Young Red Haired Girl With Blue Eyes Undresses Her White Dress On Rocky Hill At The Sea

Hills may form through a number of geomorphic phenomena: faulting, erosion of larger landforms, such as mountains and movement and deposition of sediment by glaciers (e.g. moraines and drumlins, or by erosion exposing solid rock which then weathers down into a hill. The rounded peaks of hills results from the diffusive movement of soil and regolith covering the hill, a process known as downhill creep.
Areas that would otherwise have hills do not because of glacier cover during the Ice Age. The hills that existed before the ice age were worn down by the ice (and the rocks they carry) and/or the surrounding valleys and hollows were filled in with glacial drift, therefore leaving a level topography. The contrast between the flat plains of northern Indiana, once covered by ice, and the rugged hills of southern Indiana, where the ice never reached, is a result of this. Another example is the Driftless Zone, an island of hilly country that the ice sheets missed, surrounded by glacial plains, also in the American Midwest.
There are various specific names used to describe particular types of hill, based on appearance and method of formation. Many such names originated in one geographical region to describe a type of hill formation peculiar to that region, though the names are often adopted by geologists and used in a wider geographical context. These include:
• Drumlin – an elongated whale-shaped hill formed by glacial action.