The layer of soil that is made up of impenetrable rock is known as the bedrock layer. This layer is located beneath the topsoil and subsoil layers, and it acts as a barrier to root growth and water penetration.
Sedimentary rock, such as sandstone or shale, is often formed from soil deposits carried by moving water from rivers or streams. These sediments accumulate, compress, and cement over time to form rock layers.
Clay soil has the smallest rock particles compared to sand and silt. Clay particles are less than 0.002 mm in diameter, giving the soil its fine texture and ability to hold water well.
Such soil or rock is 'impervious'.
Water stored in soil and rock is called groundwater. It fills the spaces between soil particles or within rock formations, forming aquifers that can be accessed through wells for drinking water and irrigation purposes.
The layer of soil that is made up of impenetrable rock is known as the bedrock layer. This layer is located beneath the topsoil and subsoil layers, and it acts as a barrier to root growth and water penetration.
Water contained in pores of soil or rock is groundwater..
This is known as pore water. If the soil or rock is in-situ (in other words in the ground) it may also be known as ground water.
Sedimentary rock, such as sandstone or shale, is often formed from soil deposits carried by moving water from rivers or streams. These sediments accumulate, compress, and cement over time to form rock layers.
the answer to this question is that Soil with smaller particles can hold more water when Soil with larger rock particles can hold less water.....
Soil can be formed from the erosion and deposition of any kind of rock: igneous, sedimentary, or metamorphic.
Clay soil has the smallest rock particles compared to sand and silt. Clay particles are less than 0.002 mm in diameter, giving the soil its fine texture and ability to hold water well.
Such soil or rock is 'impervious'.
Groundwater is water that is stored in layers of soil and rock beneath Earth's surface. It fills the spaces between particles of rock and soil and can be accessed by wells or springs.
Bed rock is a layer of soil. It seeps the water down.
Water stored in soil and rock is called groundwater. It fills the spaces between soil particles or within rock formations, forming aquifers that can be accessed through wells for drinking water and irrigation purposes.
The weathering process that results from the removal of minerals in soil or rock by water filtering down through the soil is known as leaching. Water dissolves and carries away minerals, leaving the remaining soil or rock altered in composition.