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Why do the rocks at the top of a moutain peak weather faster the ones at the bottom
In most cases, yes. The more dense compound(s) will sink to the bottom, while the lighter (and for our purposes) less dense ones will stay near the surface. If you're speaking from a geological stand point,(eg. - sedimentary rocks) then no, most of the layering is NOT a product of different densities.
I don't know exactly what you mean. If you are asking about specific mountain ranges, some are: The Organ Mountains in Brazil Some of the Rocky Mountains in the West US If you are talking in general, the mountain ranges made of igneous rocks are the ones formed from volcanoes. For example: most of the mountains in Hawaii are made of igneous rock because the island themselves are formed by volcanoes.
Sedimentary and igneous are types of rock (the other type is metamorphic). Sedimentary rocks are quite soft, and include chalk and limestone. Igneous rocks include granite and basalt. They are formed when magma cools.
Yep, but just the really big ones
Why do the rocks at the top of a moutain peak weather faster the ones at the bottom
wet ones
Rocks are the ones which are usually made up of mixtures of different kinds of minerals. This is what defines the various properties that different rocks have.
Metamorphic rocks have really all and any mineral based upon different rocks. However common ones are quartz, mica, and calcium carbonate.
The heaver rocks settle to the bottom and the lighter ones stay on the top and they form layers!
Sedimentary rocks are ones formed by solidified mud and loose earth. Metamorphic rocks are ones formed by some sort of change, such as melting and re-cooling. So they are similar in some senses (they are both rocks, both of the earth) but in others they are very different (physical properties).
Sediment is brought to a location from different areas by water and wind. Of course there would be different ones at a different beach.
This applies to sedimentary rocks. If you think about how sediments settle to the bottom of water, then obviously newer ones are on top of old ones. As the weight of successive layers squeezes the lowest ones into rocks, the order of layers is preserved. This happens even if the layers are subsequently tilted. Very occasionally the order is disrupted if whole sections of rock are cracked away and inverted by earth movements. Igneous rocks are formed from molten magma, which can squeeze into cracks in existing rocks, so where igneous rocks are concerned, the argument doesn't apply.
Rocks are the ones which are usually made up of mixtures of different kinds of minerals. This is what defines the various properties that different rocks have.
Igneous Rocks, Sedimentary Rocks, SandStones, Cherts, and limestone.
In most cases, yes. The more dense compound(s) will sink to the bottom, while the lighter (and for our purposes) less dense ones will stay near the surface. If you're speaking from a geological stand point,(eg. - sedimentary rocks) then no, most of the layering is NOT a product of different densities.
The ones that are on the Moon will look the same. The ones that are on Mars will look very much the same. The ones that are on Earth will look completely different, or they may be gone altogether.