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72 Cards in this Set
- Front
- Back
were land and a body of water meet
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shoreline
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movement of materials by water
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erosion
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the accumulation of eroded particles
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deposition
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ripples on the water caused by wind
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waves
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groups of waves travelling together
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wave trains
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breaking waves
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surf
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can break solid rock and reposition the peoces
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pounding surf
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the intervals between breaking waves
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wave period
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any area of the shoreline made uo if materials deposited by waves
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beaches
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waves hit the beach at a slight angle but retreat perpendicular to the shore
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wave angles
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the movement of watetr near and parellel to the shoreline
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longshore current
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an underwater or exposed ridge of sand, gravel or shell material
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sand bar
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occurs when an exposed sand bar is connect to the shoreline
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barrier spit
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produces a variety of features along the shoreline
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wave erosion
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steep slopes form when waves erode and undercut rocks
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sea cliffs
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what is a type of alpine glacier
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valley glacier
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huge contenetal masses of ice that may form across and entire continent
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contentetal glaciers
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cover over millions of sq. km with ice. anarctica is an example
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contenetal ice sheets
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what is the largest type of contenetal glaciers
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contenetal ice sheets
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an area wher ice is attached to the ice sheet but is resting over oopen water
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ice shelf
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large pecies of ice that break of an ice shelf and drift into the ocean
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iceburg
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whats bigger an icebirg or a glacier
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glacier
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the process by which an icebirg is made
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calving
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what are the two ways an icebug can be made
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1)"rolling" bottom ice melts iceburg slips and rolls
2)"sliding" they ice crystals go ontop of another and then fall down slowly |
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a large crack that forms where the glacier picks up speed or flows over a high point
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crevasse
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sharp, pyramid-shaped peaks that form when 3 or more cirques erode the mountain
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horns
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bowl-like depresions where glacial ice cut back into mountains
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cirques
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jagged ridges that form between 2 or more cirques cutting into the same mountain
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aretes
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formed when a glacier erodes a river valley form its original "v" shape to "u" shape
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u shaped valleys
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smaller glacial valleys that join the deeper main valley
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hanging valleys
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grooves on rocks caused by glaciers
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straitions
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general term used to describe all materails carried and deposited by glaciers
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glacial drift
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rock material that has been sorted and deposited in layers by water flowing from melted ice
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straified drifts
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sorted material carried by streams flowing form the melting glacier that are deosited in a broad area in front of glaciers
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outwash plain
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depression left when a block of ice from the glacier is left in the outwash plain
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kettle
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unsorted rock material that is deposited directly by the ice when it melts
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till
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means that till is made up of different sizes of rock material ranging from large glaciers to fine glacial silt
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unsorted till
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form ridges along the edges of glaciers
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moraines
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form when two different valley glaciers with lateral moraines meet
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medial moraines
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a large crack that forms where the glacier picks up speed or flows over a high point
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crevasse
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sharp pyramidshaped peaks that form when3 or more cirques erode the moutain
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horns
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bowl-like deppressions where glacialice cuts back into the mountain wall
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cirques
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formed when a glacier erodes a river valley from its original v-shaped
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u shaped valleys
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smaller glacial valleys that join the deeper main valley
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hanging valley
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groves on rocks caused by glaciers
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striations
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form along each side of a glacier
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lateral moraine
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are the unsorted materials left beneath a glacier
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ground moraines
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form when eroded materials is dropped at the front of the glacier
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terminal morianes
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what are the 4 types of moraines
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medial, terminal, lateral, and ground moraines
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is the movenment of any material such as rock,silt or snow downslope
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mass movement
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the steepest angle or slope at which loose material will not slide downslope
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angle of repose
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a group of loose rocks fall down a steep slope
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rock slide
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the sudden and rapid movement of a large amount of material downslope
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landslide
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a block of material moves downslope over a curved surface, example of a landslide
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slump
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a rapid movement of a large mass of mud
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mudflow
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mudflows of volcamic origin
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lahar
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an extreamly SLOW movement of materials downslope
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creep
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priduces a variety of features on the shoreline
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wave erosion
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steep slopes that erode and undercut rock
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sea cliffs
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offshore columns of resistnat rocks that were once connected to the main land
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sea stacks
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form when wave action continues to erode a sea cave cutting completly through rock
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sea arches
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form when waves cut large holes waves erode and undercut rocks
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sea caves
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finger shaped projection that occurs when cliffs formed of large rocks erode slowly
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headland
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form when a see cliff is worn back producing a nearly level platform beneath the water at the base of the cliff
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wave cut terrace
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the movement of sand sized particles by a skipping and bouncing action in the direction of the win
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saltation
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the lifting and removal of sediment by wind
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deflation
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hard rocky surface consisting of pebbles and small broken rocks caused by deflation
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desert pavement
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wind blown depressiosn in the sand
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depression hollow
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the grinding and wearign down of sediments
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abrasion
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mounds of wind deposited sand
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dunes
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think deposits of wind blown sediments
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loess
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an enormous mass of moving ice
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glacier
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