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5 Cards in this Set

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Bathymetry

Measurement of depth when mapping and charting the shape of the ocean floor. Bathymetric techniques use sound energy.

Echo Sounder (or Sonar)

(Sound, navigation, and ranging) Primary instrument for measuring depth. Invented in the 1920s, transmits a sound wave into the water to produce an echo when it bounces off an object, a clock measures travel time to fractions of a second. Distance(depth) is calculated with velocity of sound waves in water (1500m/sec): distance (depth)= velocity x time/2

High resolution multi beam Sonar

(Modern device) employs an array of sound sources and listening devices, obtains narrow strip of sea floor

Ophiolite complex

The structure of the oceanic crust and sequence of rocks.

Four layers

Layer 1: (top) unconsolidated sediments


Layer 2: consisting of pillow lavas


Layer 3: numerous interconnected dikes called sheeted dike complex


Layer 4: (bottom) gabbro