SHORT ANSWER TYPE QUESTION:
Q1.If a person is to travel to Lakshadweep, from which coastal plain does he prefer and why?
Answer
The person will prefer to travel from the western coastal plains because the Lakshdweep islands are situated in Arabian Sea which distance is lowest from this coast. Therefore, it will take the least time to reach the Lakshadweep.
Q2. Where in India will you find a cold desert? Name some important ranges of this region.
Answer
The cold desert in India is located in the north eastern part of the Kashmir Himalayas, which lies between the Greater Himalayas and the Karakoram ranges.
Q3.Why is the western coastal plain is devoid of any delta?
Answer
The western coastal plains are narrow and have steep slope. The rivers flow rapidly in one part and hence they don’t form any deltas. Therefore, the western coastal plain is devoid of any delta.
Q4.Make a comparison of the island groups of the Arabian Sea and the Bay of Bengal.
Answer
Island groups of the Arabian Sea | Island groups of the Bay of Bengal |
This island group consists of about 36 islands of which 11 are inhabited. | This island groups consist of about 572 islands/islets. |
These are situated between 8°N-12°N and 71°E -74°E longitude. | These are situated roughly between 6°N-14°N and 92°E -94°E. |
The entire group of islands is broadly divided by the Eleventh degree channel, north of which is the Amini Island and to the south of the Canannore Island. | The entire group of island is divided into two broad categories – the Andaman in the north and the Nicobar in the south. |
The entire island group is built of coral deposits. | These islands are an elevated portion of submarine mountains. |
Minicoy is the largest island with an area of 453 sq. km. | The two principal groups of islands include the Ritchie’s archipelago and the Labrynth island. |
Q5.What are the important geomorphological features found in the river valley plains?
Answer
The river valley plains are formed by the alluvial deposits brought by the rivers. The important geomorphological features found in the river valley plains are:
• Bhabar is a narrow belt ranging between 8-10 km parallel to the Shiwalik foothills at the break-up of the slope.
• Terai: South of the Bhabar is the Tarai belt, with an approximate width of 10-20 km where most of the streams and rivers re-emerge without having any properly demarcated channel, thereby, creating marshy and swampy conditions known as the Tarai.
→ This has a luxurious growth of natural vegetation and houses a varied wild life.
• Bhangar: It is composed of old alluvium. These areas are less prone to flooding and less fertile as well.
• Khadar: It is composed of new alluvial deposits. These areas are prone to flooding and are very fertile
• Delta: A river delta is a landform that occurs at the mouth of a river near where the river flows into the ocean. For example, the famous Sunderbans delta.
Q6. If you move from Badrinath to Sunderbans delta along the course of the river Ganga, what major geomorphological features will you come across?
Answer
Badrinath is situated along Ganga river. The Sunderban delta is on the mouth of Ganga and Brahmaputra in Bay of Bengal. If we are moving from Badrinath to Sunderbans delta along the course of the river Ganga, we will come across various of geomorphological features. As we start moving we will come across gorges, V-shaped valleys, rapids, waterfalls, etc. We will also see places where tributaries meet main river Ganga. After sometime, we will enter into northern plains. We will see various erosional and depositional landforms such as sand bars, meanders, oxbow lakes and braided channels. At last, we will reach our destination, swampy and marshy area known as Sunderbans delta formed by the Ganga and Brahmaputra river.
Long Answer Type Questions:
Q1.Write a detailed on Kashmir or north-western Himalayas.
Answer:
Kashmir or North-western Himalayas:
- Region extents over Jammu and Kashmir, Himachal Pradesh and Uttaranchal.
- It comprises of Ladakh, Zaskar and Pir Panjal.
- The north-eastern parts of Kashmir Himalayas is a cold desert which lies between greater Himalayas and Karakoram ranges.
- Between Pir Panjal and Great Himalayas in Dal Lake and Valley of Kashmir.
- Important Glaciers here are:
- Siachen
- Baltora
- Babura
- Hispar.
- Kashmir valleys are known for Karewas. Karewas are thick deposits of glacial clay and other material embedded with moraines (Zafran-Saffron is cultivated here):
- Important passes: Zoji La on the Great Himalayas, Banihal on Pir Panjal range, Photu La-Zaskar range, Kharaung La on Ladakh range. Thadala, Nitila, Lepulekh in Uttaranchal Nathula in Sikkim in Himachal Pradesh.
- Himalayas are spread between river Indus to river Mahi. The total extent of western Himalayas is 700 km and 400 km in width.
- Kashmir Himalayas, Punjab Himalayas and Kumaon Himalayas are its sub¬division.
- The important lakes are: Dal lake and Wular lake (in Jammu and Kashmir and they are freshwater lakes), Pangong Tso, Tso Moriri ( they are salt water lakes and they are situated in Jammu and Kashmir.
- Important rivers: Indus, Jhelum and Chenab.
- Important pilgrimages Vaishno Devi, Amaranth and Charar-e-Sharif.
- The southernmost part of the region has longitudinal valleys known as Duns, e.g. Jammu Dun and Pathankot Dun.
Q2.Explain the characteristics or features of Northern plains?
Answer:
The Northern Plains-
- These plains extend approximately 3,200 from the east to the west.
- The average width of these plains varies between 150-300 km.
- The maximum depth of alluvium deposits varies between 1,000-2,000 m.
- The area covered by northern plains is 7 lakhs square km and is most densely populated region of country.
From north to South, these plains can be divided into three sub divisions: Bhabar, Tarai and Alluvial Plains. The alluvial plains can be further divided into the Khadar and the Bhangar.
Bhabar
- It is a narrow belt ranging between 8-16 km parallel to the Shiwalik foothills at the breaking of the slopes.
- The streams and rivers coming from the mountain deposit heavy materials of rocks and boulders and at times, disappear in this zone.
Tarai
- Its approximate width is of 20-30 km where most of the streams and river re-emerge without having any properly demarcated channel, thereby, creating marshy and swampy condition known as the Tarai.
- It has a luxurious growth of natural vegetation and houses a varied wild life.
Alluvial Plains
- These plains have characteristic features of mature stage of fluvial erosional and depositional landforms such as sand bars, meanders, ox- bow lakes and braided channels. The Brahmaputra plains are known for their riverine islands and sand bars.
- The mouths of these mighty rivers also form some of the largest deltas of the world, for example, the famous Sunderbans delta.
- These river valley plains have a fertile alluvial soil cover which supports a variety of crops like wheat, rice, sugarcane and jute, and hence supports a large population.
Q3.Explain the physical features of coastal plains.
Answer:
On the basis of the location and active geomorphological processes, it can be broadly divided into two:
- The western coastal plains;
- The eastern coastal plains.
The western coastal plains are an example of submerged coastal plain. It is a narrow belt and provides natural conditions for the development of ports and harbours. Kandla, Mazagaon, JLN port. Navha Sheva, Marmagao, Mangalore, Cochin, etc. are some of the important natural ports located along the west coast.
Extending from the Gujarat coast in the north to the Kerala coast in the south, the western coast may be divided into following divisions – the Kachchh and Kathiawar coast in Gujarat, Konkan coast in Maharashtra, Goan coast and Malabar coast in Karnataka and Kerala respectively. As compared to the western coastal plain, the eastern coastal plain is broader and is an example of an emergent coast.
There are well- developed deltas here, formed by the rivers flowing eastward in to the Bay of Bengal. These include the deltas of the Mahanadi, the Godavari, the Krishna and the Kaveri. Because of its emergent nature, it has less number of ports and harbours. The continental shelf extends up to 500 km into the sea, which makes it difficult for the development of good ports and harbours.
It is believed that the city of Dwaraka which was once a part of the Indian mainland situated along the west coast is submerged under water. Because of this submergence it is a narrow belt and provides natural conditions for the development of ports and harbours. Kandla, Mazagaon, JLN port Navha Sheva, Marmagao, Mangalore, Cochin, etc. are some of the important natural ports located along the west coast.
Q4.How are Arunachal, Himachal, Purvachal and Uttaranchal Himalayas different from each other?
Answer
Arunachal Himalayas
- These extend from east of Bhutan to Diphu pass in East.
- Important peaks are- Kangtu and Namcha Barwa.
- They are bisected by fast flowing rivers forming deep gorges.
- Brahmaputra flows through deep a gorge after crossing Namcha Barwa.
- Subansiri, Dihang, Dibang and Lohit are the important rivers. Perennial rivers have high rate of fall which helps to generate hydro-electricity.
The Himachal and Uttarakhand Himalayas-
- It lies between river Ravi and Kali in the east.
- Northernmost part is the extension of the Ladakh desert.
- All these ranges Nimadi, Himachal and Chivalric are prominent here.
- Hill stations are Dharamshala, Mussoorie, Shimla, Ranikhet and Almora.
- Shiwaliks are important for dun formation. For example- Kalka dun, Nalagarh dun (Dehradun is the largest- dun, its length is 35-45 km and width is 22-25 km.)
- Tribes common are Dhotia’s which migrates to higher region in summer.
- Valley of flowers- Nanda devi is also situated here.
- Gail’s, the Manipur Pilgrimages common are Kedarnath, Badrinath, Hemkund Sahib.
The Eastern Hills and mountains or Purvachal.
- General alignment from the north to south direction.
- In north, they are known as Patkai Bum, Naga hills, the Manipur hills and in the south, as Mizo or Lushai Hills. This forms Purvanchal range.
- Most of these ranges are separated from each other by numerous small rivers.
- The barak is an important river in Manipur and Mizoram.
- Mizoram has a large lake known as ‘loktak lake is made up of soft unconsolidated deposits.
- Mizoram and Manipur are tributary of Barak river, which is the turn tributary of Meghna rivers in eastern part of Manipur are tributaries of Chindwin which is in turn is a tributary of Ireawady of Myanmar.
Q5.Differentiate between:
(i) Bhabar and Tarai
Answer:
Difference between Bhabar and Tarai.
Bhabar | Basis | Tarai |
It lies along the foot of shiwalik from Indus to Tista | Location | It lies to the south of Bhabar and runs parallel to it. |
It is 8 to 16 km wide. | Width | It is 20-30 km wide. |
It comprises of pebbles studded rocks in the shape of porous bed. | Composition | It is composed of firmer alluvial particles and is covered by forests. |
Due to the porousity of rocks the stream disappear and flow underground. | Appearance | The underground streams of Bhabar reappear here giving rise to a wet marshian. |
It is not suitable for agriculture. | Suitability | It is reclaimed for agriculture purpose. |
(ii) Bhangar and Khadar
Answer:
Difference between Bhangar and Khadar
Bhangar | Basis | Khadar |
It is a highland composed of old alluvium. | Composition | It’s a lowland composed of new alluvium. |
It is always above the level of flood plains. | Flood | It is flooded almost every year. |
It comprises of canvanious nodules | Fertility | It comprises of clay soil which is normally fertile |
It is not much suited for agriculture. | Suitability | It is suited for agriculture. Intensive agriculture is practiced. |
It is known as dhaya in Punjab. | Other name | It is known as bate in Punjab. |
(iii) Western Ghats and Eastern Ghats
Answer:
Difference between Western Ghats and Eastern Ghats;
Western Ghats | Basis | Eastern Ghats |
They form continuous chain from Gulf of Combay to Kanniyakumari. | Location | They form a discontinuous chain of low hills from Odisha to Coromandel coast. |
They are having an elevation of 900-1100m. | Peaks | They are denuded peaks and have lesser elevation than 900 km. |
They are divided as four regions or the four hills Sahyadri hills in Maharashtra, Nilgiri in Karnataka and Tamil Nadu, Anaimalai hills and Cardamom hills in Kerala. | Hills | Some of the important ranges include the Javadi hills, the Palconda range, the Nallamala hills, the Mahendragiri hills, etc. |
The western ghats get southward monsoon. | Rainfall | The eastern ghat gets rainfall from north-east monsoon. |
The highest peak in western ghat is Anamudi (2695 m) | Highest Peak | Highest peak of eastern ghat is Mahendragiri (1501 m) |
The height of the mountain increases from north to south. | Change in height | Height increases from south to north. |
The westward flowing river are Narmada and Tapi. | Rivers | Eastward flowing rivers are Godavari Krishna, Kaveri, Mahanadi, etc. |
(iv) Peninsular Plateau and Indo-Gangetic Plateau
Answer:
Difference between Peninsular Plateau and Indo-Gangetic Plateau
Peninsular Plateau | Basis | Indo-Gangnetic Plateau |
It is triangular plateau bounded by Vindhyas western ghats, and eastern ghats. | Stretch | It is alluvial plain stretching from Punjab to Assam valley. |
The relief of this plateau is uneven. Its average height is more than 600 m above the sea level. | Level | This is a level plain for about 200 m in height above the sea level. |
The climate is hot and humid. | Climate | The summers are hot and winters are cold. |
Kaveri, Krishna, Godavari, Mahanadi, Narmada, Tapi are seasonal rivers. | Rivers | Ganga, Yamuna, Brahmaputra are perennial rivers. |
Area has black soil. | Soil | Alluvial soil is found. |
Known as storehouse of minerals and important for industries. | Known for | Known for agriculture and provide employment to people. |
(v) Western Coastal Plains and Eastern Coastal Plains
Answer:
Difference between Western Coastal Plains and Eastern Coastal Plains
Western coastal plain | Basis | Eastern coastal plain |
They lie between western ghats and Arabian sea. | Location | They lie between eastern ghats and bay of Bengal. |
They are narrow alluvial plain which are separate by hilly terrains. | Width | They are wider plain (80-120 km) with well developed deltas of the rivers. |
The western coastal plains are further divided into two parts: Konkan coast, Malabar coast | Furtherclassification | They are further divided as northern circus and Coromandel coast. |
They are known for lagoons estuary and kayals (backwater), which are known for fishing and Inland transportation. | Known For | They are known for deltas formed by the rivers and is more suitable for agriculture. |
They receive rainfall from southwest monsoons. | Rainfall | They receive rainfall by retreating or north-west monsoon. |
The important rivers are Narmada, Tapi | Rivers | The important rivers are Krishna, Kaveri, Mahanadi, etc. |
They are submerged coast. | Merging | They are emergent coast. |
(vi) Northern Plains and Coastal Plains
Answer:
Difference between Northern Plains and Coastal Plains
Northern Plains | Basis | Coastal Plains |
They are located on foot hills of Himalayas and above peninsular plateau. | Location | They lie between Arabian Sea, Western Ghats and Eastern Ghats and Bay of Bengal. |
They spread between the area of 3200 square km and the width is 240-320 km. | Stretch | They are spread from Gujarat to Kanniyakumari and Odisha to Kanniyakumari. |
Rivers originating from Himalayas and peninsular plateau has form these plains by depositing sediments brought by rivers. | Rivers | Most of the rivers originating from peninsular plateau like Krishna, Kaveri, Godavari, Mahanadi move eastward and form delta whereas Narmada and Tapi move westward from Estuaries. |
Due to fertile alluvial soil and water supply they are known for agriculture. | Suitability | They are drained by perinial rivers and are important for fishing, lagoons, and harbours. |
They are divided as Indus plains, Ganga plains and Brahmaputra plains. | Divisions | They are divided as Konkan coast and Malabar coast, Northern Circar on eastern side and Coromandel coast. |
They are important for riverine features like natural leaves, sand bars, etc. | Known for | They are important for ports, harbours, kayals and backwaters. |
(vii) Himalayas and Central Highlands
Answer:
Difference between Himalayas and Central Highlands
Himalayas | Basis | Central Highlands |
They are the young fold mountains of comparatively recent origin. | Young vs. Old | They are part of oldest structure of Indian subcontinents. |
They are the world’s highest mountains and the Mount Everest is the highest peak of the world. | Height | They are formed of low hills and no high peak is there worth mentioning in the area. |
The mighty rivers like Indus, Ganga, Brahmaputra originate beyond the Himalayas. | Rivers | Quite a few rivers like Tapi, Chambal, Betwa, Narmada, originate from these highland. |
They are made up of sedimentary rocks. | Composition | They are formed by Igneous and metamorphic rocks. |
They are formed at the edge of northern plains. | Location | They are formed at the edge of Deccan Plateau. |
Important hill stations are Srinagar, Shimla, Dhalauzi, Dharamshala, Mussoorie, etc. | Hill stations | They are no well-known hill stations. |
Himalayas are known for glaciers and perennial rivers. | Glaciers and rivers | No glaciers and non- perennial river are there. |
They have beautiful passes and river valleys. | Scenicbeauty | They are low-lying hills with less common features. |
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