ya when ice convert to water then it flows.......
An ice flow is a mass of ice that moves slowly over land due to gravity. It is a common feature in glaciers and ice sheets, where the ice deforms and flows like a very viscous fluid. Ice flows can contribute to the movement and shaping of landscapes in polar regions.
an ice sheet
still flows and carries debris to the end of the glacier
man made
black power
Europa, one of Jupiter's moons, is a natural satellite where it is believed that ice flows. This is due to its icy surface, which shows evidence of crustal plates moving and shifting over time, suggesting the presence of subsurface oceans kept warm by tidal forces.
Probably, but it's not a natural part of their diet.
Ice cracking is a phenomenon one observes when glacial ice flows into water. The ice flows based on gravity. This is a constant process, and the ice cracking is also, therefore, constant.
ya when ice convert to water then it flows.......
Heat flows from the liquid at room temperature to the ice, in order to melt the ice and bring it to the same temperature as the liquid.
Erosional landforms dominate an area where the ice flows to, while depositional landforms are found where ice flows from.
Yes, sort of. Not LIQUID water, which would be pretty spectacular, but ice - probably in the form of frost - in the shadowed bottoms of craters near the south pole of the Moon. There's reason to believe that ice and frost is also present in similar craters near the north pole of the Moon, but this has not yet been demonstrated.
Heat flows from your hand to the ice cube, causing the ice cube to melt and warm up. This is because heat always flows from areas of higher temperature to areas of lower temperature until thermal equilibrium is reached.
It flows, by conduction, from your hand to the ice cube.
An ice flow is a mass of ice that moves slowly over land due to gravity. It is a common feature in glaciers and ice sheets, where the ice deforms and flows like a very viscous fluid. Ice flows can contribute to the movement and shaping of landscapes in polar regions.
As a glacier or ice sheet moves, it can erode bedrock. The ice can then pick up, or entrain, the eroded rock. As the ice flows, it transports the bedrock debris in the direction of flow.