sorry about spelling
- porous rocks
If they are NOT connected, then I think they are called "Voices", or voce (voh-chay).
Shakespeare was part owner of two theatres: The Globe and the Blackfriars. Some scholars think his early plays were performed at The Theatre and The Curtain.
Rocks break apart from force and heat. Water, freezing, thawing, and wind break rocks into smaller portions.
Geoffery Chaucer wrote a book called Canterbury tales about people travvelling to thomas beckets shrine. Geoffery Chaucer wrote a book called Canterbury tales about people travvelling to thomas beckets shrine.
The CPU is connected to all the peripherals, which include the keyboard, the monitor, the speakers, and anything else that is connected to your computer. Strictly speaking, the CPU is physically connected to the motherboard.
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.
Water held in pores of rocks is called groundwater. It is an important natural resource that can be extracted through wells for various uses.
Porous rocks.
It is called pore water pressure
Saturated Zone .
Air and fluids.
The process of water seeping or flowing into rocks is called infiltration. This occurs as water moves through the pores and cracks in the rock, eventually becoming groundwater.
tiny holes in the skin are called pores
Pores
Groundwater is located in aquifers which are layers of rocks underground that have pores that fill with water that comes from the above layer called the water table or phreatic surface. Further below the water table, where the pores are filled with water, is called the phreatic zone.
aquifer
Rock with unconnected pores is typically referred to as "tight" or "impermeable" rock. This type of rock has pores that do not interconnect, which prevents the flow of fluids through it. As a result, it often acts as a barrier to groundwater or hydrocarbons, making it less effective as a reservoir compared to porous rocks with well-connected pore networks. Examples include certain types of shale or dense limestones.