The Sea Floor Profiles And Scales

Science 277 1956 1962 1997 cas google scholar.

The sea floor profiles and scales. The ohaus vx series is a portable low profile floor platform and indicator scale package. Plate tectonics plate tectonics seafloor spreading. Ohaus vx series standard floor scale vx32xw10000x. Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.

Continental shelf 300 feet continental slope 300 10 000 feet abyssal plain 10 000 feet abyssal hill 3 000 feet up from the abyssal plain seamount 6 000 feet. After many profiles are made they can be assembled to create complex maps or three dimensional models of the seafloor by filling the spaces between the profiles using computer models or modeling. Long wavelength large anomalies 100 meters from the ellipsoid over thousands of km due to mass differences in the mantle many of which reflect older plate tectonics and remnants of subducted plates. The red line shows the sea floor depths and the green is the geoid anomaly.

Ocean literacy fundamental concept. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. A a featureless plain b a smooth descent with the deepest portions farthest from land c similar in rock type sediment thickness and erosional processes to those found on the land d containing ridges trenches seamounts and other features different from those found on land. The mid atlantic ridge for instance separates the north american plate from the eurasian plate and the south american plate from the african plate the east pacific rise is a mid ocean ridge that runs through the eastern pacific ocean and separates the pacific plate from the north american.

The landscape of the seafloor would best be described as. To map the seafloor research vessels cross the ocean making sonar profiles along carefully navigated parallel courses called transect lines. Seafloor mapping also called seabed imaging is the measurement of water depth of a given body of water bathymetric measurements are conducted with various methods from sonar and lidar techniques to buoys and satellite altimetry various methods have advantages and disadvantages and the specific method used depends upon the scale of the area under study financial means desired measurement. The earth has one big ocean with many features.

These age data also allow the rate of seafloor spreading to be. It is the ideal solution for freight consolidators forwarders processing plants resellers shipping and receiving departments as well as startup businesses. As upwelling of magma continues the plates continue to diverge a process known as seafloor spreading. The following features are shown at example depths to scale though each feature has a considerable range at which it may occur.