true
Cooler material is more dense and hotter material is less. This means that plates become more dense as they cool.
True. In the mantle, hotter, less dense material rises toward the Earth's surface, while cooler, denser material sinks. This process is part of mantle convection, which drives plate tectonics and influences geological activity. The continuous movement helps distribute heat from the Earth's interior to its surface.
Because it is less dense than the material that makes up the earth's crust, but more dense than the material that makes up the air.
Cooler material (magma) shrinks and becomes more dense. Gravity acts on this denser material more strongly because of its greater unit mass (density = Mass/volume). Lighter material rises as the heavier material displaces it below. This produces a the apparent bouyant force.
The dense air sinking towards the Earth's surface is called subsidence. Subsidence can lead to high pressure systems and stable weather conditions.
Cooler material is more dense and hotter material is less. This means that plates become more dense as they cool.
cooler particles are slower moving thus more dense. the more dense the material the further it will sink
True. In the mantle, hotter, less dense material rises toward the Earth's surface, while cooler, denser material sinks. This process is part of mantle convection, which drives plate tectonics and influences geological activity. The continuous movement helps distribute heat from the Earth's interior to its surface.
Because it is less dense than the material that makes up the earth's crust, but more dense than the material that makes up the air.
Cooler material (magma) shrinks and becomes more dense. Gravity acts on this denser material more strongly because of its greater unit mass (density = Mass/volume). Lighter material rises as the heavier material displaces it below. This produces a the apparent bouyant force.
because the heavier elements are pulled toward center of the earth by gravity
Cooler material in the asthenosphere rises towards the lithosphere because of its higher density compared to the surrounding warmer material. As it rises, it displaces the less dense material above it, creating convection currents that contribute to plate movement and tectonic activity.
No, when light passes into a denser material, it bends toward the normal. This phenomenon is known as refraction.
The dense air sinking towards the Earth's surface is called subsidence. Subsidence can lead to high pressure systems and stable weather conditions.
This movement is an example of convection. As the mantle is heated from below, warmer, less dense material rises toward the crust, while cooler, denser material sinks back down. This convection process drives plate tectonics and influences the movement of Earth's lithosphere.
The angle of refraction bends toward the normal when light travels from a less dense medium to a more dense medium, like from air to glass. This happens because the speed of light is slower in the denser medium, causing the light waves to refract towards the normal line.
b. Warm air is as dense as cooler air. Temperature has a direct impact on air density, with warmer air being less dense than cooler air at the same pressure.