Marine Provinces and Ocean Floor Topography Flashcards

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Vocabulary flashcards covering marine provinces, bathymetric mapping methods, continental margins, deep-ocean floor features, mid-ocean ridges, and hydrothermal vent types.

Last updated 1:37 PM on 9/8/26
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23 Terms

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Bathymetry

The measurement of ocean depths and the charting of the shape or topography of the ocean floor.

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Echo Sounder (Sonar)

The primary instrument for measuring ocean depth, invented in the 1920s, which calculates depth by reflecting sound waves off the ocean floor.

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Sounding

A historical method of measuring ocean depth using a line attached to a heavy weight, first performed by Poseidonus in 85 B.C.85\text{ B.C.}

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Fathom

A unit of water depth measurement equal to 1.8 m1.8\,m (6 feet6\text{ feet}).

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Hypsographic Curve

A curve showing the relationship between the height of land and the depth of the ocean across Earth's surface.

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Topographic Provinces of the Ocean Floor

The three major structural regions of the ocean floor: continental margins, ocean basin floor, and mid-ocean ridge.

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Passive Continental Margins

Coastal margins found along most areas surrounding the Atlantic Ocean that are not associated with active plate boundaries, experiencing little volcanism and few earthquakes.

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Continental Shelf

A gently sloping, flooded extension of the continent that varies in width from 70 km70\,km to 150 km150\,km and contains oil deposits.

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Continental Slope

A relatively steep structure with a slope of 1∘1^\circ to 25∘25^\circ that marks the seaward edge of the continental shelf and forms the boundary between continental and oceanic crust.

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Submarine Canyons

Deep, steep-sided valleys cut into the continental slope, some of which are seaward extensions of river valleys and most of which are eroded by turbidity currents.

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Turbidity Currents

Underwater downslope movements of dense, sediment-laden water that erode submarine canyons and deposit turbidites displaying graded bedding on deep-sea fans.

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Continental Rise

A gradual incline found in regions where deep-ocean trenches are absent, composed of thick accumulations of sediment deposited by turbidity currents forming deep-sea fans at the base of the continental slope.

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Active Continental Margins

Coastal margins where the continental slope descends abruptly into a deep-ocean trench, characterized by subduction zones, accretionary wedges, volcanism, and earthquakes.

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Accretionary Wedge

An accumulation of deformed sediment and scraps of ocean crust formed at subduction zones along active continental margins.

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Abyssal Plains

Extensively level places on the ocean floor extending from the base of the continental rise, formed by thick sediment deposits from suspension settling.

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Seamounts and Guyots

Isolated underwater volcanic peaks formed near oceanic ridges, where guyots represent flat-topped submerged volcanic features.

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Deep-Ocean Trenches

Long, relatively narrow features forming the deepest parts of the ocean where subducting lithospheric plates plunge into the mantle, closely associated with volcanic arcs.

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Mid-Ocean Ridge

An interconnected underwater mountain range spanning over 70,000 km70{,}000\,km (43,000 miles43{,}000\text{ miles}) and covering 23%23\% of Earth's surface, characterized by elevated topography (~2.5 km2.5\,km above seafloor) and extensive faulting.

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Ridge vs Rise vs Rift

Distinctions based on spreading rate and elevation: a ridge is slow-spreading and below sea level; a rise is fast-spreading and below sea level; a rift is slow-spreading and above sea level.

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Pillow Lavas

Basaltic lava structures with pillow-like shapes formed when molten basalt erupts underwater and rapidly quenches.

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Warm Water Vents

Hydrothermal vents on the seafloor with water emission temperatures below 30∘C30^\circ\text{C} (86∘F86^\circ\text{F}).

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White Smokers

Hydrothermal vents discharging water at temperatures ranging from 30∘C30^\circ\text{C} to 350∘C350^\circ\text{C} (86∘F86^\circ\text{F} to 662∘F662^\circ\text{F}).

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Black Smokers

Hydrothermal vents discharging dark, mineral-rich water at temperatures exceeding 350∘C350^\circ\text{C} (662∘F662^\circ\text{F}).