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Rocks and Weathering ~ REVERSED

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the crust and upper mantle. Either solid or highly viscous, this layer is not easily deformed or manipulated
upper layer of the earth, divided into continental and oceanic crust
the layer of the earth between crust and core, the upper part is the lithosphere and the majority is the asthenosphere
the movement of continents across the surface of the globe
Continental drift
it occurs at constructive margins, where ocean floors grow as plates move apart
Sea-floor spreading
the movement of an oceanic plate beneath another crustal plate. As the plate reaches the asthenosphere it melts.
Subduction zones
long, narrow depressions in the ocean floor with depths of over 6000m
the decomposition and disintegration of rocks in situ
the disintegration of rock into smaller, angular fragments of the same rock, such as scree
Physical weathering
the decomposition of rock, creating altered rock substances, such as kaolinite from granite
Chemical weathering
when plants and animals chemically alter rocks and physically break them thorough their growth and movement
Biological weathering
when water in joints or cracks freezes at 0°C and expands by 10% exerting pressure on the rock
Freeze-thaw/frost shattering
alternate expansion and contraction of minerals in rocks causes the rock to break down into small pieces
Granular disintegration
when rocks split along joints into large rectangular shaped blocks
Block disintegration
found in hot desert areas where there is a large diurnal temperature range.
a type of disintegration where the outer layers of rock peel off due to stresses caused by heat
Physical weathering process where rocks are mechanically disintegrated by the accumulation of successive layers of water molecules in between the mineral grains of a rock
Wetting and drying
the decomposition of rock by solutions of salt
Salt crystallisation
overlying rocks are removed by erosion causing underlying rocks to expand and fracture
Pressure release
occurs on rocks with orthoclase feldspar
the process whereby certain minerals absorb water expand and change
when iron compounds react with oxygen to produce a reddish brown coating
acids dervived from the decomposition vegetation
Humic acids
the process in which plant roots can absorb relatively insoluble minerals
a rock consisting of calcium carbonate, therefore susceptible to carbonation-solution
a rock prone to hydrolysis because of the presence of feldspar
cave deposits such as stalactites and stalagmites
calcium deposits around springs
deposits of calcium carbonate which form from the top of caves
deposits of calcium carbonate formed on the base of the cave
large areas of bare exposed limestone containing clints and grykes
Limestone pavements
small-scale depressions in limestone pavement
Swallow holes/sinks
large depressions in limestone pavement up to 30m in diameter
these arise when the limestone is underlain by an impermeable rock
Resurgent streams
an important influence on slop development including faults, angle of dip and vulcanicity
Geological structure
a branch of geography that studies how different processes operate in different climatic zones to produce different slop forms or shapes
Climatic geomorphology
superficial and unconsolidated material found at the Earth’s surface
the direction in which a slope faces
any large-scale movements of the Earth’s surface that is not accompanied by a moving agent such as a river, glacier or ocean wave
Mass movement
the internal resistance of the slope
Shear strength
the forces attempting to pull a mass downslope
Shear stress
a slow, small-scale process of mass movement that occurs mostly in winter
the slow movement of fragments on a scree slope
Talus creep
mass movement that occurs on steep slopes, especially bare rock faces where joints are exposed
mass movement that occurs when an entire mass of material moves along a slip plane