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formed by volcanoes above/below ground |
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Formed by the cooling of magma in underground pockets of |
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rocks formed by lava cooling on the surface, forming small crystals |
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formed by collection of sediment pressured and cemented |
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formed by fragments of other rocks |
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volcanic rock broken+ ashy material |
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liquid evaporates and leaves minerals behind |
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made up of pervious living organisms |
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rock changed by pressure and heat
I.E; limestone into marble |
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Magma=Igneous=sediment=sedimentary rock=metamorphic=magma
cooling=weathering=compaction=heat=melting=cooling |
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evidence for continental drift |
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continents, ice, rocks, plants and animals all match |
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lithospheric plates move and magma floats into the ocean |
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3 types of contact betwen plates |
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convergent- push towards-make mountains
transform -push past- cause faults (san andreas)
divergent- pull apart- make oceans |
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deformation of the earth's crust via:
Faulting; breaking/slipping and sliding of crust
Folding; crust bends in wavelike ridges
upfolds;anticlines
downfolds;synclines |
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broken by faults
types of faults;
normal; one block goes over other
transform; two blocks slide apart
overthrust; one block goes over other |
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two forms of studing landforms |
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empirical; descrpitive; study shape, size angle of slope
genetical; study orgins; underlying rock mass, porcesses sculpting, stages of development
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what 2 opposing forces does genetic approach look at? |
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endogenic; forces from within
two basic forces; diastrophis; earths movement
vulcanism; magma
exogenic; wearing of lands from outside |
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magam cools under surface and forms large crystals |
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examples of intrusive igneous rock |
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batholith; huge mass made of granite 100 thousand miles large
laccolith; not as long as batholith
sill; horizontal flow of magma
veins; minerals that flow out the magma chamber
dikes; push way though other rocks
small doby of igneous rock introduced to older rock |
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extrusive igneous rock features |
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solidify in the open air quickly |
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volcanic crater caused by erruption causing lip to collapse |
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Pahoehoe is smooth and fast moving vs aa slow and roughness |
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formed by rising heat/magma causing rocks to mels and magma to subside leading eventaully to collapse |
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shallow basins marked by desert pavement surfaces |
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low ridges formed parralle to prevailing wind directions |
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sea of sand in which dunes- accumulations of sand that are shaped by wind actions- lie in |
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Barchans; crescent shaped/convex side facing agianst winds
Parabolic;cresent shaped facing wind
Transverse; right angle ridge straight or slightly curved
Longitudinal; parrallel to prevailing winds
Loess; dust laid down by wind after long distance blowing
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exogenic- on the surface- force
two types;
mechanical; disintegation
chemical; high temps speed process of chemicals |
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examples of mechanical-phyiscal- weathering |
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granular disintegration;
exfoliation; layers peel off; granite
block separation
shattering; ice in rocks break it; heating/cooling
unloading; rocks exposed and pressure realeased breaks them
slaking; clif under the cliff gets bigger and bigger; cliff drops
wedging; roots break rock
talus slope; rock pile fallen (35-37 angle) |
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chemical content of rocks has changed
ex; caverns/caves |
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lava cools and forms vertical columns |
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volcanic material; columnar joints: mechanical and chemical weathering |
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where is chemical weathering most common |
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more common in the tropics/warmer weather |
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carbon acid wears down rocks, calicium carbonate fizzes up and limestone is worn away leaving a cave |
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stalactites vs stalagmites |
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stalactites;from celing down
stalagmites; from ground up |
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mass wasting; erosin by strees/force of gravity
water
glaciers
waves/oceans aka coastal processes
wind |
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soil creep; slow movement of soil down slope(crooked fences)
solifluction; special soil creep with constant freezing/thawing; causes rocks
slump; large piece of land caves in and rotates down slowly
mudflow; dry climates mixed with water
alluvia fans; fan shaped deposit from a mountain by a stream
landslides; large amounts of mass slide in seconds
rock fall; weathered rocks drop to foot of a cliff
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caused by water runoff which comes from rain, flows into a creek, into a rivier into the ocean |
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raindrops dislodge soil particles making them easier to move for overland water flow |
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water moves as broad sheets over land |
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uniformed small grooves along slopes caused by run off |
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1st order; no tributaries
2nd order; two first order streams meet
3rd order; 2 second orders meet
4th order; 2 third order streams meet |
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number of streams found in an area
<12; course/low drainage density
12-16; medium
17-40; high
>40; badlands; badly eroded; soft/sandy/lack of veggies |
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valleys are created by streams |
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dendritic; tree like
trellis; trees out both sides
rectangular;like a rectangal
parallel; parralell to river
deranged;crazy
radial;reside out the middle
braided; like a braid |
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stream weathering; breaks rocks surrounding
stream transportation; erosion
deposition; where it ends |
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types of stream weathering |
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hydrolic action; forces water by pushing it against rocks
abrasion; water with small pieces rub over rock
corrosion; acid in water disoloves rock
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bed load; large rocks on the bottom
suspended load; little particels trans ported by water not always on top
solution; minerals dissolve and end up in ocean(causes the ocean to be salty)
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Young stream; v shape/no flood/deep valley
early youth;
late youth;
maturity;
rejuvenation; |
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small stream flows along floodplain and into a large waterway |
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formation of a delta; velocity of stream slows/gets clogged
arcuate delta; spread farther down the river (nile)
birds foot delta; forms in shallow water and spreads
cuspate delta; strong onshore current/wind pushes against the shore
Estuarine delta; bay gets filled and extends to flood plain |
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formed by a criclular wave, forms and moves toward the land |
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distance from top of one wave to another |
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forward movement of wave onto beach |
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water receding from beach |
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material transported down the beach |
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current that runs along coast- transports material |
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waves bend towards shore straightening as they progress |
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the portion of the bay that protrudes |
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small stump like stacks in ocean cut by waves |
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large peices of rock in the middle of the sea |
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deposit built up by longshore currents |
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spits streched across and seals off bay |
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straight on one side but cut on the other by currents from both directions |
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bar/spit that conects island with mainland |
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submergeence; land drops below sea level; irregular in shap
emergence; land below sea pushes up; straight
neutral; alluvial fans, deltas, corals; usually tropical |
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all; 68 F, shallow,, salty and clean
fringing reef; coral grows around island
barrier reef; coral grows over old coral skeletons |
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only circular portion of reefs remain- rasied/pushed up |
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it snows, turns to ice, soldifies as a glacier, slides down, reaches lake/ocean, breaks into icebergs, starts over |
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firnfeild; top
zone of accumulation; snow falws and accumaltes causing pressure
zone of ablation; more melting than accumulation
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depressions caused by glaciers plucking materials as they move
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what does glaciation cause
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moraines; deposits found at bottom of a glacier
medial moraines; two glaciers meet and the moraines join together
aretes; sharp ridges between 2 adjoining cirques
cols; pass through ridge
horns; riques coming up from 3 or 4 directions
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develop in mountains; restricted by this
cause tarns; like cirques minus the ridges
u shape valleys
waterfall valleys
truncate spurs; two or more glaciers leaving flat land around the hanging valley |
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limited; large land mass; created great lakes
wisconsin ice age; 10,000 years ago this happened
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most important source of non-salty water
calving; chunks of ice break off-float in the salt water
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forms near the end of the glacier
extensive fluvial featurs
smooth
desposits
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rocky debris depositied by moving/melting ice |
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long winding ridge left behind by glacier
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eggshaped hills
tells of glaciers direction
stoss side; direction from where it came
lee side; jagged rocks/plucked objects |
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smooth sides landform caused by moving ice |
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relatively steep sided mound composed drift/deposits and lef over ice sheet material |
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