porous rocks and lime stone
When a rock is placed into a graduated cylinder containing 80 mL of water, the water level rises due to the displacement caused by the volume of the rock. The new water level can be read from the graduated markings on the cylinder, indicating the total volume of water plus the rock. The difference between the initial water level and the new level gives the volume of the rock itself. This principle is based on Archimedes' principle of displacement.
A rock containing well-connected pores is typically called a porous rock. These connected pores allow for the movement and storage of fluids such as water or oil within the rock. Examples of porous rocks include sandstone and limestone.
A rock containing organic debris is called a sedimentary rock. This type of rock forms from the accumulation and compression of organic materials like plant and animal remains. Over time, these organic materials become compacted and cemented together to form a rock.
The boundary below which the ground is saturated with water is known as the water table. It represents the upper surface of the zone of saturation, where all the soil and rock pores are filled with water. The water table can fluctuate based on factors such as rainfall, evaporation, and groundwater extraction. Below this level, the soil and rock are typically unsaturated, containing both air and water.
A blueschist is a variety of metamorphic rock containing glaucophane.
remain the same
When a rock is placed into a graduated cylinder containing 80 mL of water, the water level rises due to the displacement caused by the volume of the rock. The new water level can be read from the graduated markings on the cylinder, indicating the total volume of water plus the rock. The difference between the initial water level and the new level gives the volume of the rock itself. This principle is based on Archimedes' principle of displacement.
an aquifier
The height of the water will rise a level equal to the volume of the rock.
A rock containing well-connected pores is typically called a porous rock. These connected pores allow for the movement and storage of fluids such as water or oil within the rock. Examples of porous rocks include sandstone and limestone.
Porous rocks absorb water. Anything that can absorb water would not be good at containing it.
The zone containing well water is known as the saturated zone or the water table. This zone is the region below ground where the spaces between soil and rock particles are filled with water. Wells are typically drilled into this zone to access groundwater for various uses.
Granite is one example of a rock containing two or more minerals.
A cenote is a sinkhole in rock containing fresh ground water. It can be exposed or underground like a cave.
An ore rock containing the mineral Ilmenite.
Yes, they can be eroded chemically and mechanically.
When rain falls on rocks containing limestone it dissolves the stone and washes it into the ground. So the rock is actually in the water. This water makes its way to rivers and reservoirs. Even though your water company cleans that water and sends it to your home, the dissolved rock is still there. As soon as you heat that water, especially over 63 deg c, it re-solidifies - back into rock.