea about how the distances mentioned are plotted on the map. This is useful in understanding how to go from one place to another, especially if one is a traveller or engaged in a similar profession. 

For academics, a map scale is useful to measure exact distances between objects and base their work on that. This is useful in calculating operations such as measuring the demographics of an area, measuring the geographical faults of an area, keeping a note of all physical features of the area and its vegetation, and so on. Measuring and making a note of all detailed features of an area on a map is only possible through map scales. If maps were not drawn to scale then no one would be able to navigate through an unknown place all on their own. 

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 Chapter 8 Weather Instruments, Maps and Charts | Class 11th Practical Work in Geography revision notes

NCERT Class 11 Practical Geography Chapter 8: Weather Instruments, Maps and Charts

Weather & Forecast

Weather & Forecast
  • Weather: The condition of the atmosphere at a given place and time with respect to atmospheric pressure, temperature, humidity, precipitation, cloudiness and wind. These factors are known as weather elements.
  • Weather Forecast: Prediction with a reasonable amount of certainty about the conditions of weather that would prevail in the coming 12 to 48 hours in a certain area.
  • The Indian Meteorological Department (IMD) was established in 1875, with its headquarters at Calcutta. The IMD headquarters are presently located at New Delhi

Weather Observations – 3 Levels

Weather Observations – 3 Levels

The World Meteorological Organization (WMO) , a specialized agency of the United Nations, coordinates these observations

Spaced Based Observations (E. G. INSAT)

Spaced Based Observations

Weather satellites make comprehensive and large-scale observations of different meteorological elements at the ground level as well in the upper layers of the atmosphere. The geo-stationary satellites provide space-based observations about weather conditions

Surface Observations – IMD Class 1 (Highest Category)

Surface Observations
  • A typical surface observatory has instruments for measuring and recording weather elements like temperature (maximum and minimum) , air pressure, humidity, clouds, wind, and rainfall. Specialized observatories also record elements like radiation, ozone atmospheric trace gases, pollution, and atmospheric electricity. These observations are taken all over the globe at fixed times of the day
  • Observations are taken in these observatories normally at 00, 03, 06, 09, 12, 15,18, 21 hours (Greenwich Mean Time) around the globe.
  • For logistics – some observations are limited on daily numbers

Stevenson Screen: Thermometers

Stevenson Screen: Thermometers
  • The Stevenson screen is designed to protect thermometers from precipitation and direct sunlight while allowing air to circulate freely around them. It is made from wood with louvered sides to allow free and even flow of air. It is painted white to reflect radiation. It stands on four legs and is about 3 feet 6 inches above the level of the ground. The legs must be sufficiently rigid and be buried sufficiently in the ground to prevent shaking.
  • The front panel is hinged at the bottom to form a door, which allows for maintenance and reading of the thermometers. The door of Stevenson screen is always towards the north in the northern hemisphere and towards the south in the southern hemisphere because direct sunrays also affect mercury. The purpose of the Stevenson screen is to create a uniform temperature enclosure that closely represents the same temperature as the air outside

Maximum & Minimum Thermometers

Maximum & Minimum Thermometers
  • Thermometer is used to measure air temperature. Most thermometers are in the form of a narrow closed glass tube with an expanded bulb at one end. The bulb and the lower part of the tube are filled with liquid such as mercury or alcohol. Before the other end is sealed off, the air in the tube is released by heating it.
  • Celsius – melting ice is marked 0 degree C and that of boiling water as 100 degree C, and the interval between the two is divided into 100 equal parts
  • On the Fahrenheit thermometer, the freezing and boiling points of water are graduated as 32 degree F and 212 degree F respectively
  • While the maximum thermometer and minimum thermometer are used to measure the air temperature, the dry bulb and the wet bulb thermometers are used to determine the humidity in the air. A set of these thermometers is kept in the Stevenson Screen.
  • The maximum thermometer is designed to record the highest temperature during a day. As the temperature increases, the mercury moves up into the tube; however, as the mercury cools, it cannot move downwards because of a constriction in the tube. It must be reset again to bring it down
  • Minimum thermometer – In this thermometer, alcohol is used in place of mercury. When the temperature decreases, the metal pin in the tube goes down and strikes at the minimum temperature.

Wet & Dry Bulb Thermometers

Wet & Dry Bulb Thermometers
  • The dry bulb and wet bulb thermometers are two identical thermometers fixed to a wooden frame. The bulb of the dry thermometer is kept uncovered and is exposed to the air while the bulb of the wet bulb thermometer is wrapped up with a piece of wet muslin, which is kept continuously moist by dipping a strand of it into a small vessel of distilled water. The evaporation from the wet bulb lowers its temperature.
  • Dry bulb readings are not affected by the amount of water vapour present in the air, but the wet bulb readings vary with it since the rate of evaporation is dependent upon the amount of water vapour present in the air. The greater the humidity in the air, the slower the rate of evaporation and hence, the difference between the readings of the dry bulb and wet bulb will be small. On the other hand, when the air is dry, the evaporation from the surface of the wet bulb is rapid, which would lower its temperature and the difference between the two readings would be larger.
  • Difference of the readings of the dry bulb and the wet bulb thermometers determines the state of the atmosphere with regard to its humidity.
  • The larger the difference, the more arid is the air.

Wind Vane

Wind Vane Device
  • Wind vane is a device used to measure the direction of the wind. The wind vane is a lightweight revolving plate with an arrowhead on one end and two metal plates attached to the other end at the same angle. This revolving plate is mounted on a rod in such a manner that it is free to rotate on a horizontal plane
  • The arrow always points towards the direction from which the wind blows

Rain Gauge

Rain Gauge
  • The amount of rainfall is measured with the help of a rain gauge. The rain gauge consists of a metal cylinder on which a circular funnel is fitted. The diameter of the funnel՚s rim is normally 20 cm
  • Normally, rainfall is measured in the units of millimetres or centimetres. Snow is also measured in a similar manner by turning it into liquid form
    • Temperature- Thermometer 
    • Atmospheric Pressure -Barometer -Millibars
    • Wind (Direction) -Wind Vane -Cardinal points
    • Wind (Velocity) – Anemometer -Km/hr
    • Rainfall -Rain Gauge- mm/cm

Barometer

Barometer Weight
  • The air around us has weight, and it exerts great pressure on the earth՚s surface. At the sea level, under normal conditions, the pressure of air is 1.03 kg per square centimetre. Due to constant movement of air, change in temperature and variation in its vapour content, the weight of the air changes continuously with time and place.
  • Mercury barometer, aneroid barometer and barographs. The unit of measurement is in the millibar.
  • Mercury barometer is an accurate instrument and is used as a standard. In it the atmospheric pressure of any place is balanced against the weight of a column of mercury in an inverted glass tube
  • The mercury will flow out of the tube into the cup and stand at a definite height above the level of the liquid in the cup. This is because the weight of the column of the mercury in the tube, above the surface of the mercury in the cup, is balanced by the weight of the air column of an indefinite height exerted as pressure upon an equal cross-section of the liquid surface. The height of the column of mercury in the tube, therefore, becomes the measure of the pressure of air.
  • Aneroid barometer gets its name from the Greek work, aneros (a- ‘not’ , neros – ‘moisture’ , meaning without liquid) It is a compact and portable instrument. It consists of a corrugated metal box made up of a thin alloy, sealed completely, and made airtight after partial exhaustion of air. It has a thin flexible lid, which is sensitive to changes of pressure.
  • As the pressure increases, the lid is pressed inward, and this, in turn, moves a system of levers connected to a pointer, which moves clockwise over the graduated dial and gives higher reading. When the pressure decreases, the lid is pushed outward and the pointer moves counter clockwise, indicating lower pressure
  • Barograph works on the principle of aneroid barometer. There are a number of vacuum boxes placed one above the other so that the displacement is large. A system of levers magnifies this movement, which is recorded by a pen on a paper attached to a rotating drum. The readings of a barograph are not always accurate, and therefore, they are standardized by comparing them with a mercury barometer reading.

Weather Maps, Charts & Symbols

  • Weather Maps: A weather map is the representation of weather phenomena of the earth or a part of it on a flat surface. It depicts conditions associated with different weather elements such as temperature, rainfall, sunshine and cloudiness, direction and velocity of winds, etc. on a particular day. Such observations being taken at fixed hours are transmitted by code to the forecasting stations. The central office keeps a record of the observations, which forms the basis for making a weather map. The upper air observations, which are procured from hill stations, aeroplanes, pilot balloons, etc. , are plotted separately
  • Meteorological observatories transmit the data to the Central Observatory at Pune twice a day. Data is also collected on ships plying on the Indian seas. A good progress has been made in the field of weather forecasting and observation with the establishment of weather observatories in Antarctica, the International Indian Ocean Expedition, and the launching of rockets and weather satellites.
  • Weather Charts: The data received from various weather observatories are in plenty and detailed. As such, they cannot be incorporated in one single chart unless the coding designed to give the economy of expression is used. These are called synoptic weather charts and the codes used are called meteorological symbols. Weather charts provide the primary tools for weather forecasting. They help in locating and identifying different air masses, pressure systems, fronts, and areas of precipitation.
  • WEATHER SYMBOLS: The messages received from all the observatories are plotted on the map using weather symbols standardized by the World Meteorological Organization and the National Weather Bureaus.

Isobars, Isotherms, Isohyets, Isohels, Isonephs

Isobars, Isotherms, Isohyets, Isohels, Isonephs

Isobars: Lines connecting places of equal air pressure.

Isotherms: Lines connecting places of equal temperature.

Isohyets: Lines connecting places of equal amount of rainfall over a given period.

Isohels: Lines connecting places of same mean daily duration of sunshine.

Isonephs: Lines connecting places of same mean value of cloud cover

Isobars, Isotherms, Isohyets, Isohels, Isonephs

Weather Map Interpretation

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Chapter 7 Introduction To Remote Sensing | Class 11th Practical Work in Geography revision notes

NCERT Class 11 Chapter 7 Practical Geography Introduction to Remote Sensing

Unlike aerial photo which observe similar to human eyes.

Remote sensing can go much beyond & react to much wider range of radiations reflected/emitted, absorbed and transmitted by all object surfaces at a temperature above 0 Kelvin () .

The term remote sensing was first used in the early 1960s. Later, it was defined as the total processes used to acquire and measure the information of some property of objects and phenomena by a recording device (sensor) that is not in physical contact with the objects and phenomena in study

  • Absorptance: The ratio of the radiant energy absorbed by a substance to the energy it receives.
  • Band: The specific wavelength interval in the electromagnetic spectrum.
  • Digital image: An array of digital numbers (DN) arranged in rows and columns, having the property of an intensity value and their locations.
  • Digital Number: An intensity value of a pixel in a digital image.
  • Digital Image Processing: The numerical manipulation of DN values for extracting information about the phenomena of the surface they represent.
  • Electromagnetic Radiation (EMR) : The Energy propagated through a space or a medium at a speed of light.
  • Electromagnetic Spectrum: The continuum of EMR that ranges from short wave high frequency cosmic radiations to long wavelength low frequency radio waves.
  • False Colour Composite (FCC) : An artificially generated colour image in which blue, green and red colours are assigned to the wavelength regions to which they do not belong in nature. For example, in standard a False Colour Composite blue is assigned to green radiations (0.5 to ) , green is assigned to red radiations (0.6 to  and red is assigned to Near Infrared radiation (0.7 to ) .
  • Gray scale: A medium to calibrate the variations in the brightness of an image that ranges from black to white with intermediate grey values.
  • Image: The permanent record of a scene comprising of natural and synthetic features and activities, produced by photographic and non – photographic means.
  • Scene: The ground area covered by an image or a photograph.
  • Sensor: Any imaging or non – imaging device that receives EMR and converts it into a signal that can be recorded and displayed as photographic or digital image.
  • Reflectance: The ratio of the radiant energy reflected by a substance to the energy it receives.
  • Spectral Band: The range of the wavelengths in the continuous spectrum such as the green band ranges from 0.5 to  and the range of NIR band 0.7 to .

Stages in Remote Sensing

Stages in Remote Sensing
  • Source of Energy (sun/self-emission) – artificially by flashguns and energy beams in radar (radio detection and ranging)
  • Transmission of energy from the source to the surface of the earth – propagates at speed of light called Electromagnetic Radiation (EMR) – vary in size and frequency
  • Interaction of energy with the earth՚s surface
  • Propagation of reflected/emitted energy through atmosphere – atmosphere comprises of gases, water molecules, and dust particles. The energy reflected from the objects comes in contact with the atmospheric constituents and the properties of the original energy are modified. , H, and  molecules absorb energy in the middle infrared region; the dust particles scatter the blue energy. Hence, the energy that is either absorbed or scattered by the atmospheric constituents never reaches to sensor placed onboard a satellite and the properties of the objects carried by such energy waves are left unrecorded
  • Detection of the reflected/emitted energy by the sensor
  • Conversion of energy received into photographic/digital form of data – Digital image comprises digital numbers that are arranged in rows and columns. These numbers may also be converted into an analogue (picture) form of data product. The sensor onboard an earth-orbiting satellite electronically transmits the collected image data to an Earth Receiving Station located in different parts of the world. In India, one such station is located at Shadnagar near Hyderabad
  • Extraction of the information contents from the data products – errors are eliminated in data collected, image is corrected – digital image processing is done
  • Conversion of information into Map/Tabular forms – converted into different layers of thematic maps (use quantitative measures as well)
Electromagnetic Specturum

Based on the size of the waves and frequency, the energy waves are grouped into Gamma, X – rays, Ultraviolet rays, visible rays, Infrared rays, Microwaves, and Radio waves. Each one of these broad regions of spectrum is used in different applications. However, the visible, infrared and microwave regions of energy are used in remote sensing

Energy with the Earth՚s Surface

Interaction of Energy with the Earth՚s Surface: The propagating energy finally interacts with the objects of the surface of the earth. This leads to absorption, transmission, reflection, or emission of energy from the objects. We all know that all objects vary in their composition, appearance forms, and other properties. Hence, the objects՚ responses to the energy they receive are also not uniform.

For example, a fresh water body absorbs more energy in the red and infrared regions of the spectrum and appears dark/black in a satellite image whereas turbid water body reflects more in blue and green regions of spectrum and appears in light tone

Spectral Signatures Are Important

Spectral Signatures
  • Detection of Reflected/Emitted Energy by the Sensor: The sensors recording the energy that they receive are placed in a near – polar sun synchronous orbit at an altitude of 700 – 900 km. These satellites are known as remote sensing satellites (e. g. Indian Remote Sensing Series) . As against these satellites, the weather monitoring and telecommunication satellites are placed in a Geostationary position (the satellite is always positioned over its orbit that synchronizes with the direction of the rotation of the earth) and revolves around the earth (coinciding with the direction of the movement of the earth over its axis) at an altitude of nearly 36,000 km (e. g. INSAT series of satellites)
  • Sun Synchronous – 700 – 900 km, cover  N to , earth resource applications
  • Geostationary – 36000 km, cover  rdof the globe, orbital period is 24 hours, used in Telecommunication and weather monitoring
  • The images so acquired by space-borne sensors are in digital format as against the photographic format obtained through a camera-based system
Himalayas and Northern Indian Plain

Images of Himalayas and Northern Indian Plain by IRS Satellite taken in May (Left) and November (Right) show differences in the types of vegetation. The red patches in May image refer to Coniferous vegetation. In November image the additional red patches refer to deciduous plants and the light red colour is related to the crops

Satellite Multispectral Scanners

Satellite Multispectral Scanners
  • A sensor is a device that gathers electromagnetic radiations, converts it into a signal, and presents it in a form suitable for obtaining information about the objects under investigation. Based upon the form of the data output, the sensors are classified into photographic (analogue) and non – photographic (digital) sensors
  • A photographic sensor (camera) records the images of the objects at an instance of exposure. On the other hand, a non – photographic sensor obtains the images of the objects in bit-by-bit form. These sensors are known as scanners.
  • MultiSpectral Scanners (MSS) are used as sensors. These sensors are designed to obtain images of the objects while sweeping across the field of view. A scanner is usually made up of a reception system consisting of a mirror and detectors. A scanning sensor constructs the scene by recording a series of scan lines. While doing so, the motor device oscillates the scanning mirror through the angular field of view of the sensor, which determines the length of scan lines and is called swath. It is because of such reasons that the mode of collection of images by scanners is referred bit – by – bit. Each scene is composed of cells that determine the spatial resolution of an image. The oscillation of the scanning mirror across the scene directs the received energy to the detectors, where it is converted into electrical signals. These signals are further converted into numerical values called Digital Number (DN Values) for recording on a magnetic tape.
  • Whiskbroom (Across track) Scanners: The whiskbroom scanners are made up of a rotating mirror and a single detector. The mirror is so oriented that when it completes a rotation, the detector sweeps across the field of view between  and  to obtain images in a large number of narrow spectral bands ranging from visible to middle infrared regions of the spectrum. The total extent of the oscillating sensor is known as the Total Field of View (TFOV) of the scanner. While scanning the entire field, the sensor՚s optical head is always placed at a particular dimension called the Instantaneous Field of View (IFOV) .
  • Push broom (Along track) Scanners: The push broom scanners consist of a number of detectors, which are equivalent to the number obtained by dividing the swath of the sensor by the size of the spatial resolution. For example, the swath of High Resolution Visible Radiometer – 1 (HRVR – 1) of the French remote sensing satellite SPOT is 60 km and the spatial resolution is 20 metres. If we divide  metres, we get a number of 3000 detectors that are deployed in SPOT HRV – 1 sensor. In push broom scanner, all detectors are linearly arrayed and each detector collects the energy reflected by the ground cell (pixel) dimensions of 20 metres at a nadir՚s view.
Push Broom Scanners

Satellite Sensors Types of Resolution

Types of Sensor Resolution

Sensor Resolutions
  • Temporal – how many image in a given time
  • Spectral – shades can be recorded – frequency and sensitivity – quantization Data can be 0 to 16 or can be 0 to 255 – Color – The principles in obtaining such images is the extension of the dispersion of light in nature resulting in the appearance of the ‘rainbow’ and the use of prism in the lab. Strong absorption properties of fresh water in band 4 (Infrared) and mixed strong reflectance in band 2 (green) by dry surfaces
  • Radiometric resolution corresponds to the sensitivity of a sensor, i.e.. its ability to measure and to enable distinction within the same spectral band of differences (intensity or energy)
  • Spatial – distance – With an increasing resolution the identification of even smaller object surfaces become possible
Types of Resolution
Types of Resolution
Types of Resolution
Types of Resolution
Radiometric Resolution

Band 2: 0.52 to 0.59 

Band 3: 0.62 to 0.68 

Band 4: 0.77 to 0.86 

Dispersion of Light (The principle that is utilized in obtaining Multispectral Images)

The overall mechanism of obtaining images in a number of bands derives strength from the principle of the dispersion of light. You must have seen the rainbow. It is formed through a natural process of dispersion of light rays through water molecules present in the atmosphere. The same phenomena may be experimented by putting a beam of light at one side of a prism. At the other side of the prism, you may notice the dispersion of energy into seven colours that form white light

Elements of Image Interpretation

Image Interpretation
  • Tone or color: smooth and dry object surfaces reflect more energy in comparison to the rough and moist surfaces. Healthy vegetation reflects strongly in the infrared region because of the multiple-layered leaf structure and appears in a light tone or bright red colour in standard false colour composite and the scrubs appear in greyish red colour. Similarly, a fresh water body absorbs much of the radiations received by it and appears in dark tone or black colour, whereas the turbid water body appears in light tone or light bluish colour in FCC due to mixed response shown by the water molecules as well as suspended sand particles
  • Texture: dense residential areas in a large city form fine texture due to the concentration of the houses in a smaller area and the low-density residential areas produce a coarse texture. Similarly, in high-resolution images the sugarcane or millet plants produce coarse texture in comparison to the fine texture of rice or wheat plants. One can also notice the coarse texture in the images of scrubbed lands if compared with the fine texture of lush green evergreen forests.
  • Size: It helps in distinctively identifying the industrial and industrial complexes with residential dwellings, stadium in the heart of the city with brick kilns at an urban fringe, size and hierarchy of the settlements
  • Shape: railway line can be readily distinguished from a road due to its long continuous linearity in shape with gradual change in its course.
  • Shadow: The shape of some of the objects is so typical that they could not be identified without finding out the length of the shadow they cast. For example, the Qutub Minar located in Delhi, minarets of mosques, overhead water tanks, electric or telephone lines, and similar features can only be identified using their shadow
  • Pattern: planned residential areas with the same size and layout plan of the dwelling units in an urban area can easily be identified if their pattern is followed. Similarly, orchards and plantations produce arrangements of the same type of plants with uniform inter plant distances.
  • Association: an educational institution always finds its association with its location in or near a residential area as well as the location of a playground within the same premises. Similarly, stadium, race course and golf course holds good for a large city, industrial sites along highway at the periphery of a growing city, and slums along drains and railway lines
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Chapter 6 Introduction To Aerial Photographs | Class 11th Practical Work in Geography revision notes

Aerial Photographs Revision notes

  • When we look to an object directly – horizontal perspective
  • When we look below – birds eye view – aerial perspective
  • The photographs taken from an aircraft or helicopter using a precision camera are termed aerial photographs.
  • Aerial Camera: A precision camera specifically designed for use in aircrafts.
  • Aerial Film: A roll film with high sensitivity, high intrinsic resolution power and dimensionally stable emulsion support.
  • Aerial Photography: Art, science and technology of taking aerial photographs from an air-borne platform.
  • Aerial Photograph: A photograph taken from an air-borne platform using a precision camera.
  • Fiducial Marks: Index marks, rigidly connected at the central or corner edges of the camera body. When the film is exposed, these marks appear on the film negative.
  • Forward Overlap: The common area on two successive photographs in the flight direction. It is usually expressed in per cent.
  • Image Interpretation: An act of identifying the images of the objects and judging their relative significance.
  • Nadir Point: The foot of the perpendicular drawn from the camera lens center on the ground plane.
  • Principal Point: The foot of the perpendicular drawn from the camera lens center on the photo plane.
  • Principal Distance: The perpendicular distance from the perspective center to the plane of the photograph.
  • Perspective Centre: The point of origin (perspective center) of the bundle of light rays.
  • Photogrammetry: The science and technology of taking reliable measurements from aerial photographs.

Uses of Aerial Photography

  • development of photogrammetry and photo/image interpretation
  • Photogrammetry: It refers to the science and technology of making reliable measurements from aerial photographs – precise measurement of length, breadth and height – creating and updating topographic maps
  • Image Interpretation: It is an art of identifying images of objects and judging their relative significance – get qualitative information on land use and soil and analyses land use data
  • India – started in 1920s for Agra; Irrawaddy Delta forests in 1923 – 24,
  • Today, aerial photography in India is carried out for the entire country under the overall supervision of the Directorate of Air Survey (Survey of India) New Delhi.
  • Three flying agencies, i.e.. Indian Air Force, Air Survey Company, Kolkata and National Remote Sensing Agency, Hyderabad as A, B and C respectively
  • The procedure for indenting aerial photographs for educational purposes could be made with APFPS Party No. 73, Directorate of Air Survey, Survey of India, West Block IV, R. K. Puram, New Delhi.

Advantages of Aerial Photography

  • Improved vantage point: Aerial photography provides a bird՚s eye view of large areas
  • Time freezing ability: An aerial photograph is a record of the surface features at an instance of exposure – provide historical record
  • Broadened Sensitivity: Our eyes perceive only in the visible region of the electromagnetic spectrum, i.e.. 0.4 to 0.7 μm whereas the sensitivity of the film ranges from 0.3 to 0.9 μm.
  • Three Dimensional Perspective: Aerial photographs are normally taken with uniform exposure interval that enables us in obtaining stereo pair of photographs

Types of Aerial Photographs Based on the Position of the Cameral Axis

Types of Aerial Photographs
  • Vertical Photographs: While taking aerial photographs, two distinct axes are formed from the camera lens center, one towards the ground plane and the other towards the photo plane.
  • If such a deviation is within the range of plus or minus 3o, the near-vertical aerial photographs are obtained. Any photography with an unintentional deviation of more than 3o in the optical axis from the vertical axis is known as a tilted photograph.
  • Low Oblique: An aerial photograph taken with an intentional deviation of 15° to 30° in the camera axis from the vertical axis is referred to as the low oblique photograph. In reconnaissance surveys.
  • High Oblique: The high oblique are photographs obtained when the camera axis is intentionally inclined about 60° from the vertical axis
Types of Aerial Photographs

Types of Aerial Photographs Based on Scale

  • Large Scale Photographs: When the scale of an aerial photograph is 1: 15,000 and larger
  • Medium Scale Photographs: The aerial photographs with a scale ranging between 1: 15,000 and 1: 30,000
  • Small Scale Photographs: The photographs with the scale being smaller than 1: 30,000
  • Small area and try to zoom it – large scale map covers smaller area with greater detail and then from a colony to a city

Geometry of Aerial Photographs

Geometry of Aerial Photographs
  • To understand the geometry of an aerial photograph, it is important to appreciate the orientation of the photograph with respect to the ground
  • Parallel Projection: In this projection, the projecting rays are parallel but not necessarily perpendicular. The triangle ABC is projected on LL1 as triangle abc
  • Orthogonal Projection: This is a special case of parallel projections with light source at infinity. Maps are orthogonal projections of the ground – here distances, angles or areas on the plane are independent of the elevation differences of the objects. Orthogonal projection where the projecting rays are perpendicular to the line LL1.
  • Central Projection: The projecting rays Aa, Bb and Cc pass through a common point O, which is called the perspective Centre. The image projected by a lens is treated like a central projection as in aerial photographs. In an absolutely vertical flat terrain, the aerial photograph will be geometrically the same as the corresponding map of the area. However, because of the tilt of the photograph and relief variations of the ground photographed, an aerial photograph differs geometrically from the map of the corresponding area.
  • vertical line (plumb line as indicated by the direction of gravity)
  • For an oblique photograph, the angle between the camera axis and the plumb line is the tilt angle.
  • The geometry of the positive and the negative planes are identical.

SP = distance b/w camera lens and negative plane = focal length

SPG = distance b/w camera lens and ground = flying height

Aerial Photograph

  • It is a central Projection.
  • An aerial photograph is geometrically incorrect. The distortion in the geometry is minimum at the center and increases towards the edges of the photographs.
  • The scale of the photograph is not uniform.
  • Enlargement/reduction does not change the contents of the photographs and can easily be carried out.
  • Aerial photography holds good for inaccessible and inhospitable areas.

Map

  • It is an orthogonal Projection.
  • A map is a geometrically correct representation of the part of the earth projected.
  • The scale of the map is uniform throughout the map extent.
  • Enlargement/reduction of the maps involves redrawing it afresh.
  • The mapping of inaccessible and inhospitable areas is very difficult and sometimes it becomes impossible.
  • Even vertical aerial photographs do not have a consistent scale unless they have been taken of a flat terrain. Aerial photographs need to be transformed from perspective view to the planimetric view before they can be used as map substitute. Such transformed photographs are known as orthophotos.
  • In a perspective view, all light rays reflected from the Earth՚s surface pass through a single point at the center of the camera lens. A planimetric (plan) view looks as though every position on the ground is being viewed from directly above.
  • A map cannot be directly traced out of an aerial photograph. The reason is that there is a basic difference in the planimetry (projection) and perspective of a map and an aerial photograph.
  • Method 1: By Establishing Relationship Between Photo Distance and Ground Distance
  • Method 2: By Establishing Relationship Between Photo Distance and Map Distance
  • Method 3: By Establishing Relationship Between Focal Length (f) and Flying Height (H) of the Aircraft
  • Scale is the ratio of a distance on an aerial photograph the distance between the same two places on the ground in the real world expressed as RF. Scale determines what objects would be visible, the accuracy of estimates and how certain features will appear
  • Method 1: By Establishing Relationship Between Photo Distance and Ground Distance scale of an aerial photograph will be measured as a ratio of the two, i.e.. Dp/Dg

Question: The distance between two points on an aerial photograph is measured as 2 cm. The known distance between the same two points on the ground is 1 km. Compute the scale of the aerial photograph (Sp) .

Sp = Dp: Dg

= 2 cm: 1 km

= 2cm: 1 x 100,000 cm

= 1: 100,000/2 = 50,000 cm

= 1 unit represents 50,000 units

Therefore, Sp = 1: 50,000

Scale of Aerial Photograph

  • Method 2: By Establishing Relationship Between Photo Distance and Map Distance, distances between two points identifiable both on a map and the aerial photograph enable us to compute the scale of the aerial photograph (Sp) . The relationship between the two distances may be expressed as under: (Photo scale: Map scale) = (Photo distance: Map distance)
  • We can derive, Photo scale (Sp) = Photo distance (Dp) : Map distance (Dm) x Map scale factor (msf)

Question: The distance measured between two points on a map is 2 cm. The corresponding distance on an aerial photograph is 10 cm. Calculate the scale of the photograph when the scale of the map is 1: 50,000.

Sp = Dp: Dm x msf

Or = 10 cm: 2 cm x 50,000

Or = 10 cm: 100,000 cm

Or = 1: 100,000/10 = 10,000 cm

Or = 1 unit represents 10,000 units

Therefore, Sp = 1: 10,000

  • Method 3: By Establishing Relationship Between Focal Length (f) and Flying Height (H) of the Aircraft
  • Focal Length (f) : Flying Height (H) = Photo distance (Dp) : Ground distance (Dg)

Question: Compute the scale of an aerial photograph when the flying height of the aircraft is 7500m and the focal length of the camera is 15cm.

Sp = f: H

Or Sp = 15 cm: 7,500 x 100 cm

Or Sp = 1: 750,000/15

Therefore, Sp = 1: 50,000

Marginal Information Given on Vertical Aerial Photographs

Marginal Information Given on Vertical Aerial Photographs

⚹ 793 is a Photo Specification number maintained by the 73 APFPS Party of the Survey of India. B is the Flying Agency that carried out the present photography (In India three flying agencies are officially permitted to carry out aerial photography. They are the Indian Air Force, the Air Survey Company, Kolkata and the National Remote Sensing Agency, Hyderabad, identified on the aerial photographs as A, B and C respectively) , 5 is the strip number and 23 is the photo number in strip 5.

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Chapter 5 Topographical Maps | Class 11th Practical Work in Geography revision notes

NCERT Class 11 Chapter 5 Practical Geography Topographical Maps

Topographical Maps

Topographical Maps
  • These maps show important natural and cultural features such as relief, vegetation, water bodies, cultivated land, settlements, and transportation networks, etc. These maps are prepared and published by the National Mapping Organization of each country. For example, the Survey of India prepares the topographical maps in India for the entire country. The topographical maps are drawn in the form of series of maps at different scales. Hence, in the given series, all maps employ the same reference point, scale, projection, conventional signs, symbols, and colours.
  • Topographic Map: A map of a small area drawn on a large-scale depicting detailed surface features both natural and manmade. Relief in this map is shown by contours.

Topographical Maps in India in 2 Series

India in 2 Series
  • India and Adjacent Countries Series: the Survey of India prepared topographical maps under India and Adjacent Countries Series until the coming into existence of Delhi Survey Conference in 1937. Henceforth, the preparation of maps for the adjoining countries was abandoned and the Survey of India confined itself to prepare and publish the topographical maps for India as per the specifications laid down for the International Map Series of the World. However, the Survey of India for the topographical maps under the new series retained the numbering system and the layout plan of the abandoned India and Adjacent Countries Series. The topographical maps of India are prepared on 1: 10,00, 000,1: 250,000, 1: 1,25, 000,1: 50,000 and 1: 25,000 scale providing a latitudinal and longitudinal coverage of  and , respectively.
  • International Map Series of the World: Topographical Maps under International Map Series of the World are designed to produce standardized maps for the entire World on a scale of 1: 10,00, 000, and 1: 250,000.
  • The study of topographical maps is simple. It requires the reader to be acquainted with the legend, conventional sign, and the colours shown on the sheets.
Topographical Maps
  • The Survey of India is India՚s central engineering agency in charge of mapping and surveying. Set up in 1767 to help consolidate the territories of the British East India Company It is one of the oldest Engineering Departments of the Government of India. The Survey of India՚s distinguished history includes the handling of the mammoth Great Trigonometric Survey under William Lambton and George Everest
  • Among the many accomplishments of the Survey were the demarcation of the British territories in India and the measurement of the height of the Himalayan giants: Everest, K2, and Kanchenjunga. The Great Trigonometrical Survey of India started on 10 April 1802 with the measurement of a baseline near Madras. The East India Company thought that this project would take about 5 years but eventually it took more than 60 years, draining the profits of the Company, so much so it was brought under the Crown after 1857
Toposheet
  • Toposheet number, state, district, latitude, longitude
  • Legend sheet, index to sheet, map scale, district outline, legend
  • National Map Policy: To provide, maintain and allow access and make available the National Topographic Database (NTDB) of the SOI conforming to national standards. To promote the use of geospatial knowledge and intelligence through partnerships and other mechanisms by all sections of the society and work towards a knowledge-based society.
  • Two Series Of Maps – DSM Defense Series Maps (DSMs) – These will be the topographical maps (on Everest/WGS-84 Datum and Polyconic/UTM Projection) on various scales (with heights, contours, and full content without dilution of accuracy) . These will mainly cater for defense and national security requirements. This series of maps (in analogue or digital forms) for the entire country will be classified, as appropriate, and the Ministry of Defense will formulate the guidelines regarding their use.
  • Two Series Of Maps – OSM Open Series Maps (OSMs) for supporting development activities in the country. OSMs shall bear different map sheet numbers and will be in UTM Projection on WGS-84 datum. Each of these OSMs (in both hard copy and digital form) will become “Unrestricted” after obtaining a one-time clearance of the Ministry of Defense. SOI will ensure that no civil and military Vulnerable Areas and Vulnerable Points (VA՚s/VP՚s) are shown on OSMs
  • National Topographical Data Base (NTDB) NTDB in analogue and digital forms consisting of following data sets: National Spatial Reference Frame, National Digital Elevation Model, National Topographical Template, Administrative Boundaries, and Toponomy (place names) . Both the DSMs and OSMs will be derived from the NTDB
Representative Fraction
  • Representative Fraction (RF) : It is the ratio between the distances on the map to its corresponding distance on actual ground. The RF on this map is 1: 50,000.
  • Scale: Scale is the ratio between the distance of any two points on the map and the actual distance of the same points on the ground. The scale of the given map extract is 2 cm: 1 km or 1: 50,000.
  • Contour: Contours are imaginary lines drawn on maps, joining all places with the same height above sea level.
  • Contour Interval: The interval between two consecutive contours is called contour interval.
  • Index Contour: Contour lines are thickened at regular intervals to make it easier to read contours. For example at every 100 mts, the contour line is made darker. The darker lines are called Index Contours.
  • Triangulated Height: It is the height of a place which has been calculated using trigonometry, represented by a small triangle e. g. 
  • Spot Height: The height of random places between contours shown with a dot. Eg – 0.425
  • Bench Mark: Height of a place actually marked on a stone pillar, rock or shown on a building as a permanent reference. It is written as BM 200 m.
  • Relative Height: Relative height is the height of a feature with reference to the height of the surrounding land and NOT to sea level. It is represented by the height with a small ‘r’ e. g. – 12r.
  • Mixed Forest: A forest with more than two varieties of trees growing in close proximity to each other.
  • Open Jungle: A forest where trees are widely scattered
  • Dense Jungle: A forest where trees grow very close to each other
  • OPEN SCRUB: Scrub is a vegetation found in regions with less than 100 cm of rainfall. Therefore, it indicates a dry region.
  • Embankment: They are raised rock or soil filled constructions on which roads/railway tracks are built. Also made near tanks and rivers to prevent flooding
  • Form Lines: Form lines are contour lines, but show only approximate heights above sea level as they are used to indicate the elevations of the area, which are not accessible for proper survey. Hence, they are drawn as broken lines and are called ‘form lines’ .
  • Q. C. Q. D. , OC, OD, PQ, ETC: These are alphabetical codes used to represent the biggest grid sq. of 10,000 square kms

Methods of Relief Representation

Relief Representation
  • Methods of Relief Representation: The earth՚s surface is not uniform and it varies from mountains to hills to plateaus and plains. The elevation and depressions of the earth՚s surface are known as physical features or relief features of the earth. The map showing these features is called a relief map.
  • A number of methods have been used to show the relief features of the Earth՚s surface on maps, over the years. These methods include hachure, hill shading, layer tints, benchmarks and spot heights and contours. However, contours and spot heights are predominantly used to depict the relief of an area on all topographical maps.
  • Settlements, buildings, roads, and railways are important cultural features shown on topographical sheets through conventional signs, symbols, and colours.
  • Four types of rural settlements may be identified on the map
    • Compact
    • Scattered
    • Linear
    • Circular
  • Similarly, urban centres may also be distinguished as
    • Cross-road town
    • Nodal point
    • Market centre
    • Hill station
    • Coastal resort centre
    • Port
    • Manufacturing centre with suburban villages or satellite towns
    • Capital town
    • Religious centre
  • Various factors determine the site of settlements like
    • Source of water
    • Provision of food
    • Nature of relief
    • Nature and character of occupation
    • Defence
  • Density of settlement is directly related to food supply. Sometimes, village settlements form alignments, i.e.. they are spread along a river valley, road, embankment, and coastline, – and these are called linear settlements.
  • In the case of an urban settlement, a crossroad town assumes a fan-shaped pattern, the houses being arranged along the roadside, and the crossing being at the heart of the town and the main market place. In a nodal town, the roads radiate in all directions

Contours

Types of Contours
  • Contours are imaginary lines joining places having the same elevation above mean sea level. A map showing the landform of an area by contours is called a contour map.
  • Earlier, ground surveys and levelling methods were used to draw contours on topographical maps. However, the invention of photography and subsequent use of aerial photography have replaced the conventional methods of surveying, levelling and mapping. Henceforth, these photographs are used in topographical mapping.
  • Contours are drawn at different vertical intervals (VI) , like 20,50, 100 metres above the mean sea level. It is known as contour interval. It is usually constant on a given map. It is generally expressed in metres. While the vertical interval between the two successive contour lines remains constant, the horizontal distance varies from place to place depending upon the nature of slope. The horizontal distance, also known as the horizontal equivalent (HE) , is large when the slope is gentler and decreases with increasing slope gradient.
Contour Vertical Intervals
  • Contours: Imaginary lines joining all the points of equal elevation or altitude above mean sea level. They are also called “level lines.”
  • Contour Interval: Interval between two successive contours. It is also known as vertical interval, usually written as V. I. Generally, it is constant for a given map.
  • Cross-section: A side view of the ground cut vertically along a straight line. It is also known as a section or profile.
  • Hachures: Small straight lines drawn on the map along the direction of maximum slope, running across the contours. They have given an idea about the differences in the slope of the ground.
  • The slopes can broadly be classified into gentle, steep, concave, convex and irregular or undulating. The contours of different types of slopes show a distinct spacing pattern.
  • Gentle Slope – When the degree or angle of slope of a feature is very low, the slope will be gentle. The contours representing this type of slope are far apart.
  • Steep Slope – When the degree or angle of slope of a feature is high and the contours are closely spaced, they indicate steep slope.

Steps for Drawing a Cross-Section

The following steps may be followed to draw cross-sections of various relief features from their contours:

  • Draw a straight line cutting across the contours on the map and mark it as AB.
  • Take a strip of white paper or graph and place its edge along the AB line.
  • Mark the position and value of every contour that cuts the line AB.
  • Choose a suitable vertical scale, eg  cm = 100 metres, to draw horizontal lines parallel to each other and equal to the length of AB. The number of such lines should be equal or more than the total contour lines.
  • Mark the appropriate values corresponding to the contour values along the vertical of the cross-section. The numbering may be started with the lowest value represented by the contours.
  • Now place the edge of the marked paper along the horizontal line at the bottom line of the cross-section in such a way that AB of the paper corresponds to the AB of the map and mark the contour points.
  • Draw perpendiculars from AB line, intersecting contour lines, to the corresponding line at the cross-section base.
  • Smoothly join all the points marked on different lines at the cross section base.
Concave Slope
  • Concave Slope: A slope with a gentle gradient in the lower parts of a relief feature and steep in its upper parts is called the concave slope. Contours in this type of slope are widely spaced in the lower parts and are closely spaced in the upper parts.
  • Convex Slope: Unlike concave slope, the convex slope is fairly gentle in the upper part and steep in the lower part. As a result, the contours are widely spaced in the upper parts and are closely spaced in the lower parts.
Conical Hill

Landforms

  • Conical Hill: It rises almost uniformly from the surrounding land. A conical hill with uniform slope and narrow top is represented by concentric contours spaced almost at regular intervals.
  • Plateau: A widely stretched flat – topped high land, with relatively steeper slopes, rising above the adjoining plain or sea is called a plateau. The contour lines representing a plateau are normally close spaced at the margins with the innermost contour showing wide gap between its two sides.
A Geomorphic Feature
  • Valley: A geomorphic feature lying between two hills or ridges and formed because of the lateral erosion by a river or a glacier is called a valley.
  • ‘V’ -shaped Valley: It resembles the letter V. A V-shaped valley occurs in mountainous areas. The lowermost part of the V – shaped valley is shown by the innermost contour line with very small gap between its two sides and the lowest value of the contour is assigned to it. The contour value increases with uniform intervals for all other contour lines outward.
  • ‘U’ – shaped Valley: A U – shaped valley is formed by strong lateral erosion of glaciers at high altitudes. The flat wide bottom and steep sides makes it resemble the letter ‘U’ . The lowermost part of the U – shaped valley is shown by the innermost contour line with a wide gap between its two sides. The contour value increases with uniform intervals for all other contour lines outward.
Gorge: In High Altitudes
  • Gorge: In high altitudes, gorges form in the areas where the vertical erosion by river is more prominent than the lateral erosion. They are deep and narrow river valleys with very steep sides. A gorge is represented by very closely spaced contour lines on a map with the innermost contour showing small gap between its two sides.
  • Spur: A tongue of land, projecting from higher ground into the lower is called a spur. It is also represented by Vshaped contours but in the reverse manner. The arms of the V point to the higher ground and the apex of ‘V’ to the lower ones.
Cliff: It is a Very Steep
  • Cliff: It is a very steep or almost perpendicular face of landform. On a map, a cliff may be identified by the way the contours run very close to one another, ultimately merging into one.
  • Waterfall and Rapids: A sudden and more or less perpendicular descent of water from a considerable height in the bed of a river is called a waterfall. Sometimes, a waterfall succeeds or precedes with a cascading stream forming rapids upstream or downstream of a waterfall. The contours representing a waterfall merge into one another while crossing a river stream and the rapids are shown by relatively distant contour lines on a map.

Interpretation

Marginal Information

Marginal Information: It includes the topographical sheet number, its location, grid references, its extent in degrees and minutes, scale, the districts

  • Relief – hill, plateau, plains, mountains
  • Drainage – trellis, radial, ring
  • Land use – vegetation, agriculture, services
  • Transport and communication
  • Settlement – rural and urban
  • Occupation – lumbering, forestry, fishing

Interpretation Procedure

Interpretation Procedure
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Chapter 4 Map Projections | Class 11th Practical Work in Geography revision notes

NCERT Class 11 Practical Geography Chapter 4 Map Projections

  • Map projection – transform spherical surface into flat location
  • Globe show directions and distances accurately
  • Horizontal – parallels and vertical lines are longitudes
  • Problems with globe – expensive, cannot be carried easily, meridians are semicircle and parallels are circles – on paper they become straight or curved line
  • Need for map projection
  • Detailed regions
  • Compare 2 natural regions
  • Transfer latitude and longitude on flat paper
  • Distortions increase with distance from tangential point (throwing light from center)
  • Tracing shape, size and directions, etc. from a globe is nearly impossible because the globe is not a developable surface
  • Lexodrome or Rhumb Line: It is a straight line drawn on Mercator՚s projection joining any two points having a constant bearing. It is very useful in determining the directions during navigation.
  • The Great Circle: It represents the shortest route between two points, which is often used both in air and ocean navigation.
  • Homolographic Projection: A projection in which the network of latitudes and longitudes is developed in such a way that every graticule on the map is equal in area to the corresponding graticule on the globe. It is also known as the equal-area projection.
  • Orthomorphic Projection: A projection in which the correct shape of a given area of the earth՚s surface is preserved

Elements of Map Projection

  • Reduced Earth: A model of the earth is represented by the help of a reduced scale on a flat sheet of paper. This model is called the “reduced earth.” This model should be more or less spheroid having the length of polar diameter lesser than equatorial and on this model, the network of graticule can be transferred.
  • Parallels of Latitude: These are the circles running round the globe parallel to the equator and maintaining uniform distance from the poles. Each parallel lies wholly in its plane, which is at right angle to the axis of the earth. They are not of equal length. They range from a point at each pole to the circumference of the globe at the equator. They are demarcated as  to  North and South latitudes.
  • Meridians of Longitude: These are semi-circles drawn in north south direction from one pole to the other, and the two opposite meridians make a complete circle, i.e.. circumference of the globe. Each meridian lies wholly in its plane, but all intersect at right angle along the axis of the globe. There is no obvious central meridian but for convenience, an arbitrary choice is made, namely the meridian of Greenwich, which is demarcated as  longitudes. It is used as reference longitudes to draw all other longitudes
  • Global Property: In preparing a map projection the following basic properties of the global surface are to be preserved by using one or the other methods:
    • Distance between any given points of a region;
    • Shape of the region;
    • Size or area of the region in accuracy;
    • Direction of any one point of the region bearing to another point.

Classification of Map Projection

  • Drawing Surface- Perspective, non-perspective & Mathematical
  • Developable (cylindrical, conical and zenithal) & Non-Developable
  • Source of light – gnomonic, stereographic and orthographic
  • Global properties – area, shape, direction, distance
Classification of Map Projection

Classification of Map Projection: Area, Shape & Distance

  • Drawing SurfacePerspective projections can be drawn taking the help of a source of light by projecting the image of a network of parallels and meridians of a globe on developable surface. Non – perspective projections are developed without the help of a source of light or casting shadow on surfaces, which can be flattened.
  • Mathematical or conventional projections are those, which are derived by mathematical computation and formulae and have little relations with the projected image (Mollweide, sinusoidal/Samson flam steed or homolosine)
  • Developable surface: A developable surface is one, which can be flattened, and on which, a network of latitude and longitude can be projected- cylindrical, conical and zenithal projections.
  • Zenithal projection is directly obtained on a plane surface when plane touches the globe at a point and the graticule is projected on it. Generally, the plane is so placed on the globe that it touches the globe at one of the poles. These projections are further subdivided into normal, oblique or polar
  • If it is tangential to a point between the pole and the equator, it is called the oblique projection; and if it is tangential to the pole, it is called the polar projection
  • If the developable surface touches the globe at the equator, it is equatorial or normal projection.
  • Non-Developable surface – non-developable surface is one, which cannot be flattened without shrinking, breaking, or creasing. A globe or spherical surface

Source of Light

  • Gnomonic projection is obtained by putting the light at the centre of the globe. Stereographic projection is drawn when the source of light is placed at the periphery of the globe at a point diametrically opposite to the point at which the plane surface touches the globe. Orthographic projection is drawn when the source of light is placed at infinity from the globe, opposite to the point at which the plane surface touches the globe
  • Global Properties: As mentioned above, the correctness of area, shape, direction, and distances are the four major global properties to be preserved in a map based on global properties; projections are classified into equal area, orthomorphic, azimuthal and equidistant projections.
  • (Area) Equal Area Projection is also called homolographic projection. Areas of various parts of the earth are represented correctly in that projection.
  • (Shape) Orthomorphic or True-Shape projection is one in which shapes of various areas are portrayed correctly. The shape is generally maintained at the cost of the correctness of area.
  • (Direction) Azimuthal or True-Bearing projection is one on which the direction of all points from the centre is correctly represented.
  • (Distance) Equi-distant or True Scale projection is that where the distance or scale is correctly maintained. It cannot be maintained throughout but at certain specific locations.

Examples of Cylindrical Projections

  • Equal-area cylindrical projection
  • Equidistant cylindrical projection
  • Mercator projection
  • Miller projection
  • Plate Carree projection
  • Universal transverse Mercator projection

Examples of Conical Projections

  • Albers Equal-area projection
  • Equidistant projection
  • Lambert conformal projection
  • Polyconic projection

Examples of Azimuthal Projections

  • Equidistant azimuthal projection
  • Gnomonic projection
  • Lambert equal-area azimuthal projection

Draw a Mercator՚s projection for the world map on the scale of 1: 250,000, 000 at  interval

Draw a Mercator՚s Projection

Construction of Projections

Mercator՚s Projection

A Dutch cartographer Mercator Gerardus Karmer developed this projection in 1569. The projection is based on mathematical formulae. So, it is an orthomorphic projection in which the correct shape is maintained. The distance between parallels increases towards the pole. Like cylindrical projection, the parallels and meridians intersect each other at right angle. It has the characteristics of showing correct directions. A straight line joining any two points on this projection gives a constant bearing, which is called a Laxodrome or Rhumb line.

  • Draw a line of 6.28 inches representing the equator as EQ:
  • Divide it into 24 equal parts. Determine the length of each division using the following formula: 
  • Calculate the distance for latitude with the help of the table given below:-

Latitude Distance

 inch

 inch

 inch

 inches

 inches

Properties

  • All parallels and meridians are straight lines and they intersect each other at right angles.
  • All parallels have the same length, which is equal to the length of equator.
  • All meridians have the same length and equal spacing. However, they are longer than the corresponding meridian on the globe.
  • Spacing between parallels increases towards the pole.
  • Scale along the equator is correct, as it is equal to the length of the equator on the globe; but other parallels are longer than corresponding parallel on the globe; hence, the scale is not correct along them. For example, the  parallel is 1.154 times longer than the corresponding parallel on the globe.
  • Shape of the area is maintained, but at the higher latitudes, distortion takes place.
  • The shape of small countries near the equator is truly preserved while it increases towards poles.
  • It is an azimuthal projection.
  • This is an orthomorphic projection as scale along the meridian is equal to the scale along the parallel.

Limitations

  • There is greater exaggeration of scale along the parallels and meridians in high latitudes. As a result, size of the countries near the pole is highly exaggerated. For example, the size of Greenland equals to the size of USA, whereas it is  thof USA.
  • Poles in this projection cannot be shown as  parallel and meridian touching them are infinite.

Uses

  • More suitable for a world map and widely used in preparing atlas maps.
  • Very useful for navigation purposes showing sea routes and air routes.
  • Drainage pattern, ocean currents, temperature, winds and their directions, distribution of worldwide rainfall and other weather elements are appropriately shown on this map

Construct a cylindrical equal area projection for the world when the R. F. of the map is 1: 300,000, 000 taking latitudinal and longitudinal interval as .

Construct a Cylindrical Equal

Cylindrical Equal Area Projection

The cylindrical equal area projection, also known as the Lamber՚s projection, has been derived by projecting the surface of the globe with parallel rays on a cylinder touching it at the equator. Both the parallels and meridians are projected as straight lines intersecting one another at right angles. The pole is shown with a parallel equal to the equator; hence, the shape of the area is highly distorted at the higher latitude.

Construction

  • Draw a circle of 2.1 cm radius;
  • Mark the angles of  and  for both, northern and southern hemispheres;
  • Draw a line of 13.2 cm and divide it into 24 equal parts at a distance of  apart. This line represents the equator;
  • Draw a line perpendicular to the equator at the point where  is meeting the circumference of the circle;
  • Extend all the parallels equal to the length of the equator from the perpendicular line

Properties

  • All parallels and meridians are straight lines intersecting each other at right angle.
  • Polar parallel is also equal to the equator.
  • Scale is true only along the equator.

Limitations

  • Distortion increases as we move towards the pole.
  • The projection is non-orthomorphic.
  • Equality of area is maintained at the cost of distortion in shape.

Uses

  • The projection is most suitable for the area lying between N and S latitudes.
  • It is suitable to show the distribution of tropical crops like rice, tea, coffee, rubber and sugarcane

Construct a conical projection with one standard parallel for an area bounded by  N to  N latitude and  E to  E longitudes when the scale is 1: 250,000, 000 and latitudinal and longitudinal interval is 

Construct a Conical Projection

Conical Projection with One Standard Parallel

A conical projection is one, which is drawn by projecting the image of the graticule of a globe on a developable cone, which touches the globe along a parallel of latitude called the standard parallel. As the cone touches the globe located along AB, the position of this parallel on the globe coinciding with that on the cone is taken as the standard parallel. The length of other parallels on either side of this parallel are distorted

Construction

  • Draw a circle or a quadrant of 2.56 cm radius marked with angles COE as  interval and BOE and AOD as standard parallel.
  • A tangent is extended from B to P and similarly from A to P, so that AP and BP are the two sides of the cone touching the globe and forming Standard Parallel at  N.
  • The arc distance CE represents the interval between parallels. A semi-circle is drawn by taking this arc distance.
  • X-Y is the perpendicular drawn from OP to OB.
  • A separate line N-S is taken on which BP distance is drawn representing standard parallel. The line NS becomes the central meridian.
  • Other parallels are drawn by taking arc distance CE on the central meridian.
  • The distance XY is marked on the standard parallel at  for drawing other meridians.
  • Straight lines are drawn by joining them with the pole

Properties

  • All the parallels are arcs of concentric circle and are equally spaced.
  • All meridians are straight lines merging at the pole. The meridians intersect the parallels at right angles.
  • The scale along all meridians is true, i.e.. distances along the meridians are accurate.
  • An arc of a circle represents the pole.
  • The scale is true along the standard parallel but exaggerated away from the standard parallel.
  • Meridians become closer to each other towards the pole.
  • This projection is neither equal area nor orthomorphic.

Limitations

  • It is not suitable for a world map due to extreme distortions in the hemisphere opposite the one in which the standard parallel is selected.
  • Even within the hemisphere, it is not suitable for representing larger areas as the distortion along the pole and near the equator is larger.

Uses

  • This projection is commonly used for showing areas of mid-latitudes with limited latitudinal and larger longitudinal extent.
  • A long narrow strip of land running parallel to the standard parallel and having east-west stretch is correctly shown on this projection.
  • Direction along standard parallel is used to show railways, roads, narrow river valleys, and international boundaries.
  • This projection is suitable for showing the Canadian Pacific Railways, Trans-Siberian Railways, international boundaries between USA and Canada and the Narmada Valley.
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