HYPSOGRAPHIC CURVE PDF

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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Our editors will review what you’ve submitted, and if it meets our criteria, we’ll add it to the article. We read the hypsographic curve like a graph, with an x-axis horizontal and a y-axis vertical. Here, the ocean floor is marked by thousand-mile cracks called fracture zones that lie at right angles across the mid-ocean ridge. Not to be confused with Hypsometric tints. Principles of Physical Oceanography.

Most bathymetric maps show isobaths lines of equal depths as contours for the body of water.

Guyots are drowned volcanic islands that become submerged due to subsidence of the oceanic lithosphere. Your contribution may be further edited by our staff, and its publication cyrve subject to our final approval. This curve has been drawn to represent the total Earth and all of its oceans; likewise, curves can be constructed for each individual ocean….

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Posted by Leah Moore at 2: The abyssal plain, which is the deepest, most level part of the ocean, is found where the continental rise ends, at a depth of about 4 kilometers 2. The most popular type of bathymetric maps are ones on which lines of equal depths called isobaths are represented. If the depth of the ocean is measured along a line drawn cyrve out from a continental shore, the following sequence of bottom features are typically seen.

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Learn More in these related Britannica articles: For the first time, scientists knew what 70 percent of Earth’s surface really looked like radar, which produces images by bouncing radio waves rather than sound waves off distant objects, cannot be used for bathymetry because water absorbs radio waves.

However, unlike bathymetric maps, a hypsographic curve shows a relationship between elevation or underwater depth and the amount of Earth’s surface covered.

This page was last edited on 13 Decemberat Neumann, Gerhard, and Willard Pierson.

Hypsographic Curve | Article about Hypsographic Curve by The Free Dictionary

Help us improve this article! Introductory Oceanography, 9th ed. The disappearance of oceanic crust into subduction hypsograaphic is occurring primarily along the western, northern, and eastern edges of the Pacific Ocean. Keep Exploring Britannica Water. Then compare your response to the correct answer.

Along the center of the mid-ocean ridge is the rift valley, a deep V-shaped notch. There was a problem with your submission. Please note that our editors may make some formatting changes or correct spelling or grammatical errors, and may also contact you if any clarifications are needed.

If we look at the y-axis of the graph, we can see that continental margins are found from 0 to 4 km depth in the ocean. In the twentieth century, sounding lines were entirely replaced by sonar systems. In the hypsometric curve of the total Earth surface there exist two maxima of frequencies—at the metre yard and the 4,metre 5,yard elevations, which correlate with the mean level of the lowland continental areas and the deep-sea floor. Abyssal hills more than 1 kilometer 0.

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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 land at different altitudes, in a graph called the hypsographic curve see the figure. Continental shelves and slopes account for about another 15 percent, abyssal plains and mid-ocean ridge systems for almost 50 percent, and deep-sea trenches account for a small fraction.

These growing sheets of crust have the effect of forcing the distant continents farther apart, a process called sea-floor spreading. From Wikipedia, the free encyclopedia. Views Read Edit View history.

G115 – Introduction to Oceanography

This would be the case in crossing the Atlantic Ocean. The curve shows that a small percentage of Earth’s surface consists of high-altitude continental mountains, 30 percent of the surface consists of continental lowlands. The hypsographic curve shows what percentage of Earth’s surface rises above present-day sea level to a given height, or sinks below it to a given depth.

Beyond the rift valley, the depth sequence described above is observed in reverse: This flat, wide margin is found around every continent and is known as the continental shelf. The resulting curve is shown below in Figure 1. Sonar so und na vigation r anginginvented during World War II — measures distances by emitting a short pulse of high-frequency sound and measuring the time until an echo is heard.

This area is the flank of the mid-ocean ridge, a long, undersea mountain chain that usually extends down the middle of the ocean.