It is a curve which join highest point of the earth and lowest point of the the basis of this curve we can identify ocean reliefs as well as. The hypsographic (or hypsometric) curve is the representation of the statistical distribution of elevations over the entire world. In the areas which are covered. Hypsometry is the measurement of land elevation Bathymetry is the underwater equivalent. Hypsography of the Earth. Notice that A hypsometric curve is a histogram or cumulative distribution function of elevations in a geographical area.

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Hypsographic Curve

Our editors will curvve what you’ve submitted, and if it meets our criteria, we’ll add it to the article. In class, we created a hypsographic curve from a given bathymetric map of a lake ranging from feet in depth.

In the original paper on this topic, Arthur Strahler proposed a curve containing three parameters to fit different hypsometric relations: Using a square cutout of the scale representing 10, square meters and precise cutouts of the lake following each depth contour, the area at each depth was determined through a weight-area relationship 0.

Physical geography Geomorphology Fluvial geomorphology Geomorphology stubs Cartography stubs. This geomorphology article is a stub.

Upper Saddle River, NJ: Guyots are drowned volcanic islands that become submerged due to subsidence of the oceanic lithosphere. Abyssal hills more than 1 kilometer 0. There was a problem with your submission. At the bottom of the article, feel free to list any sources that support your changes, so that we can fully understand their context.

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Hypsometry – Wikipedia

Subsequent research using two-dimensional landscape evolution models has called the general applicability of this fit into question, [5] as well as the capability of the hypsometric curve to deal with scale-dependent effects. A hypsometric curve is essentially a graph that shows the proportion of land area that exists at various elevations by plotting relative area against relative height.

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In addition, Murray’s map gave birth to the idea of the Telegraphic Plateau, a submarine land formation from Canada to the British Isles, across which the first transatlantic cable was laid.

The abyssal plain is dotted with thousands of small, extinct volcanoes called abyssal hills. Contact our editors with your feedback. This steep embankment is called the continental slope and is grooved by submarine canyons and gullies.

The vertical dashed line marks the division between land and sea at present-day sea level.

The average width of a continental shelf is 70 kilometers 43 miles. Along the length of a typical subduction zone hypsographif deep-sea trench, a sheet of old oceanic crust is forced beneath continental crust. If you prefer to suggest your own revision hypsographif the article, you can go to edit mode requires login.

The Ocean Floor in Cross-Section The oceans begins, of course, at the shore, the irregular boundary where the surface of a continent descends first to sea level and then beneath it. Your turn – Contrast this to the deep ocean provinces — shown on the graph as a fairly flat slope and answer the questions below.

From this valley, new oceanic crust is constantly being extruded from Earth’s mantle by processes not yet fully understood. Medwin, Herman, and Clarence Clay. Retrieved from ” https: Earth Surface Processes vurve Landforms.

The cumulative hypsographic curve right hypslgraphic the percentage of surface area from the highest peaks to the deepest depths of the oceans. When high-resolution images are desired, an underwater unit may be towed behind a ship, scanning to the left and right with multiple sonar beams sidescan sonar.


Bathymetric mapping involves the production of ocean and sea maps based upon bathymetric data see historic map. However, unlike bathymetric maps, a hypsographic curve shows a relationship between elevation or underwater depth and the amount of Earth’s surface covered.

Archived from the original on The Hypsographic Curve The elevation features of the ocean floor—shelves, slopes, rises, plains, ridges, and trenches—are quantitatively summarized by oceanographers, along with the distribution of dry hypsographc at different altitudes, in a graph called the hypsographic curve see the figure. The curved line on the graph tells us about the provinces — where we see a change in the slope of the line, hypsographoc are looking at a different province.

Internet URLs are the best.

Ocean-Floor Bathymetry – river, sea, depth, oceans, percentage, types, system, effect

On other planets within this solar system, elevations are typically unimodalowing to the lack of oceans on those bodies. Not to be confused with Hypsometric tints.

Some features, such as mid-ocean ridges where oceanic crust is constantly produced and subduction zones, also called deep-sea trenches where it is constantly destroyedare unique to the ocean floor. Freeman and Company, Some continental margins are characterized by subduction zones, whereby oceanic crust is destroyed beneath the edge of a continental plate. The hypsographic curve shows the amount of Earth’s surface at various elevations and depths.

Newer Post Older Post Home. This gradual zone, which may be several hundred miles wide, is called the continental rise.