oldest
The crust is the thickest under mountain ranges, up to 70 miles. Average depth of continental crust is 27 miles.
Sediments become thicker away from the mid ocean ridge. This is because the oceanic crust away from the mid ocean ridge is older than the crust close to it, so sediment has had more time to accumulate.
the thickest accumulation of sediment on the ocean floor is at the CONTINENTAL SLOPES AND RISES. :)
At ocean spreading ridges, new oceanic crust is formed. The magma that forms this new crust emerges from the ridge and pushes the pre-existing rocks away from the ridge laterally. This results in a strip of new rock cutting through the older rock. As formation of the crust continues, the older rocks will be pushed further away from the ridge, while younger, newly produced rocks will occupy the area closest to the ridge.
In an ocean-continent convergence, the collision of ocean and continental crust causes the accretion of marine sedimentary deposits to the edge of the continent. These sediments, then, are forced up through normal mountain building orogenic uplift and compression (and faulting). In another method, as the underlying oceanic crust area of a plate tips down at a subduction zone, its ocean-floor sediment can be scraped off along the front edge of the overriding continental plate. The result is an increase in the width and thickness of the overriding plate, and thus, a mountain range. This is seen well at the convergence of the Nazca plate and South American plate (Peru-Chile Trench or Atacama Trench) forming the Andes Mountains - which are actually originally volcanic in origin, but are being buttressed by the new sediments.
To investigate the evolution of ocean basins by core drilling of ocean sediments and underlying oceanic crust.
The Earth's crust is thinnest under the oceans and thickest in the mountains.
The crust is the thickest under mountain ranges, up to 70 miles. Average depth of continental crust is 27 miles.
Sediments become thicker away from the mid ocean ridge. This is because the oceanic crust away from the mid ocean ridge is older than the crust close to it, so sediment has had more time to accumulate.
Trenches... I don't know why, but I'm 100% sure it's correct!
the thickest accumulation of sediment on the ocean floor is at the CONTINENTAL SLOPES AND RISES. :)
Ocean sediments are deposits of materials(organic or in-organic) at the substractum of the ocean.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
The Earth's oceanic crust is very thin at the mid-ocean ridges, and gradually thickens as it moves away from the ridges. The continental crust is thickest under mountain ranges. The average depth of oceanic crust is around 5 miles. The average depth of continental crust is 22 miles.
The thickest part of the South American tectonic plate lies below the Andes Mountains. They were created from the compression of the South American plate with the Nazca Plate and the Antarctic Plate.
The ocean is never pulled under the continent. Oceanic crust--the rock and some sediments, however, slide under the edges of continental crust and are pushed downward toward the mantle in areas of oceanic to continental plate collisions.