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Geology Study

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Geology Study

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À propos de cette activité

:) I hope this helps you study Idk what else to write here but it says my description is too short so I'mma keep on writing and writing and writing and writing, ok bye. :3

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Geology Study
 

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Geology StudyVersion en ligne

:) I hope this helps you study Idk what else to write here but it says my description is too short so I'mma keep on writing and writing and writing and writing, ok bye. :3

par bethany hinkle
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The mechanical and chemical processes that reshape the earth over time.

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Physically breaking objects into smaller pieces.

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Causing a chemical change to the composition or make-up of something.

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The grinding or wearing down of rock surfaces by power or other objects bumping against it.

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Water seeping into cracks in rocks and expanding when frozen.

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The grinding or wearing down due to wind blowing or pushing objects against each other.

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The grinding or wearing down due to water flow or pushing objects against each other.

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Combines with or draws out substances in the objects it touches, created by air pollution.

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When oxygen in air or water combines with substances to cause rust.

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When an object is broken into smaller pieces it increases the surface area.

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Increased surface area increases the rate of weathering.

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The removal of weathered material from one place to another.

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Involves both chemical weathering and erosion, where soil loses its nutrients.

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Wind, water, glaciers, gravity.

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A mixture of weathered rock, rock fragments, decayed organic material, air, and water.

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Increases the rate of weathering and soil formation (burrowing, roots, acid secretion).

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Moving masses of ice on land.

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Glaciers move because pressure from ice on top causes the ice on the bottom to melt.

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A mound of unsorted sediment that is deposited when a glacier moves.

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A mound of sorted or layered material deposited by a glacier.

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A sharp, fin-shaped ridge carved by two glaciers.

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A pointed mountain-shaped peak carved on at least 3 sides by glaciers.

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Rapid mass wasting of soil and debris downward.

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Rapid mass wasting of volcanic ash and water downward.

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Slow mass wasting of a large area of land downward.

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Material carried close to the bottom of a river.

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Material carried within the body of the river.

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Minerals and other substances leached out of soil into a river.

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The area of raised ground that separates one drainage basin from another.

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Area of land drained by a river system.

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Smaller streams or rivers that run into larger ones.

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The path that a river follows

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The amount of water that a river carries in a certain amount of time.

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The point where a river empties into another river or the ocean.

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A bend or curve in a river's channel.

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The material deposited by a river.

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An alluvium deposited into a body of water.

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Alluvium deposited on dry land.

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Where most deposition would occur in a river.

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River with high velocity, rapids, waterfalls, steep gradient, and few tributaries.

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River that is wide, slow, shallow, and has many tributaries.

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Sediment deposit behind the dam, erosion downstream, reservoir creation, earthquakes, and leakage.

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Water on the Earth's surface moving downhill in a channel due to gravity.

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Area of land drained by a river where all precipitation flows downhill in its channels.

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High, elevated land that forms the boundary of a drainage basin.

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A basin where no water flows out on the surface.

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Many small channels that merge into one large channel downstream.

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Irregular pattern common in permafrost and glacial deposit areas.

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Find the easiest way downhill, carry maximum sediment, reach base level, and reduce gradient to zero.

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The slope or angle of the river channel.

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Where a river stops being a river (velocity goes to zero).

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Volume of water moving in a channel (velocity × depth × width).

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Constant discharge; always has water flowing.

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Intermittent discharge; can be dry for large parts of the year.

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Base flow, bankful discharge, and dominant discharge.

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All sediment in the river channel (moving and stationary).

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Steep gradient, fast water, small discharge, coarse/poorly sorted bedload.

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Gentle gradient, slow water, large discharge, fine/well sorted suspension.

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Water moves along irregular pathways with vertical and lateral movement.

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Water moves along parallel pathways with no vertical or lateral movement.

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Impact of moving water, impact of sediment in water, and hydraulic lift.

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Solution, suspension, saltation, and traction.

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Measures how many pieces of sediment water can transport.

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Measures the maximum size of sediment it can transport.

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Occurs when water velocity drops, causing sediment to stop moving.

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Re-establish flow, remove/provide sediment, restore fish migration.

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Multiple small/wide/shallow channels, steep gradient, low/variable discharge, large bedload.

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One large/narrow/deep channel, shallow gradient, high/consistent discharge, small suspension load.

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Pile of sediment that divides flow into multiple channels.

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Where erosion occurs on the outside bend.

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Where deposition occurs on the inside bend.

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Moving to find the shortest/steepest path downhill.

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Old meander loop abandoned when the river forms a cutoff.

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Used to store excess water (short term) and sediment (long term).

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Braided (little floodplain, sudden); Meandering (wide floodplain, slow).

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"Bird Foot" delta; river grows into the sea.

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Has barrier islands and beaches at its front.

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Sediment reworked by tides into linear bars.

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More water in the system than the channel can hold.

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Raised bank that increases channel size/depth.

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Intense rains and rapid snow melt from warm temperatures.

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Described based on size and rate of past events.

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Liquid freshwater within sediments and rock below the Earth's surface.

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The sinking of surface waters and precipitation into the ground.

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High porosity and high permeability.

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Low porosity and low permeability (unless fractured).

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High permeability.

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Material through which water readily flows.

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May be permeable or impermeable (depending on connection of pores).

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An impermeable layer of rock or sediment

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Aquitard located above and below it.

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Pore spaces only partially filled with water.

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Mimics the land surface because flow rates are low.

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Rises during rain, sinks during drought.

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From greater hydraulic head to lesser hydraulic head.

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High concentrations of dissolved calcium and magnesium.

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Minerals in the aquifer rock that have dissolved.

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If it doesn't reach above ground, no artesian wells/springs exist.

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Flows on its own without a pump.

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Contains more dissolved salts and minerals than average groundwater.

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Example: Old Faithful; periodically ejects water/steam.

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Formed by pumping vast quantities of water locally.

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Sinking of land when pore spaces collapse after water table is lowered.

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Pumping faster than the aquifer can resupply.

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Saltwater contaminating freshwater in coastal communities.

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Unconfined aquifers are more likely to be contaminated than confined ones.

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Topography dominated by depressions from collapsed caves.

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Feature resulting from land collapsing into an underground cavern.

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Natural forces that change earth's surface.

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The hard outer layer of earth.

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Movement of plates below earth's surface.

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Formation and eruption of volcanoes.

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Break in the crust where magma erupts.

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Creation and movement of glaciers.

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Large piece of crust floating on the liquid Mantle.

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Created by folding of earth's crust.

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A break in the continuity of a body of rock.

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Surface line occurring at a break in the crust.

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Created when a block of crust tilts upward.

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A very large, unbroken area of land.

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Molten rock flowing out of a volcano.

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Narrow bottom valley formed by a river.

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Bits of soil/sand left by moving water.

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Flat bottom valley formed by a glacier.

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Sudden movement of ice/snow/rocks down a mountain.

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Huge ice sheets in extremely cold climates.

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24 regions coinciding with meridians.

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Where magma bursts through the crust.

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Deep underground collection of magma.

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Zone of activity around the Pacific Plate.

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Area where magma plumes rise (e.g., Hawaiian Islands).

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Oceanic plate dives beneath a continental plate.

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Converging, Diverging, and Transform.

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