The cool air from the ocean is forced up the mountain slopes, where it cools and condenses to form fog. This process, known as orographic lifting, occurs because the air on the ocean side of the mountain is moister and cooler than the air on the other side. As a result, coastal sides of mountains often experience foggy conditions.
A mesa is formed through a combination of geological processes such as erosion and uplift. Over time, the surrounding land erodes away, leaving a flat-topped mountain or hill with steep sides. The erosion-resistant top layer of rock is what forms the flat tabletop of a mesa.
Gravity is a property of a mass. Even you generate your own gravity field, though it is too small to be simply detected. So, as long as the mass exists, gravity will exist. In the 18th century, an experiment was made to determine the mass of the Earth. For this, the investigators measured the mass of a small mountain named Schiehallion in Perthshire. This experiment measured the deflection induced in a pendulum by the mass of this mountain. Measured on opposite sides of course, and consisted of measuring the apparent position (astronomical angle) of some stars. The difference between the two sets of measurements was due to the gravitation attraction of the mountain.
Fossil records of identical species found on different continents. Geological similarities in rock formations across continents. Matching coastlines and mountain ranges on opposite sides of continents. Distribution of similar species across continents, indicating they were once connected.
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The sun shines on the side that is facing towards it.
A flattop mountain is called a mesa. Mesas are elevated landforms with flat tops and steep sides, often found in arid regions.
A mountain gully is often referred to as a ravine. It is a deep, narrow valley with steep sides, typically formed by running water erosion.
a plateau.
The sides of a mountain are called slopes. These slopes can vary in steepness and play a role in determining the overall shape and characteristics of the mountain.
The correct term is a volcanic plug, which is a tall and narrow volcanic mountain formed around a vent with steep sides. They are often the solidified remnants of volcanic pipes that once transported magma from deep within the Earth to the surface.
plateau
windward and leeward side(:
a butte or a mesa.
Ghats
Sides of a mountain/ship/hill.
applacation mountains
Erosion.