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53 Cards in this Set
- Front
- Back
2/3 million years ago maybe 45,000
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there was point mugu (land bridge to the channel islnads).
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250,000 YA
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sea level was 100-300 ft higher than today, and islands were under water
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30,000 YA
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oldest human culture associated with the islands
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12,000 YA
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people on islands and mainland, sea food gathers
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2,500-3,000 YA
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island chumash (canalino) culture began
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island undisturbed until 1542
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discovered by JR Cabrillo
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1812
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major earthquake occurred; santa rosa cracked the earth and ocean-->chumash moved to mainland
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1853
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juana maria found on san nicolas island and brought to mainland
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1938
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channel island national monument established
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1979
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channel island national park bill by bill lagomarsino
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1980 (March and May)
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Channel islands national park is official
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San Miguel
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northern most;sand-blasted and is 2/3 owned by military and has 6 species of pinniped
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santa rosa
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2nd largest; 30 miles north of SB and has air force base and cattle company, but now owned by national park
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santa cruz
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island of sacred cross. "back country" with 3 rivers. biggest cattle ranch resided here and is now part of the national park but with visiting permission
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anacapa
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2nd smallest and made of 3 igneous rock. east is camp grounds mid is off limits and west is an ocean.
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san nicholas
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island of blue dolphins. Juana maria lived. owned by navy. moving sand and heavu kelp beds and no one is allowed.
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santa barbara
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smallest, made of vegetation. like anacapa, but with elephant seals.
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santa catalina
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owned by the Wrigley family. 3rd largest, 34 miles from long beach. Use to be a women indian island and men were allowed only for sexual purposes. many endemic species
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san clemente
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last and 60 miles south of la harbor. off limits because ammunition all over the beach. use to be used for bootlegging.
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true-bony fin-fish
moray eel -gymnothorax mordax |
the california eel; pelagic spawner (long-lived). found in crevices of rocks and eats octopus, small fish and crustaceans at night
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true bony, fin-fish
northern anchovy, anchoveta and smelt |
make schools, which eat euphausiids, copepods and decapod larvae by filter feeding or pecking
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true bony, fin-fish
flat fish; halibut and flounder |
bilaterally symetrical at birth but eye migrates to left or right, have flat body and lay on floor, with top side similar to environment and bottom is white. feeds on sea urchins, and sand dollars
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senorita fish-oxyjulis californica
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important to algae bc they are scavengers; eat fish. they are gold in color with a black spot at tail
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garibaldi-hypsypops rubicundus
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male is terretorial and protects eggs. state fish because of hunting and is big and orange
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opaleye
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round body fish and drk gray colored body, white spot on one side of body. common in anacapa
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kelp bass (calico) Paralabrax clathratus
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white spots on top with black bkground and white on bottom. eat small fish like squid and plankton and the juvenile fish live in the kelp blades
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surf perch
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they are metallic with black band and live in the sand flats to be carried by water
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pile surfperch
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blk band on 2/3 of body and is closer to kelp forest
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black perch- embiotoca jacksoni (mesograzer)
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black lips with series of black stripes on body. nibble on macrocystis
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ca sheephead
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eats sea urchin, is protrandy (change sex) and female is pink with white chin and male is balck and red with knob on head
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kelp rockfish
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day looks dead, but at night its active.
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sunfish-mola mola
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live on outskirts of macrocystis. sit on side to get sun and is as big as table top. eat jellyfish and sml fish
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wolf eel
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eats sea urchins with no teeth.
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bathmetry
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measures the depth of the ocean (creates map of ocean) by echo sounders or fathometer
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mid-oceanic ridge
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does not have vertical magma, but magma releases outward. 8,000ft tall. discountinuities occur
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1 discontinuity
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off midline axis
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2 discontinuity
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off axis and now parallel to axis
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3 discontinuity
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different elevation because of spreding-->changes elevation
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4 discontinuity
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areas around the mid-oceanic ridge that is flucutaing
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island formation
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sea floor spreading and are created at the hot spot and then move and grow.
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topography
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physical features of the earths crust
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soundings
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depth recorded by fathoms taken by ship with two views; a depth profile (looking at peaks and valleys) or the contour map (bird-eye view of the bottom. all are recorded on a base map and translated to computer.
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isobaths
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lines of equal depth which create the countour lines.
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continental shelf
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extension of the continent lying under the water. usually 40 miles ca is like 110 miles
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continental slope
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drop off land at the end of the continental shelf.
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continental margin
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shelf and slope together, as part of the continents
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abyssal plain
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ocean floor about 16,000 ft below sea lefvel and mid-oceanic ridge is here which is not flat
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mid-oceanic ridge
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rise, 40,000 miles long and 8,000 ft tall. three main sections. mid-atlantic (1 in/ year), mid-indian and east pacific rise (3 in/yr)
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sea floor spreading
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created at the mid-oceanic ridge with older crust moving away from oirgin and new crust is created.
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continental drift
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or plate tectonics, which carry the continents with them.
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magma
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motletn crust while still beneath the earths thing crustal skin
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lava
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when it reaches the earths crust.
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fault-transfrom fault
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fissure in earths crust,where land on both sides slide and create the sea floor spreading. In the pacific plate is the san andreas fault.
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