Rilles
The valleys on the moon are called rilles. They are long, slender depressions that may have curved or twisting shapes. They may be caused by collapsed lava tubes, cooling lava flows, or parallel crustal faults.
The valley that runs through western Kenya is called the Great Rift Valley. It is a geological feature that extends from the Middle East to Mozambique, with various branches and lakes along its length. The Great Rift Valley is known for its diverse landscapes, wildlife, and importance in human evolution.
Another name for a lunar valley is a rille. These are long, narrow depressions on the moon's surface that can be several kilometers wide and hundreds of kilometers long. Rilles are believed to have formed through a combination of volcanic and tectonic processes.
Ah, Mercury's surface is quite rocky and covered in craters, kind of like a painting with lots of texture. You can also see long cliffs and pockmarks from meteorite impacts - it's all quite beautiful in its own rugged way! Just imagine yourself hiking those lunar landscapes, with each little detail telling a story of our Solar System's history.
The valley which lies between River Mahabharata and Churiya Range is called inner terai.
Drainage system
One of the features that make up the earth's surface, such as a plain, mountain, or valley.
This is known as a meandering river. Meandering rivers have a sinuous flow pattern characterized by smooth, curved banks and slow lateral erosion that gradually widens the valley over time.
A basin is a depression in the earth's surface that can be dry or filled with water.
When the crust splits and a valley is formed, it is called a rift or a rift valley. This process commonly occurs as a result of tectonic plate movements and can lead to the formation of new land features such as mountains and valleys.
California's central valley natural features
the genesee river follows a meandering course...take a look what the river looks like on google image.
A deep crack in the earth's surface is a fault It can also be a joint.
Such valleys are typically formed by sediments carried and deposited by meandering streams over time. The slow and lateral movement of meandering streams creates a wide, flat valley floor as they continuously deposit sediment along their banks. These types of valleys can often be found in regions with low gradients and high sediment loads.
what is the phisical features of willamette valley
Wide streams and valleys are typically characterized by large amounts of sediment deposition, broad and flat valley bottoms, and gentle slopes. They may have meandering channels and alluvial plains along their banks. These features are often associated with low-energy flow conditions and are conducive to agriculture and settlement.
The Yangtse Valley, Indus Valley, Tigris Valley, Euphrates Valley, Nile Valley.