Magma gets heated, rises, flows horizontally (the plate over it moves with it, but not as fast as the magma), cools and sinks.
First the heat below the mantle makes even the solid part of the mantle flow very slowly as though it were very thick liquid. the hot rising part of the mantle cools as it nears the crust. as the cooling mantle moves sideways it drags along the plate floating on top of it. the arrows show the cooled mantle sinking back down. later on the mantle will may be get warm and rise again.
Heat from Earth's core creates mantle convection currents causing molten rock to rise along mid-ocean ridges. As the rock cools, it moves sideways dragging the tectonic plates along. The cooler, denser rock then sinks back into the mantle at subduction zones, completing the cycle.
Convection is the transfer of heat by the movement of a fluid, such as air or water. In the context of land, convection helps explain how heat from the ground is transferred to the atmosphere, leading to differences in temperature between the land surface and the air above it. This temperature difference is responsible for the movement of air masses and the formation of weather systems over land.
Sea floor spreading occurs at mid-ocean ridges where magma rises to create new oceanic crust. As the crust forms, it pushes the existing plates on either side away from the ridge, causing the plates to move. This process helps explain the movement of tectonic plates and how they interact with each other on Earth's surface.
Infiltration is the movement of surface water into rocks or soil through cracks or pore spaces.
First the heat below the mantle makes even the solid part of the mantle flow very slowly as though it were very thick liquid. the hot rising part of the mantle cools as it nears the crust. as the cooling mantle moves sideways it drags along the plate floating on top of it. the arrows show the cooled mantle sinking back down. later on the mantle will may be get warm and rise again.
A force acting in a horizontal direction, such as wind, earthquake, or soil pressure against a foundation or a retaining wall.
i think there's maybe 12..Precipitation- any form of water which falls from the atmosphereInterception by vegetation- raindrops prevented from falling directly onto the soil by a layer of vegetationTranspiration- The loss of water from the pores in plantsStem flow- movement of water from plantsOverland flow- or surface run off; movement of water across the land surfaceSurface storage- where water is temporarily held in the ground surface as an interception storageInfiltration- movement of water through soilSoil moisture storage- The maximum rate that water can pass through soilPercolation- Downward vertical movement of water from the soil, to rockThrough flow- Sideways movement of water into soilGround water flow- slow sideways movement of water through rockEvaporation- water changed into water vapor (gas)hope this helped :)
The smallest stars in the main sequence are the stars with cooler surface temperatures.
A sloping road surface or unbalanced load.
No. They have the lowest temperatures on the main sequence. The hottest main sequence stars are blue.
Heat from Earth's core creates mantle convection currents causing molten rock to rise along mid-ocean ridges. As the rock cools, it moves sideways dragging the tectonic plates along. The cooler, denser rock then sinks back into the mantle at subduction zones, completing the cycle.
Chemotropism is the directional growth or movement of an organism in response to chemical stimuli, guiding its movement towards or away from the source. Galvanotropism is the directional growth or movement of an organism in response to electrical stimuli. Thigmotropism is the directional growth or movement of an organism in response to physical touch or contact with a solid surface.
Surface Currents.
Surface tension.
Yes; upward, downward, and sideways. Surface texture can make a difference.
Convection is the transfer of heat by the movement of a fluid, such as air or water. In the context of land, convection helps explain how heat from the ground is transferred to the atmosphere, leading to differences in temperature between the land surface and the air above it. This temperature difference is responsible for the movement of air masses and the formation of weather systems over land.