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78 Cards in this Set

  • Front
  • Back

Volcanic Explosivity Index

1-3: Strombolian


3-5: Vulcanian


4-7: Plinian

Lahar

Mudflow due to volcanic eruption

Fumarole

Vent where gas is emitted from a volcano



Vog

Volcanic air pollution

Maar

Volcanic lake

Basaltic Lavas

Divergent boundaries, hot spots (1k-2k C)


Shield volcano


Lava dome


Cinder cone


Large Igneous provinces

Andesitic/rhyolitic lavas

Convergent boundaries


High viscosity, silica content


Stratovolcano


Caldera

Stress

Force/Area

Strain

Amount of deformation expressed as a %


of distortion

Strength

Rocks break when stressed beyond their strength

Elastic Rebound Theory

Rocks deform elastically, then rebound during an earthquake rupture

Focus

Point at which the fault begins to slip

Epicenter

Point on earth's surface directly above focus

Foreshock, aftershock

small quakes before or after main quake

Moment magnitude

Fault area, avg rupture size

Modified Mercalli Scale

Shaking intensity based on ppl who felt quake

Shallow earthquakes

Mid-ocean ridges, transform faults

Range of earthquake depth

Shallow: 0-70 km


Intermediate: 70-300 km


Deep: 300-700 km

Benioff Zone

Zone of seismicity across a subduction zone

Intraplate earthquakes

Occur due to pre-existing stresses


From a pre-existing fault, fracking, or new fault formation

River authority

Public agency given authority to develop, manage the waters of the state. Can distribute water for the benefit of the public

Reservoir

Where is water stored?

Residence time

How long stored?

Chemical interactions

How does it react?

Transport

How long to transfer from one reservoir to the next?

Relative humidity

Amt. of water vapor in the air; how much water is in spaces between air molecules

Rain shadow

Area of low price caused by mtn. range

Drainage basin, watershed

Area of land where surface water converges to a single point at a lower elevation

Surface runoff

Water flow that occurs when soil is infiltrated to full capacity. Reservoirs, wetlands store runoff

Wetland

Wetland - land area saturated w/ water

Reservoir

Natural or artificial lake, storage pond, or


impoundment from dam

Dams

Benefits: Water supply, electricity, job development, manage water, hydropower, drinking water


Problems: transformed rivers, displaced people, debt burden, water quality

Aquifer

Formation that stores water underground

Aquiclude

Doesn't store water

Porosity

Percentage of total volume taken up by a rock's pores

Permeability

Capacity of a solid to allow fluids to pass through it

Vadose

Unsaturated zone of aeration

Phreatic

Zone of saturation

Perched water table/aquifer

Occurs in vadose zone; does not store large amounts of water, not good place for well

Recharge zone

Water enters aquifer

Discharge zone

Water exits here

Saltwater intrusion

Movement of saline water into freshwater aquifers

Unconfined aquifer

Water seeps underground; static

Confined aquifer

Aquiclude above and below; pressurized

Karst features

Caves, caverns, disappearing streams, sinkholes

Water stress

Measure of water availability in relation to population density

Eolian

Geologic processes powered by wind

Haboob

Intense dust storm

Annual precip less than 25 cm


Potential to evaporate more than falls


So little vegetation that cannot support abundant life

Desert requirements

Subtropical


Rain shadow


Coastal


Mid-latitude


Polar

Desert types

Desertification

Expansion of deserts into formerly productive lands

Playa

Desert lake

Climate


Pop increase


Over-exploitation of resources

Causes of desertification

Barchan


Blowout dunes


Transverse dunes


Longitudinal

Dune types

Ventifacts

Sand blasted rocks

Yardangs

Streamlined wind-eroded ridges

Wadi/arroyo

Dry lake or stream

Pediment

Mountain remnants surrounded by sediments

Glacial erratics

Large rocks carried by glaciers

Valley glaciers (alpine)


Continental glaciers (ice sheets)


Ice shelves (thick, floating ice slabs)

Types of glaciers

Shelf calves

Water-filled fractures carved thru ice shelf

Iceberg calving

Part of ice shelf falls off

Ablation

Glacial melting

Plastic flow

Laminar, ice crystals deform

Basal flow

Liquid water at base

Crevasses

Form where a glacier moves over steps in bedrock topography...and where it curves around topography

Till

Glacial Sediment; poorly sorted

Moraines

Piles of till

Permafrost

Permanently frozen soil/sediment

Pleistocene Era

When glaciers were around

Milankovich Cycle Theory

Changes in earth's movements controls climate

Eccentricity

Departure of its ellipse from circularity

Precession

trend in the direction of earth's axis of rotation relative to the fixed stars

Fossil fuels

Buried combustible geologic deposits; originally organic materials formed from decaying plants and animals

Rocks where hydrocarbons form


Shale/siltstone


Limestone


1-5% organic carbon content


T < 302

Ideal Source Rock

Rocks where oil from source rock can migrate


Porous/permeable


Well-sorted, coarse-grained sandstones


Cracked limestones


Porosity > 30%

Ideal Reservoir Rock



Impermeable rock that traps petroleum


Small, closely-fitting pieces of sediment


Shale


Holds petroleum for millions of yrs

Ideal Cap Rock



Aniticlinal Trap


Fault Trap


Stratigraphic trap


Salt Dome Trap

Types of Oil Traps