mountains
A graben forms when two normal faults cause valleys to drop down on either side of a block of rock. This landform is characterized by a depressed area between two parallel faults, with the central block lowered relative to the surrounding blocks.
Faults are fractures in the Earth's crust where rocks on either side have moved relative to each other. When this movement occurs, it can cause earthquakes, as the stress built up from the shifting rocks is released suddenly. Additionally, faults can create topographical features such as mountains, valleys, and plateaus due to the uplift or subsidence of the land along the fault line.
Mountain ranges are typically formed by compressional or convergent boundaries, where tectonic plates collide and cause uplift and folding of the crust. Valleys, on the other hand, can be created by various types of faults and processes, such as normal faults (resulting from tensional forces), erosion by rivers or glaciers, or subsidence of the crust.
A ridge is a narrow, elongated elevated landform that slopes downwards on both sides. A horst is a raised block of the Earth's crust bounded by faults on either side. In essence, a ridge is a continuous elevated feature, while a horst is a raised block that is bounded by faults.
Tensional stress occurs when layers of rock are pulled apart. This type of stress results in the stretching and thinning of rock layers, leading to the formation of features like rift valleys or normal faults.
A graben forms when two normal faults cause valleys to drop down on either side of a block of rock. This landform is characterized by a depressed area between two parallel faults, with the central block lowered relative to the surrounding blocks.
Yes, there are valleys on the surface of the Moon, primarily formed by faults, impacts, and volcanic activity. These valleys are known as rilles or grabens and are found in various regions across the Moon's surface.
Faults are fractures in the Earth's crust where rocks on either side have moved relative to each other. When this movement occurs, it can cause earthquakes, as the stress built up from the shifting rocks is released suddenly. Additionally, faults can create topographical features such as mountains, valleys, and plateaus due to the uplift or subsidence of the land along the fault line.
Mountain ranges are typically formed by compressional or convergent boundaries, where tectonic plates collide and cause uplift and folding of the crust. Valleys, on the other hand, can be created by various types of faults and processes, such as normal faults (resulting from tensional forces), erosion by rivers or glaciers, or subsidence of the crust.
trenches or mountains or rift valleys or faults depends which direction the plates move
A ridge is a narrow, elongated elevated landform that slopes downwards on both sides. A horst is a raised block of the Earth's crust bounded by faults on either side. In essence, a ridge is a continuous elevated feature, while a horst is a raised block that is bounded by faults.
Because they realy dont create any prominent geographical or geological feature/landform.
Yes, dip-slip faults can create mountains and valleys. When one block of the Earth's crust moves vertically relative to another along a dip-slip fault, it can result in the formation of mountains by uplifting one block and valleys by sinking the other block. The movement can be caused by compression (reverse fault) or extension (normal fault) forces.
Tensional stress occurs when layers of rock are pulled apart. This type of stress results in the stretching and thinning of rock layers, leading to the formation of features like rift valleys or normal faults.
The two types of faults that can result in mountains are thrust faults and normal faults. Thrust faults occur when older rock is pushed on top of younger rock, causing uplift and mountain formation. Normal faults occur when tensional forces cause one block of rock to drop down relative to another block, creating valleys and mountain ranges.
A transform fault or a strike-slip fault is formed when two tectonic plates slide past each other horizontally. This movement can lead to earthquakes due to the accumulated stress along the fault line.
Earthquakes occur along the faults, and volcanoes form where the magma reaches the surface. And from there it forms valleys.