what is the differences between folding and faulting?
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The difference between folding and faulting is that folding is the pressure of converging plates causing the crust to fold and buckle, resulting in the creation of mountains and hills and faulting is where cracks in the earth's rock are created because of different movement of tectonic plates.
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As nouns the difference between fault and earthquake is that fault is a defect; something that detracts from perfection while earthquake is a shaking of the ground, caused by volcanic activity or movement around geologic faults.
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Weathering and erosion are processes by which rocks are broken down and moved form their original location. They differ based on whether a rock's location is changed: weathering degrades a rock without moving it, while erosion carries rocks and soil away from their original locations.
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The difference between cleavage and fracture is that cleavage is the break of a crystal face where a new crystal face is formed where the mineral broke, whereas fracture is the "chipping" of a mineral. ... If a mineral with cleavage is chipped a certain way, it will fracture rather than cleave.
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Joints and faults are types of fractures. A joint is a fracture along which no movement has taken place, usually caused by tensional forces. A fault is a fracture or break in the rock along which movement has taken place.
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A transform boundary is when two plates slide past one another. What is the difference between normal faults and rift valleys? Rift valleys are formed from normal faults. ... A boundary where rocks on opposite sides of the fault move in opposite or the same directions at different rates/speeds.
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In fault-block mountains, tectonic plates slide past each other to create the mountain. In folded mountains, the tectonic plates slam together, forming the peaks and valleys we see in many famous mountain ranges, such as the Himalayas, the Andes, and the Swiss Alps.
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A NORMAL fault moves because it is under tension. In geology a fault refers to a planar fracture in a rock volume, which has been displaced as a result of rock mass movement. There are three types of fault, they are: normal, reverse and strike-slip fault.
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Fracture is the characteristic way a mineral breaks. The difference between cleavage and fracture is that cleavage is the break of a crystal face where a new crystal face is formed where the mineral broke, whereas fracture is the "chipping" of a mineral. ... Uneven - A fracture that leaves a rough or irregular surface.
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Answer and Explanation: The reverse fault is the type of fault that is created by two faults under compression. It is a type of dip-slip fault and is the location of two...
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What is the difference between cleavage and fracture? Cleavage is when a mineral breaks in smooth, flat surfaces and fracture is when a mineral breaks and forms uneven surfaces.
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Anticlines are folds in which each half of the fold dips away from the crest. Synclines are folds in which each half of the fold dips toward the trough of the fold. You can remember the difference by noting that anticlines form an “A” shape, and synclines form the bottom of an “S.”
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In summary the Divergent and Convergent plate margins have similar and different topographical features that would have been formed or is still forming as a result of tectonic plate movement. The similarities are volcanoes and mountain ranges while the differences are rift valleys and ocean trenches.
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A normal fault occurs under tension, the hanging wall of the fault has been down thrown relative to the foot wall. A reverse fault occurs under compression where the foot wall has been down thrown relative to the hanging wall.
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Upwarped mountains are generally the result of broad arching of the crust or sometimes great vertical displacement along a highangle fault. ... Fault‐block mountains result from tensional stress. They are bounded by high‐angle normal faults, and usually form a series of horsts and grabens.
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The Formation of Fold Mountains Form along both destructive and collision plate boundaries, in other words where two plates are pushing towards each other. The best examples are the Himalayas, the Rockies, the Andes and the Alps, all of which are huge fold mountain ranges caused by the collision of two plates.
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Most earthquakes occur along the edge of the oceanic and continental plates. ... Earthquakes can also occur far from the edges of plates, along faults. Faults are cracks in the earth where sections of a plate (or two plates) are moving in different directions.