A convergent plate boundary is where one of the plates is sinking beneath another, and the other one is being pushed on top of the subducting plate. This is called a subduction zone. This happens when denser, heavier oceanic crust meets less dense, thicker, continental crust.
When two plates converge, and one is less dense, that plate goes under the more dense plate into the mantle, this is called subduction.
subduction will happen and a volcano will be formed. when one plate slides beneath another one magma from earths mantle is being pushed up on earths surface.
Sinks and toilets are most often made of porcelain.
It sinks. By pressing it under the water, the water pressure on the balloon increases slightly and compresses the air in the balloon. This increases the density of the (balloon, weight) combo so that is more dense than water, hence it sinks. High altitude weather balloons are only inflated partway with helium when they are launched from the ground. The envelope of the balloon expands as it rises in the atmosphere.
One of the trendiest varieties of bathroom sinks are vessel sinks--these sinks have a free-standing bowl that is mounted to a countertop, reminiscent of old wash basins. These are available in glass, porcelain, cast iron, and even marble. For fixtures, brushed nickel is the trendiest finish.
Actually you are wrong, its vise versa, hot water rises and cold water sinks. This is because when water molecules gain energy, they become hot. Molecules try to move away from one another. And this leads to reduction in density. Since density of water reduces as it becomes hot, how water moves up and cold water sinks down.
it is heated by the ground , and becomes less dense and rises i found that in my science book I'm in 6th grade
Trenches are typically found at the boundaries of tectonic plates, where one plate is being subducted beneath another. The most well-known trenches are oceanic trenches, found underwater near subduction zones where one tectonic plate sinks beneath another.
a destructive plate boundary
In an oceanic-oceanic subduction boundary, one oceanic plate subducts beneath another oceanic plate. This process can result in volcanic island arcs being formed. In an oceanic-continental subduction boundary, an oceanic plate subducts beneath a continental plate. This can lead to the formation of volcanic mountain ranges on the continental plate.
The boundary where one tectonic plate is subducted beneath another is called a convergent boundary. In this zone, the denser oceanic plate typically sinks into the mantle beneath the less dense continental or oceanic plate, leading to geological features such as deep ocean trenches and volcanic arcs. This process can result in significant seismic activity, including earthquakes and volcanic eruptions, as the plates interact and stress builds up.
Subduction is the process where one tectonic plate moves beneath another plate into the Earth's mantle at a convergent boundary. This can lead to the formation of deep ocean trenches and volcanic activity. It is a fundamental process in plate tectonics that drives the movement and interaction of Earth's lithospheric plates.
Subduction is the process where one tectonic plate moves beneath another plate at a convergent boundary. This occurs because the denser oceanic plate sinks into the mantle due to gravity, causing the less dense continental plate to override it.
Subduction is the process where one tectonic plate moves beneath another plate at a convergent boundary. This occurs because the denser plate sinks into the mantle, creating a subduction zone. The sinking plate can cause earthquakes, volcanic activity, and the formation of mountain ranges.
A subduction zone is the plate boundary where old and heavy oceanic crust sinks into the mantle. At subduction zones, oceanic crust is forced beneath another tectonic plate, typically a continental plate, due to differences in density. This process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
A convergent plate boundary leads to subduction. This occurs when two tectonic plates collide and one plate is forced beneath the other, typically resulting in the formation of deep oceanic trenches and volcanic arcs.
Mount Fuji is located on the convergent boundary between the Pacific Plate and the Philippine Sea Plate. This boundary is a subduction zone, with the Philippine Sea Plate being forced beneath the Pacific Plate. The intense geologic activity in this region is responsible for the formation of Mount Fuji and the volcanic activity in the area.
A subduction plate involves an oceanic plate being pushed beneath a continental plate or another oceanic plate. The oceanic plate is denser and sinks into the mantle at a convergent boundary, creating a subduction zone. Common examples include the Pacific Plate subducting beneath the North American Plate along the west coast of North America.
This means that the cooler, heavier oceanic plate at an oceanic to oceanic convergent boundary is forced into the mantle - under the hotter, lighter oceanic plate. OR At oceanic to continental boundary the heavier oceanic plate is forced into the mantle under the lighter continental plate.