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β 9y agoA Block Mountain.
Sister Little
This is called a strike slip fault.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
A strike-slip fault moves ground horizontally. This type of fault occurs when rocks on either side of the fault slide past each other horizontally. The San Andreas Fault in California is a well-known example of a strike-slip fault.
Fault-block mountains are formed when blocks of the Earth's crust are uplifted and tilted along a fault line, creating steep mountain ranges. Hot-spot volcanoes, on the other hand, are formed by volcanic activity at a fixed hot spot in the Earth's mantle, leading to the eruption of magma and the formation of volcanic peaks. Both types of mountains have distinct formation processes that set them apart from other types of mountains, such as fold mountains or volcanic arcs.
A Block Mountain.
A fault-block mountain is characterized by steep, rugged slopes on one side and a more gradual slope on the other. They are formed when tectonic forces cause a block of rock to be uplifted along a fault line, creating a mountain range with distinct asymmetric features. Examples include the Sierra Nevada in California and the Teton Range in Wyoming.
This is called a strike slip fault.
Where fault blocks collide into each other. The most prominent example of this are the Himalayan Mountains formed by the collision of the Indian plate and the Eurasian Plate making what is called a folded mountain.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
fault block
A reverse fault occurs when a portion of rock moves upward and over the other with a steep dip angle. This type of fault occurs in compressional tectonic settings where the forces push the rocks together, causing one block to thrust over the other.
When a fault is under compression, it may either become locked or slip, depending on the amount of stress applied. If the stress exceeds the fault's strength, it will slip and release energy in the form of an earthquake. If the stress is not enough to overcome the fault's frictional resistance, the fault will remain locked until enough stress builds up to cause slippage.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
strike-slip
The Sierra Nevada and the Tetons are among the mountain ranges formed by means other than tectonic movement. Many mountain ranges are formed by fault block shifts up and down as well as sculpting by erosion, volcanoes and glaciers. The mountains that we see are most often the result of many complex interactions over long periods of time.
A fault-block mountain forms where the edges of two plates come together to create a fault. When one plate pushes up over the other one, the upper one can continue up until it is high enough to create a fault-block mountain.