Some of the water from precipitation will soak into the soil and rocks as groundwater. Some of this water will stay in the shallow soil layer and will move towards streams and rivers. When groundwater soaks deeper into the soil, it refills underground stores. In cold climates the precipitation may build up on land as snow, ice or glaciers. If the temperatures rise, this solid snow and ice will melt into liquid water, which soaks into the ground or flows into rivers or the ocean. Some of the precipitation will soak into the soil and move through the ground until it reaches the rivers or the open water, large lakes and the oceans. Water that reaches the surface of the land may flow directly across the ground into the rivers, lakes and oceans. This water is called surface run-off. When there is a lot of surface run-off, soil can be carried off the land and into the rivers. This can cause them to become silted up and blocked.