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The igneous rock underlying the deep ocean basins is basaltic, as its source material comes from the asthenosphere. Andesitic igneous rock is formed at colliding plate margins, where subducting oceanic crust is partially melted and undergoes differentiation as it rises through the continental crust. Granitic rock is less dense than oceanic crust and composes the continents.
The continents are thicker and less dense than the materials that make up the ocean basins.
They don't. The presence of magma at mid-ocean ridges is due to the effect of less pressure on the mantle below known as "decompressional melting". Mantle rock is extremely hot, yet it remains in solid state because it is under immense pressure. At mid-ocean ridges, where tectonic plates are pulling apart, the crust is thinner, meaning less pressure on the mantle rocks below, thus they are able to melt, become less dense and rise.
The depth of water at the apex of the ridge is less than 2,700 metres.
The cold would affect it from growing in the deep water and depending on how deep the it would receive less and less sunlight which it needs to grow
Mantle convection works to uplift rocks at mid-ocean ridges where they are exposed to less overburden and therefore, less pressure. As the pressure decreases, the rocks begin to melt.
Mining on land is less costly than mining in the deep ocean because it takes more equipment to go down to the bottom of the ocean, and all of that equipment costs more money than what they use on land.
By average wave size, the Arctic Ocean, since for most of the year it is covered by pack ice, and the average depth is less around the continents.
The further down, the less sunlight is able to penetrate into the darkness.
I think that it causes a deep ocean current.....
Deep ocean currents have enormous effect on climatic conditions. Deep ocean currents are also known as conveyor belt for temperature. There are two types of water currents, cold and warm. The warm water currents are less dense than cold water currents.
On average, continents are older than ocean basins. Due to the action of plate tectonics, ocean crust is being formed and destroyed continuously. The oldest oceanic crust is about 200 million years old, whereas continents, which are less dense than oceanic crust and tend not to be subducted into the mantle, can be more than 3,000 million years old in places.