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The landforms that are formed at a transform boundary forms features such as fault lines and oceanic fracture zones. Fault lines are also known as strike slip faults. They produce powerful earthquakes.
Strike-slip faults Fault rupture of the ground generates vibrations-or waves-in the rock that we feel as the ground is shaking. Faults are weaknesses in the rock and therefore earthquakes tend to occur over and over along the same faults. Most major faults in the United States, particularly in California, are what are known as strike-slip faults. For strike-slip faults, the rupture is nearly vertical and during an earthquake one side slides past the other. The San Andreas fault is a strike-slip fault formed where two parts of the earth's crust (plates) slide past each other.
The surface feature formed when two plates meet is known as a fault. In some cases mountains can also be formed when two plates collide.
When electrons are transferred between two atoms a covalent bond is formed is known as an ionic bond.
Gneiss which is formed frm the metamorphism of ignous rock is known as orthogneiss and gneiss which is formed from the metamorphism of sedimentary rocks is known as paragneiss.
Strike-slip mountains, also known as fault-block mountains, form from high to moderate angle faults on at least one side. Broad uplifting forms the mountains causing elongation and faulting.
Mountains are formed at convergent plate boundaries or also known as fault lines.
The valley that forms between two normal faults is known as a graben structure. This may develop further into a rift valley and ultimately form a new mid ocean ridge.
The landforms that are formed at a transform boundary forms features such as fault lines and oceanic fracture zones. Fault lines are also known as strike slip faults. They produce powerful earthquakes.
The mountains which are formed by by the blocks earth's crust or rock-bed developed by the tensional forces and faulting are known as Relict Mountains.It is also known as Block mountains.
Strike-slip faults Fault rupture of the ground generates vibrations-or waves-in the rock that we feel as the ground is shaking. Faults are weaknesses in the rock and therefore earthquakes tend to occur over and over along the same faults. Most major faults in the United States, particularly in California, are what are known as strike-slip faults. For strike-slip faults, the rupture is nearly vertical and during an earthquake one side slides past the other. The San Andreas fault is a strike-slip fault formed where two parts of the earth's crust (plates) slide past each other.
Mountains formed from the buildup of volcanic lava often take this shape
Mountains formed from the buildup of volcanic lava often take this shape
The one mass of land known as Pangaea was formed In the Era Paleozoic, along with mountains, and land breathing animals.
Cracks in the Earth's crust are called faults. They are typically a result of the action of tectonic forces and may be the cause of earthquakes.
The surface feature formed when two plates meet is known as a fault. In some cases mountains can also be formed when two plates collide.
These mountains are formed out of the existing mountain i.e., Fold, Block or Volcanic mountains. High mountains are weared away by the agents of denudation i.e. wind, water, glacier, waves etc. The remaining part of these mountains is known as residual mountais.