D.mesa mesa is table in spanish, technically mesa's arent supposed to have a slope.
With reference to its orbital plane the axis of the earth is tilted to about 66.5 degrees.
<h3>What is Earth's orbital plane?</h3>
The orbital of the earth is the flat and the disc part shaped part of the earth that connects all orbiting objects.
In the solar system, all of the planets in the world are known to have this same orbital system which they move around.
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Answer:
Following are the solution to this question:
Explanation:
Throughout layers called sheets or stratification were placed silicate minerals. Any formal credit with a uniform lithology or texture is defined as asleep. Beds are built on top of one another by deposition with disk diffusion.
Physical danger rocks characteristics:
- Bedding is also a sedimentary stone's most obvious feature. It comprises of language service as major corridors marking the boundaries of various layers of the earth.
- Grade grounds are popular when sediment does have a sluggish stream accumulated.
- Fossils, and Fractures and ripples of decomposition, etc.
H=88 G=92 K=91 M=89
How you solve this is G is the same thing as 92 because it crosses each other same thing with K. Then after that you just subtract 180 by 92 to get H because the line angle equals to 180 same thing with M
In general, what are the himalayan mountains composed of: folded and bent rock.
- The geology of the Himalayas is a record of the most dramatic and visible creations of the immense mountain range formed by plate tectonic forces and sculpted by weathering and erosion.
- The Himalayas, which stretch over 2400 km between the Namcha Barwa syntaxis at the eastern end of the mountain range and the Nanga Parbat syntaxis at the western end, are the result of an ongoing orogeny — the collision of the continental crust of two tectonic plates, namely, the Indian Plate thrusting into the Eurasian Plate.
- The Himalaya-Tibet region supplies fresh water for more than one-fifth of the world population, and accounts for a quarter of the global sedimentary budget.
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