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Driving force behind Plate Tectonics. The heat transfer from the earths interior to exterior |
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Carved by Alpine Glaciers |
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Steep Walled, Bowl Shaped |
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Tributary valley that has been isolated by down cutting of the glaciers in the main valley |
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Jagged ridges along the divide produced by erosion of cirque or tributary glaciers |
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Parallel scratches show direction of movement |
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Slowest mass wasting (mm/year) Unconsolidated material moves slowly down slope under influence of gravity |
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Rapid slide of unconsolidated material |
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Material dissolves in water |
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Water chemically reacts with minerals and breaks them down |
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Large Cone shaped. Mt Rainer |
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Symmetrical and have deep craters at their summit |
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After a major eruption may collapse into the large, drained magma chamber below. |
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Right lateral Strike Slip |
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Single channels that form on steep to low slopes. Fast Flowing |
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Miultiple chanels that split and rejoin |
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bedding sediments at an angle to horizontal. Formed from wind or water |
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Bed progress from coarse grain at bottom to fine grains at the top |
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wave lines on the top of sand or silt by waves or currents |
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arrays of gashes at the surface of a bed formed when mud dries out and shrinks |
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Dendritic Drainage Pattern |
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pattern of branches connected to a trunk of a tree |
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surface of a cone shaped mountain and flow outward from the mountain peak |
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Rectangular Drainage Pattern |
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rectangular grid of fractures and channels form in pre existing fractures. Streams join at right angles |
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Earthquakes scales based on observed facts |
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What will happen to a glacier same accumulation as ablation |
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Glacier will remain the same |
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Intrusive igneous rocks eroded away |
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Short term Glacial Fluctuations |
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1. Eccentricity of Orbit 2. Tilt of Earths axis of rotation 3. Precession earths axis wobbles like a top |
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Most abundant mineral group in crust |
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