nevado , lake thao, rocky mountain
In between mountains, inside mountain ranges.
The likely word is the plural noun "valleys."
Valleys What is a valley? A valley is a elongated lowland between ranges of mountains, hills, or other uplands, often having a river or stream running along the bottom. Are valleys useful? Valleys can provide shelter from harsh weather. Valleys also help with drainage. They can be dangerous to live in because of flash flooding. Where are valleys most likely to be found? In between mountains, inside mountain ranges. Examples: Sacramento Valley, Northern California Death Valley, Eastern California
Yes, Mercury has both valleys and mountains. Some of its valleys were likely formed by tectonic activity, while its mountains are thought to be the result of volcanic activity. Mercury's surface features are the result of a combination of tectonic forces and volcanic processes.
Yes, there are valleys on the moon called rilles or sinuous rilles. They are long, winding valleys that were likely formed by ancient lava flows or collapsed lava tubes. One of the most famous lunar valleys is Vallis Schröteri, located near the Aristarchus Plateau.
We do not know for certain at this time, but it is likely, since a perfectly smooth terrestrial planet is a near impossibility.
Thermal inversions are more likely to occur in valleys rather than on hills. This is because valleys trap cold air near the ground, preventing it from rising and mixing with warmer air above, leading to the formation of a thermal inversion.
Glaciers are least likely to be found in wide valleys due to the flatter terrain and lack of steep slopes needed for glacier formation and movement.
North Dakota and surrounding states
Valleys are most likely produced by erosion from running water, glaciers, or tectonic activity. These processes gradually wear away the land, forming a depression in the Earth's surface.
Fog can be especially prevalent in coastal areas, near bodies of water, and in valleys. These areas are more likely to experience fog due to the presence of moist air and temperature inversions that trap cool air near the surface.
On the plains of river valleys which were fertile and well watered.