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134 Cards in this Set

  • Front
  • Back

Biosphere

Context within which life exists

Population

A population comprises all the individuals of a given species in a specific area or region at a certain time

Communities

Community refers to all the populations in a specific area or region at a certain time and their interactions.

Ecosystem

Ecosystems are a self sustaining association of living plants and animals and their nonliving physical environment

Biome

large, stable, terrestrial or aquatic ecosystem classified by the predominant vegetation type and the adaptations to that environment.

Habitat

environment in which an organism resides or biologically is adapted to live.

Niche

function, or occupation of a life form in a given community.

Mutualism

associations between pairs of species that bring mutual benefit.

Parasitism

obtain food at the expense of their hosts and prey

Autotrophs

Produce their own food

Heterotrohps

Consumers; have to obtain food from outside source


Decomposers

Digest organic debris outside their bodies and release nutrients in the process


Photosynthesis

6Co2+6H2O+Sunlight=C6H12O6+6O2

Net Primary Productivity

Takes account for Loss.

Life Zones

Originally=Alexander Humboldt, Elevation


Modern= Hart Merriam, temp and Precip


Succession

organized change in community, from simple to complex


Primary Succession

establishment of plants on land that has not been previously vegetated

Secondary Succession

is the invasion of a habitat by plants on land that was previously vegetated.

Tropical Rain Forests

1.) Most diverse expression of life


2.) High Precip=ITCZ


3.) High Temp=Insolation


4.) Big Trees


5.) Cancer Drugs


6.) Half of all Species


Tropical Savanna

1.) Grasslands


2.) Almost half of surface


3.) warm


4.) distinct wet and dry


5.) scattered trees and shrubs


6.) Heterotrophs


7.) Xerophytes

Xerophytes

Have adaptations that help them conserve water

Deserts

1.) Hot and dry


2.) Continental


3.) Large Temp Variations


4.) Low Precip=Subtropical high


5.) Little biomass


6.) Succulents


7.) Jojoba


8.) atacama Desert

Succulents

thick, fleshy plant tissue, hold water well, needles for protection

Jojoba

Plant that you get oil from for shampoo, vertically oriented leaves-less transpiration


Atacama Desert

Dryest place on earth


Temperate Deciduous Forest

1.) Deciduous Trees dominate


2.) Coniferous Trees


3.) Common NA animals


Deciduous Trees

trees that lose their leaves, so they dont lose water


Coniferous trees

Evergreen trees- trees that do not lose their leaves, cant store as much water, less transpiration

Temperate Rain Forest

1.) High Rainfall


2.) High diversity


3.) Some of tallest trees in world


4.) Coastal RedWood


5.) Northern Spotted Owl

Coastal Redwood tree

largest trees in world, 30 stories high

Mediterranean Shrubland

1.) Hot Dry seasons=subtropical high


2.) Mild, wet winters=subpolar lows


3.) shrubland-short plant, multiple stems


4.) Schlerophyllous


5.) fires


6.) Santa Ana Winds

Schlerophylls leaves

small, hard, waxy leaves

Midlatitude Grassland

1.) Lower Precip


2.) Continental


3.) Steppe


4.) Great Plains


5.) Argentina-Beef


6.) Crops


7.) most heavily modified


8.) Tall and Short Grass


9.) Grasses dependent on fire

Tall Grass

deeper roots, eastward, wetter, being converted to farmland


Short grass

middle US, westward, dense leaves and roots

Boreal Forest (Taiga)

1.) Subartic


2.) Short summers, Long winters


3.) Precip=Snow


4.) Coniferous Trees Dominate


5.) Discontinuous Permafrost


6.) Cone Serotiny


7.) Giant Sequoia

Cone Seroteny

cones open, and release seeds in presence of heat and fire

Giant Sequoia

3000 years old, 810 tons in weight, similar to redwood


Tundra (Artic/Alpine)

1.) Short Summer, Long Winter


2.) Scarce trees


3.) shrubs, and low line vegetation


4.) Continuous Permafrost


5.) Few Deep Roots ^^^^


6.) low level of diversity


7.) Concern for melting permafrost

Earths Interior

1.) Thin Crust


2.) Upper Mantle


3.) Lower Mantle


4.) Outer Core


5.) Inner Core


How they came up with idea of earths interior?

1.) Magnetic field from iron core


2.) Path of seismic waves and ability to detect

Crust

1.) Thin shell


2.) Ocean Crust- more dense


3.) Continental Crust- less dense


4.) When they come in contact=ocean crust sinks beneath

Magma

molten rock


Igneous Rock

cooled magma


Sediment

weathering and erosion of igneous rock


Sediment Rock

sediment compacts


Metamorphic rock

sediment rock heated and pressurized


Plate Tectonics

1.) Earths crust is not 1 solid piece


2.) Alfred Wegener first proposed- Cont. Drift


3.) Rocks are same on different continents


4.) Species " " " " "


5.) coal in Anartica- formed by tropical plants


6.) Continental Drift

Pangea


1.) One large continent


2.) believe it split through millions of years


Magma

1.) Molten Rock


2.) Comes through cracks in earths surface


Lava

1.) when magma comes through earths surface

Ocean to Ocean Convergent

1.) Creates Volcanic Island Chains


2.) When ocean plates collide into each other


Ocean to Continent Convergent

1.) Ocean plates collide into land


2.) Creates long mtn Chains of Volcanic Islands on pacific coasts of America


3.) Ocean subducts under lighter cont. plate


4.) Trenches, volcanoes and Earthquakes

Continent to Continent Convergent

1.) Crustal plats converge


2.) Creates Earthquakes


3.) Mtn Range formed at plate boundries

Divergent Plates

1.) Plates Separate


2.) Volcano eruptions


3.) Plates move apart from each other


4.) Primary Succession potential


5.) Creates gap in surface

Pacific Ring of Fire

Ring of volcanic activity and seismic waves surrounding the pacific coast

Mariana Trench

1.) East of Phillipenes


2.) the deepest Trench in the world, over 7 miles

Hot Spots

1.) Holes where magma rises up


2.) How Hawaii Formed


3.) Individual sights of upward movements from the mantle


4.) Forms new Islands

Earthquakes

1.) Divergent plates creates stress


2.) When energy is released, called earthquake


3.) Epicenter


4.) Focus

Epicenter

1.) Point on Earths surface directly above the focus


Focus

1.) Point of origin of earthquake

Scales for Earthquakes

1.) Mercalli


2.) Moment Magnitude Scale

Mercalli Earthquake Scale

1.) Qualitive measure of how strong and amount of damage


Moment Magnitude Scale

1.) How to measure the amount of energy released


2.) Logarithmic scale


Tsunamis

1.) Harbor waves

How Tsunamis Form

1.) Plate boundary slips


2.) Earthquake happens


3.) Displaces Water


4.) Builds up as wave


5.) Hits shore and caused damage


6.) Hard to detect, bc they happen so fast

Volcanos

1.) vent that magma rises up out of and builds a mountain

AA Lava

1.) Jagged


2.) Sharp


3.) Thick Lava

Pahoehoe Lava

1.) Smooth


2.) Slow moving lava

Pyroclastic Flow

1.) Bits of pulverized rock and fire mixed together

Viscosity

1.) Resistance to flow


2.) Less viscous- less severe eruptions


3.) More viscous- more severe eruptions; it clogs vent, builds up pressure and explodes

Shield Volcano

1.) Less viscous lava


2.) Gentle sloped


3.) Effusive (not explosive)


4.) Hawaii

Cinder Cone

1.) Bits of hot rocks and clasts


2.) When they explode the rocks and clasts build up around vent


3.) Smaller


4.) Explosive


5.) Paricutin in Mexico

Stratovolcano (Composite Cone)

1.) layers of alternating cooled lava and clasts by stratification


2.) Mt. Fiji


3.) Explosive


4.) high Viscosity


5.) Magma and gas build up psi-explosive


6.) Often they are most Destructive

Caldera

1.) Huge Volcano


2.) Eruption is so violent that top of Mtn collapses into itself


3.) Craters in Lake Oregon

Explosive

The gasses build up to high psi, bc the magma rises to top then cools, blocking off vent, once enough psi builds up it explodes. More Viscous Magma

Effusive

Less viscous magma, not explosive


Weathering

1.) Breaking down of rock

Erosion

1.) Movement away of broken down rock

Physical Weathering


1.) Frost action/Freeze thaw


2.) Salt Crystal Growth


3.) Exfoliation

Frost action/Freeze thaw

1.) Water Gets in crack


2.) Freezes, then thaws


3.) Widens crack


4.) Forces Rock apart


5.) Increases surface area


6.) Microthermal climate, high elevation


7.) Layers of hard rock and soft rock


8.) Patterns in the Artic are example

Salt Crystal Weathering

1.) Water gets in rock along with salt


2.) Salt builds up into crystals


3.) Adds force to rock


4.) Slowly splits it apart


5.) Near oceans, and arid deserts


6.) Can make honeycomb looking things called tafoni's

Tafoni

Honey comb looking things on rock where salt crystal weathering has taken place. Happens near oceans.


Exfoliation

1.) Magma beneath surface rises


2.) Cools (pluton), making rock over head


3.) overhead rock causes over burden


Chemical Weathering

1.) Breakdown of rock due to chemical reaction


Oxidation

1.) Chemical breakdown of rock (usually metallic) w/ the presence of water.


2.) Makes red appearance (rust)


3.) warm, moist environment


Carbonation

1.) Chemical breakdown of rock from reaction of CO2 with water


2.) Produces acids that eat away rock

Mass Movements 4 types:

1.) Creeps


2.) Falls


3.) Landslides


4.) Flows


Driest_______________________________Saturated


Slowest


| Creep Flows


| Landslides Flows


| Falls Flows


Fastest

Creeps

1.) Gradual


2.) Mass movement of surface soil


3.) Soil Creep


4.) Occurs with frost action


5.) Human Activity, cattle


6.) dry


Falls

1.) Mass movement at faster rate


2.) little to intermediate water content


3.) Mtn Regions


Landslides

1.) Sudden, rapid movement of cohesive mass of bedrock that is not saturated with moisture


2.) High Rainfall


3.) Marine west coast

Mudflow

1.) Fast movement of rock and mud


2.) High moisture


3.) If this happens stay in car and buckle seat belt


Lahar

1.) Mudflow on a volcano


2.) Water from snow melted by heat from lave

Solifluction

1.) Slow moving of saturated soil in Artic


2.) Snow Melts


3.) Carries saturated soil away slowly

Scarification

1.) Humans are involved in mass movement


2.) Ore piled up that cannot use-Mine tailings

Fluvial

Rivers, streams, water flow, etc....


Drainage Basin

1.) Control what comes in and out of river basin


2.) Local Scale


Drainage Divide

1.) Dividing line between drainage basins


2.) Local Scale

Rills/Gullies

1.) Carved into landscapes


2.) Cuts into land


3.) Start at high elevation


4.) Flows down, cutting into land


5.) Water adds up, builds into streams

Discharge

1.) amount of water that flows through section per unit of time


2.) Help know how dangerous river are


3.) Helps estimate when and how large a flood


4.) Gullies merge-discharge becomes higher


5.) Faster river flows- more availability to erosion and weathering


6.) Dissolved Load- chemically weathered


7.) Suspended load- particles you can see


8.) Bed load- larger rocks

Dissolved load

chemically weathered


Suspended load

Particles you can see


Bed load

Larger rocks

Braided Stream

1.) No definite channel


2.) Areas with lots of sediments deposited


3.) Mud


4.) Chokes on sediment


5.) Mtn and Glaciers

Meandering Stream

1.) Single, Definite channel


2.) Each curve is a meandering


3.) Changes over time due to flooding, deposit.


Oxbow Lake

1.) Former Meander becomes isolated from the rest of the river


2.) When meandering stream curves meet


3.) Water takes shortest path


Point bar

1.) Where velocity is the slowest


2.) Where sediment is built up and deposited


3.) Builds little beach looking things


4.) usually on the inside of curve


Cut bank

1.) Bend in stream where velocity is highest


2.) Usually on the outside of curve

Delta

1.) Where river slows down and sediments are deposited


2.) High biodiversity


3.) Hunting and fishing is good


4.) Wetlands help to filter out Pollutants


5.) Example is Mississippi River delta

Alpine Glacier

1.) Mtn Glaciers


2.) High Altitude


3.) Form from gradual build up of snow


4.) Alps, Rockies, Hemilaya, Andies, Kilimenjaro

Continental Glaciers

1.) Large Area


2.) High latitude


3.) Antartica


4.) Greenland

Cirque

1.) Bowl Shaped formation


2.) Where old river or drainage basin was


3.) Moves down and converges to form large glaciers


4.) When they merge they make valley glaciers

Tidewater Glacier

1.) Valley Glacier that extends all the way to the ocean


2.) Front is suceptable to melting by ocean water


3.) Ice melts and breaks up-forming icebergs


Calving

1.) Breaking off and formation of ice bergs from tidewater glaciers

Valley Glacier

1.) Cirque glacier formed together were river was

Accumulation Zone

1.) Snow falls and accumulates


2.) weight increases and compresses into ice


3.) Starts to flow downhill


4.) Net gain if Accumulation is greater than ablation

Ablation Zone

1.) Rate of loss of ice is greater than gain


2.) sucseptable to melting


3.) Sublimation- ice to gas



Crevasses

1.) difference in psi in glacier


2.) Causes glacier to move at different speeds


3.) To relieve psi, makes break in glacier called a creavass

Plucking

1.) Act of picking up rocks and grinding along glacier


Abrasion

1.) the lines that rock form on glaciers from plucking


2.) Grinding on surface

Arete

1.) Sharp, knife like


2.) Form between Cirque


3.) Susceptible to more erosion


4.) If erosion occurs its called a Col

Col

1.) Where Arete is worn down


2.) Saddle shaped formation formed from eroded Aretes

Horn

1.) Sharp


2.) Triangular peak around cirque


3.) Sharp pyramid shapes around cirque

Hanging Valley/Waterfall

1.) Series of Cirque Glaciers meet with Valley Glaciers


2.) Valley Glacier cuts into rock deeper than cirque


3.) When they recede they make hanging valley, and often a waterfall

Fjord

1.) Type of Tidewater Glacier


2.) Flooded U shape Valley


3.) Carves out land till below sea level


4.) When glacier retreats it forms a Fjord, water then floods river bc its below sea level

Till (Glacial Drift)

1.) Rocks dropped by glacier


2.) Find braided stream bc lots of sediments


Erratics (Glacial Drift)

1.) Big boulders piled up by glacier


2.) after piled and become to large they drop

Moraines (Glacial Drift)

Small hills or mounds of till


1.) Lateral- forms side of glacier


2.) Medial- when lateral merge from valley glacier


3.) Terminal- farthest extent glacier has reached.

Lateral Moraine

1.) Forms side of glacier


Medial Moraine

1.) When lateral moraine merge from two valley glaciers

Terminal Moraine

1.) Farthest extent glacier has reached.


2.) Picks up till and drops it at bottom

Freeze Thaw Causes

1.) Rock Falls in Mountains


2.) Rocks Splitting


3.) Patterned Ground in Artic


4.) Cracked and Pothole Roads

Salt Crystal Growth causes

1.) Niches in Canyons


2.) Tafonis


oxidation Causes

1.) rust


2.) red soils