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Yogita Ingle 5 years, 1 month ago
Features of Himalayan Mountains :
(i) The Himalayan mountains are the youngest mountains in the world. They are folded mountains.
(ii) They run along the northern border of India and form an arc which is around 2,400 km long.
(iii) Their width is up to 150 km in Arunachal Pradesh and 400 km in Kashmir.
(iv) They are the loftiest and the most rugged mountains.
(v) The altitudinal variations are greater in the eastern part than in the western part.
(vi) They form an arc.
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Yogita Ingle 5 years, 1 month ago
Apparently it is Bangladesh that shares the longest boundary with India, followed by China, Pakistan, Nepal, Myanmar, Bhutan, and Afghanistan (in descending order).
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Yogita Ingle 5 years, 2 months ago
Sinkholes are just one of many forms of ground collapse, or subsidence. A sinkhole is a depression in the ground that has no natural external surface drainage. Basically, this means that when it rains, all of the water stays inside the sinkhole and typically drains into the subsurface.
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Igneous rocks are those rocks which have been formed by the cooling and solidification of molten natural matter of the earth.
The igneous rocks are formed when magma cools and turns into solid forms. The process of the cooling and solidification can happen in the earth's crust as well as on the surface.
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Sia ? 3 years, 5 months ago
- A volcanic cone is a triangle-shaped hill formed as material from volcanic eruptions piles up around the volcanic vent, or opening in Earth’s crust. Most volcanic cones have one volcanic crater, or central depression, at the top. They are probably the most familiar type of volcanic mountain.
- A volcanic plateau is a plateau produced by volcanic activity. There are two main types: lava plateaus and pyroclastic plateaus.
- Lava plateaus are formed by highly fluid (runny) basaltic lava during numerous successive eruptions through numerous vents without violent explosions (quiet eruptions).
- Pyroclastic volcanic plateaus are produced by massive pyroclastic flows and they are underlain by pyroclastic rocks: agglomerates, tephra, volcanic ashes cemented into tuffs, mafic or felsic.
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Yogita Ingle 5 years, 2 months ago
Orogenic forces cause deformation of the Earth’s lithosphere and result in the occurrence of several geological processes. This process is called orogeny and can take place over a period of several million years. As a result, mountains get formed from the seabed or plains.
On the other hand, epirogenic forces cause depressions or upheavals of land with long wavelengths and broad ripples. This process is called epirogeny, and the result can be either transient or permanent.
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