Hilly land on the lower slopes of mountains is called
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hilly land on the lower slopes of mountains is called Block mountain
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Hilly land on the lower slopes of mountains is called valley.
Valley
- valley, extend sorrow of the Earth's surface. Valleys are generally normally depleted by streams and may happen in a somewhat level plain or between scopes of slopes or mountains. Those valleys created by structural activity are called break valleys. Extremely restricted, profound valleys of comparable appearance are called gorges. Both of these last option types are generally cut in level lying layers however may happen in other land circumstances.
- Any place adequate precipitation happens, the opportunity exists for the land surface to advance to the natural examples of slopes and valleys. There are, obviously, hyperarid conditions where fluvial movement is insignificant. There likewise are geomorphological settings where the penetrability of rocks or dregs instigates such an excess of invasion that water can't focus on the land surface.
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