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| develops adjacent to an intrusion. |
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| metamorphism due only to the consequences of very deep burial |
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| Occurs by shearing ONLY without requireing temp of pressure change. |
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| process of how buried rocks end up back at the surface |
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| repetion of planar surfaces or layers in a metamorphic rock |
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| dark & light layerd metamorphic rock |
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| non-foliated rock which depends on the composition of the protolith & the temp & the pressure od metamorphism |
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| hydrothermal metamorphism |
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| hydrothermal fluids rising to the crust of the ocean floor basalt |
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| metamorphism of limestone |
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| save conditions of slate, a protolith of conglomerate composition |
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| distinct belt of metamorphic rock that forms around an igneous intrusion |
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| metamorphic mineral assemblegas indicative of a ceratin range of pressure & temp |
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| parallel alignment of platy minerals of alterning light & dark colored layers |
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| the intensity of metamorphism, the amount or degree of metamorphic change |
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| new minerals that grow only under metamorphic change |
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| a pre-exisiting rock that underges a solid-state change in response to enviornmental change |
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| grains have grown in place within the solid rock |
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| regions between 2 isograds; zones are named after an index mineral that wasn't in the previous lower grade |
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| process of change by a solid-state in response to an environmental modification |
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| changing a rock's chemical composition b reactions with hydrothermal fluids |
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| a foliation that roughly parallels that fault |
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| fine-grained metamorphic rock witha foliation caused by the preferred orientation of very fine-grained white mica |
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| preffered mineral orientation |
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| alignment of inequant minerals in a rock |
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| pre-exisint rock; "parent" rock |
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| metamorphism of pure quarts sandstone |
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| metamorphism affecting a large region |
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| medium to coarde grained metamorphic rock with large mica flakes |
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| vborad region of long-lived stable continental where Phanerzonic sedimentary cover was not deposited or eroded away |
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| knife-edge ridge, seperated by two cirques |
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| water or wet slurry holds the glacier above the underlying rock |
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| bowl-shaped depression carved by a glacier ont he side of a mountain |
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| vast ice sheets that spread over continental crust |
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| large crack developed by brittle deformation in a glacier |
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| glacier flow molding till & sediment into streamlined, elongated hills |
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| sediment that reached the toe & forms a pile |
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| boundary between the zone of accumilation & ablation |
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| boulders that have traveled a long ways ontop of a glacier |
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| ridges of sorted sand & gravel that were deposited in subglacial meltwater |
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| valleys cut by glaciers that are filled with seawater |
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| glacier grows into previous unglaciated regions |
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| glacier moves back toward that orgiin of the glacier |
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| scratches of troughs carved into the rock by the sediment embedded in ice at the base of a flowing glacier |
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| sediment transported by ice & depositedd on, beneath, or at the toe of the glacier |
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| slowing flowing masses if ice that survive the summer melt |
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| a glacially carved tributary valley whose floor lies at a higher elevation than the floor of the trunk valley |
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| mountain peak surrounded by at least 3 cirques |
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| climate was signifcantly colder & glaciers grew |
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| a large block of ice that calves off the front of a glacier & drops into the sea |
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| a circular depression in the ground made when a bloack of ice calves f the toe of a glacier & become buired by till, & later melts |
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| strips formed along the side edges of a glacier |
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| layers of fine-grained sediments deopisited from the wind |
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| debri in a stripe running down the interior of a glacier |
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| climate cycles that occur over tens to hundreds of thousands of years, because of changes in Earth's orbit & tilt. |
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| piles of rocks & dirt-used by Alpine farmers |
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| a glacier that exists in or adjacent to a mountain region |
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| annual thawing & refreezing that splits the ground into pentagonal & hexagonal shapes |
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| the mass of ice slowly changes shape internally without breaking apart |
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| enhanced rainfall, lakes accumilated in low-lying land even at a great distance from the ice front |
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| atmospheric temp is so low that the glacier is well below the metling temp through out the years |
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| s hill's profile looks like a sheep lying in a meadow |
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| in polar climates sea surface freezes |
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| a glacier that exists in regions where it is warm enough for liquid water to occur in films between the grains of ice |
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| end moraine at the farthest linit of glaciation |
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| glacier that has flowed into the sea |
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| leading edge or margin of the glacier |
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| glacial abrasion & plucking lower the sides of the floor |
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| subtracts snow from glacier |
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