Convection currents
What is a convection current and how does move the tectonic plates. The convection current is magma that is heated up by the core then rises to the top and when it gets cold it sinks to the bottom to repeat the process, it moves the tectonic plates when the magma is heated up and sent to the top that is when the tectonic plate moves across the earth. Magma rises when its get hot it then moves the tectonic plate across the earth then after that it sinks back down to the core and repeats. This shows that when the magma rises the tectonics plates move then the magma sinks.
Divergent plate boundaries:
All the Earth's new outside layer structures at exclusive limits, yet most are not known in light of the fact that they lie deep under the seas. These are zones where two plates move far from each other, letting magma from the mantle to ascend and make another outside layer. Divergent limits are the place the plates move separated. Ocean bottom spreading is a process which makes the magma make new land submerge, this procedure assumes control of about a ten foot slope causes the development of the ranges from two-ten centimetres for every year this is a million + year process. The magma is light and makes more edges and a sample of this is Mid-Atlantic Ridge.
Convergent:
Convergent is the impact of two plates clashing. A crash of a less denser tectonic plate with a more denser oceanic plate slams into a mainland plate and the sea plate goes under the mainland plate. This takes a lot of vitality and results in the softening the mainland hull, this can create volcanoes are created. The sorts of volcanoes which can happen relies on the chemicals that are in it, the substance creation of the magma which decides its constant and there are three distinct sorts of stream one is Basaltic is when it makes magma fields or shield volcanos, Andesite is the point at which it makes composite volcanoes , Dacite or rhyolite is the point at which it makes a cavity, for example, St. Helens.
Transform:
Here two plates slide by each other in different directions, so they are parallel to each other. The San Andreas Fault is the most surely understood (and most dangerous) unpredictable interface. The two plates slide by each other along an expansive scale issue. Since these are two extensive bits of rock, there is a lot of frictional coupling that happens. Now and again the plates get secured some nearby district and incredible arrangement of strain vitality is put away in that locale. In the long run, the strain vitality develops to the point where the it is abruptly discharged which makes a vast scale earthquake.In a transverse wave the molecule removal is opposite to the bearing of wave proliferation. one-dimensional transverse plane wave engendering from left to right. The particles don't move alongside the wave; they essentially sway all over about their individual positions as the wave cruises by.
What is a convection current and how does move the tectonic plates. The convection current is magma that is heated up by the core then rises to the top and when it gets cold it sinks to the bottom to repeat the process, it moves the tectonic plates when the magma is heated up and sent to the top that is when the tectonic plate moves across the earth. Magma rises when its get hot it then moves the tectonic plate across the earth then after that it sinks back down to the core and repeats. This shows that when the magma rises the tectonics plates move then the magma sinks.
Divergent plate boundaries:
All the Earth's new outside layer structures at exclusive limits, yet most are not known in light of the fact that they lie deep under the seas. These are zones where two plates move far from each other, letting magma from the mantle to ascend and make another outside layer. Divergent limits are the place the plates move separated. Ocean bottom spreading is a process which makes the magma make new land submerge, this procedure assumes control of about a ten foot slope causes the development of the ranges from two-ten centimetres for every year this is a million + year process. The magma is light and makes more edges and a sample of this is Mid-Atlantic Ridge.
Convergent:
Convergent is the impact of two plates clashing. A crash of a less denser tectonic plate with a more denser oceanic plate slams into a mainland plate and the sea plate goes under the mainland plate. This takes a lot of vitality and results in the softening the mainland hull, this can create volcanoes are created. The sorts of volcanoes which can happen relies on the chemicals that are in it, the substance creation of the magma which decides its constant and there are three distinct sorts of stream one is Basaltic is when it makes magma fields or shield volcanos, Andesite is the point at which it makes composite volcanoes , Dacite or rhyolite is the point at which it makes a cavity, for example, St. Helens.
Transform:
Here two plates slide by each other in different directions, so they are parallel to each other. The San Andreas Fault is the most surely understood (and most dangerous) unpredictable interface. The two plates slide by each other along an expansive scale issue. Since these are two extensive bits of rock, there is a lot of frictional coupling that happens. Now and again the plates get secured some nearby district and incredible arrangement of strain vitality is put away in that locale. In the long run, the strain vitality develops to the point where the it is abruptly discharged which makes a vast scale earthquake.In a transverse wave the molecule removal is opposite to the bearing of wave proliferation. one-dimensional transverse plane wave engendering from left to right. The particles don't move alongside the wave; they essentially sway all over about their individual positions as the wave cruises by.