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53 Cards in this Set

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