No. According to scientific theory, tectonic plates of the lithosphere (the Earth's crust and outermost mantle) are below the ocean.
The crust, on which we live on, is like islands of tectonic plates that are floating on the semi-molten magma.
New ocean crust is formed at mid-ocean ridges where tectonic plates are diverging (spreading apart).
yes
Pieces of Earth's crust that are floating on the mantle are known as tectonic plates. These plates are rigid sections of the Earth's lithosphere that move and interact with each other, leading to phenomena such as earthquakes and volcanic activity.
The mid-ocean ridge is where new oceanic crust is formed as tectonic plates pull apart. This process, known as seafloor spreading, allows magma to rise from the mantle, solidify, and create new oceanic crust. As the crust forms at the mid-ocean ridge, it pushes older crust away, driving the movement of lithospheric plates.
Although it may be true that some misinformed people believe that land is floating on the water, it is FALSE that it does so. Land (earth's crust that is exposed to the air) could be said to be floating on MAGMA, along with the rest of the earth's crust. The oceans are above the crust, not under it.
Tectonic Plates are sections of the Earth's crust that are actually floating on the surface of the semi-molten Magma.
Large masses of Earth's crust floating on magma are known as tectonic plates. These plates move and interact with each other, leading to processes such as earthquakes, volcanic eruptions, and the formation of mountain ranges. The movement of these plates is driven by the heat and circulation of the underlying molten rock in the Earth's mantle.
The youngest oceanic crust can be found along mid-ocean ridges, where tectonic plates move apart and magma rises to create new crust. As the plates diverge, the molten rock solidifies and forms the youngest part of the ocean floor.
At a divergent ocean-ocean boundary, two tectonic plates move away from each other. This movement creates a gap or rift between the plates where new oceanic crust is formed through volcanic activity. Over time, the seafloor spreading results in the widening of the ocean basin.
The plates (continental and ocean plates) ride atop the asthenosphere, a layer of viscous rock in the upper mantle beneath the crust.
Volcanic action between the edges of tectonic plates are forcing them to move apart, and the plates are floating on the fluid, molten magma beneath the crust.