Difference between bhangar and khadar class 9

Hint: Bhabar, Bhangar, Khadar, and Terai are the names given to the different types of plains where humans have settled and accommodated themselves over a period of time. Complete answer: The names in the question are the different parts of the northern plains that lie between the Northern Mountains and the Deccan Plateau. The details of these plains are given as under: The Bhabar plains are located in the immediate foothills of the Northern Mountains and stretch from the union territory of Jammu and Kashmir to Assam in the northeast. It has vast deposits of gravel and large sediment deposits which have come from the glacial rivers originating in the Himalayas. It is not good for the production of food crops but can be highly beneficial for certain cash crops. Generally the vegetation found here comprises trees with large roots. The Bhangar soils are present in the alluvial tracts of Uttar Pradesh and Bihar and parts of Madhya Pradesh and Chhattisgarh. It has a very rich content of nutrients and is suitable for the growth of food as well as cash crops. The soil also has high humus content and lies in the regions that are not flooded by the rivers often. A notable feature of this type of plain area is the presence of calcium carbonate particles called kankar. The Khadar plains are formed due to the recent deposits of alluvium from the rivers. It mostly has clay, silt and sand and receives fresh deposits of sediments every year. Such plains are suitable for the cultivation o...

Difference between Bhangar and Khadar India has two types of soil: Khadar and Bhangar. Alluvial soils like the khadar type are typically found in river floodplains. It is an excellent soil for farming since it is fertile and abundant in organic matter. Bhangar soil, upland soil, can be found at higher altitudes. While it is frequently used for construction, the soil is less productive. Before we move on to the difference between Khadar and Bhangar, let us discuss alluvial soil. What is Alluvial Soil? The word "alluvial" comes from the Latin word "alluvius," which means "about a flood." It is related to the word "alluvium," which refers to sediment deposited by a body of water, such as a river or a flood . Alluvial soil is formed by sediment deposited by a river or flood. It is typically found in floodplains and river valleys and is high in nutrients and organic matter. Alluvial soil is fertile and frequently used for agriculture. It is also known for retaining moisture, making it ideal for irrigation. Alluvial soil can be made of various materials, including sand, silt, clay, and rocks. Alluvial soil is formed through alluviation, which occurs when a body of water, such as a river or a flood, carries and deposits sediment in a new location. As the water flows, it picks up soil, rocks, and other materials and transports them downstream. When the water slows down or comes to a stop, it drops the sediment it is carrying, creating a new layer of soil. Over time, this process c...

Differences between Bhangar and Khadar are- Bhangar Khadar The land covered with old alluvial soil is called Bhangar. The land covered with the new alluvial soil is called Khadar. It lies above the floodplains of the rivers. It lies near the rivers and in the flood area. Because the floodwater does not reach this plain,it is less fertile. Flood water reaches, so it is renewed every year andis fertile. It is less suited for agriculture. It is suited for intensive agriculture .

Khadar is more fertile than Bhangar: • Bangar is discovered away from the Ganga. • It has a high kankar knob convergence. • Its soil is relatively less ripe. • These areas have been depleted. • Bhangar soil is suitable for development. • The soil here is dark in color and rich in humus. • The Khadar plains are low-lying along a river. • Khadar areas are prone to flooding. • It includes former riverbeds that became available for agriculture. • Khadar soil is made up of new alluvial deposits and is frequently very fertile. • It is making them more fertile than Bangar soils.

Bhabar, bhangar, khadar and terai are the geological divisions of alluvial soils. • Bhabar: It is found in the foothills of Shivaliks. It is 8 to 16 kms wide . It comprises of pebble studded rocks and hence no rivers. It is not suitable for agriculture. • Bhangar: It covers large parts of northern plains. It is composed of old alluvial soil. It contains calcareous deposits locally known as 'Kankar' . Soil is not very fertile. • Khadar: Ii is also present in northern plains like that of Bhangar. It contains new alluvium. Used extensively for agriculture. • Terai: It is composed of comparatively finer alluvium and is covered by forests. It has underground streams and makes the area marshy. Suitable foragriculture.