terrane
The interior of the Indian subcontinent is hot and dry primarily due to its geographical location and topography. The region is situated away from the moderating influence of the ocean, leading to extreme temperatures, especially in summer. Additionally, the Himalayas block cold winds from the north, while the Thar Desert contributes to arid conditions. These factors combined result in high temperatures and low precipitation in the interior regions.
New kids on the block
The Secretary of Block Samiti in the village of India is called Sabhadhipati.
The duration of Attack the Block is 1.47 hours.
MSNBC Doc Block was created in 2006-07.
A terrane is a crustal block with a geologic history distinct from that of surrounding areas. They are often composed of a variety of rock types that were accreted to a continent during tectonic processes such as subduction or collision.
The Himalaya block the summer monsoon winds and redirectthe rainfall to the plains.
in places where earth crustal rocks are weak.
hot n dry
hot n dry
A fault-block mountain can be found in Death Valley, California and also in the Sierra Nevada mountains in California. Movement of large crustal blocks form fault-block mountains.
A fault-block mountain can be found in Death Valley, California and also in the Sierra Nevada mountains in California. Movement of large crustal blocks form fault-block mountains.
No, normal faults result in crustal extension, not shortening. Normal faults form as a result of tensional stresses that stretch the Earth's crust, causing one block of rock to move downward relative to the other block. Crustal shortening is typically associated with reverse faults or thrust faults, where compressional stresses push rocks together, shortening the crust.
The Himalayan Mountains act as a barrier preventing cold air from the north to enter India, leading to a milder climate in the northern regions. They also block the monsoon winds, causing heavy rainfall on the Indian subcontinent. The snow melt from the Himalayas contributes to the major rivers in India, supporting agriculture and biodiversity.
A crustal block that is downthrown with a steep fault scarp is typically referred to as a fault block. This geological feature is formed when a section of crust is displaced downward along a fault line, resulting in a steep, often visible, boundary. Fault blocks are common in areas with active tectonic activity.
The oldest landmass of the Indian subcontinent is the Peninsular Plateau, also known as the Peninsular India Plate. It is a stable block of ancient rocks that make up the southern part of India. The Peninsular Plateau has some of the oldest geological formations in India, dating back to over 3 billion years.
In the late 16th century, the Ottoman Empire was a major power in western Asia. The Mughal Empire ruled much of the Indian subcontinent.