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31 Cards in this Set

  • Front
  • Back

velocity of sound through seawater


Rate is always

1.5 km/sec

Distance can be

depth or width

echo sounding

part of the ship's hull- most basic sonar method


sound generated by source then receiver on shippicks up echos



seismic reflection profiling

device is towed behind the ship


used to image layers of rock underneath the seafloor echos return from internal layers


ultrasound



Side scan sonar

"tow fish" towed from ship


black and white


rocky and sandy features

swath

like echo sounder


sweeps wider area wider area than echo sounder


more expensive

high frequency

gives detail

low frequency

gives depth

anticlines

when rocks are folded upward


(oil and gas trapped near axis of the fold)

synclines

when rocks are folded downward

abyssal hills

the majority of the oceanic province features


3-4km

abyssal plains

flat features


1: 1000


5-6 km

ridges

underwater mountain ranges



guyots

flattened seamounts

seamounts

volcanoes that don't break the surface

trench

deep crevice, >6 km

passive continental margins

shelf, slope, rise

active continental margins

shelf, slope, trench

beach to shelf break range

0-300m

depth world's ocean

3.7/3.8km

continental shelf

128 m


1:500

continental margin province

shelf, slope, rise

gradient

slope/steepness, ratio, rise/run

shelf break

300 m deep

two basic parts of crust

granite, basalt come together mid-slope

vertical exaggeration

x and y axis not on same scale vertical/horizontal- ratios

small scale

1: big number (wider area in view) country

large scale

1: small number (smaller area in detail) city

oceanic ridge province

continuous volcanic mountain chain >65,000 km 26% of earth's surface. Steep, rugged, seismic activity, extensive volcanism and high heat flow.

slope

300 m- 3 km


1:40

magnetic north

0 degrees. use for navigation in ocean