MadSci Network: Earth Sciences |
Your question is both simple and copmplex. There are two basic ways to create a hill. One is to push or otherwise move the material that makes up the hill into place. Examples of this include everything from huge mountain chains such as the Himalaya, which have been pushed up by the collision of two continents, to morraines, which have been pushed up by glaciers, to coastal sand dunes, which have been piled up by the wind, to little piles of dirt that get heaved up by the frost in cold climates. The other way to make a hill is to remove all of the material that is not the hill. Erosion is constantly eating away at the landscape and some parts erode faster than others. That could be beacuse they are weaker, or because they are acted on by stronger erosive agents, but for whatever reason, if some part of the landscape is preferentially removed, what is left will likely stick up as a hill. In England, the latter is probably the case, as there hasn't been much tectonics recently, although they could be glacial as well. I'm afraid you'd need a local expert to answer the details (although glacial morraines are pretty obviously a mixed up mess of everything from clay to boulders). Hope this helps, Dave Smith
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