The first thing to say is that there are two geographical features with the same name: the Rocky Mountain System and the Rocky Mountains (s.s.) that are part of it.The complete orographic system is something like a very varied sample of geological and tectonic processes.The system extends for more than 2982 miles, from Canada to the southern United States, (state of New Mexico). Its transverse extension varies between 68 and 300 miles, with the eastern edge being very close to Denver, and constituting a prominent feature within the central plains of the continent.The far west is not far from Salt Lake City, Utah, and is separated from the Sierra Nevada, Cascade, and Coastal chains-farther west-by the Great Basin and the Columbia River Plateau.The Rocky Mountains end before entering Alaska, not the System that contains them, which is also known to include the highest peaks in North America. In the United States, the highest height is recorded at Mount Elbert in Colorado, showing 4,401 m.s.n.m.Also in the Rocky Mountains is the watershed of the continent, which obviously separates the basins that drain towards the Pacific from those that drain towards the Atlantic.
Based on the meteorological analysis, the natural process in which the massive amount of material in the atmosphere halt or stops is known as the "GreenHouse Effect."
This is because GreenHouse Effect is a natural process that occurs in the earth's atmosphere.
The GreenHouse Effect occurs when Sun’s radiation comes in contact with the Earth’s atmosphere.
During the contact, some of the massive solar radiation is stopped or halted and returned to space.
The rest of this massive solar radiation, however, is taken and re-radiated by the greenhouse gases.
Greenhouse gases include water vapor, carbon dioxide, methane, ozone, etc.
Hence, in this case, it is considered that GreenHouse Effect is a significant occurrence or process in the Earth's existence.
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Europe and Asia are in the same landmass, like you can see in this picture.
Answer:
sedimentary rock
Explanation:
The fossils are found in sedimentary rocks such as sandstone, limestone and even coal. This type of rock tends to be in very deep layers and for this reason they are easier to house the fossils. they are formed by the melting of other rocks.
