lava= material flowing from a volcano
The saturation horizon refers to the depth in the subsurface where all the pore spaces in a rock are filled with fluid. Below this horizon, the rock is completely saturated with fluid, usually water or hydrocarbons, and any additional fluid injected will displace some of the existing fluid.
High temperature and pressure in the mantle cause the rock to become more fluid-like. This allows it to flow slowly over geological timescales, contributing to the movement of tectonic plates. Additionally, the presence of partial melting can further decrease the viscosity of the rock, increasing its fluidity.
Sandstone is known to have a porosity of around 22%. In 50 liters of sandstone with 22% porosity, there could be approximately 11 liters of fluid present (50 L * 0.22).
Yes, it is possible for a rock to have high porosity, meaning it has a lot of open spaces or pores, but low permeability, indicating that the pores are not well connected or that the rock's structure hinders the flow of fluids. As a result, while the rock can hold a lot of fluid within its pores, the fluid may not be able to flow easily through it.
the plasic like rock of the lower mantle is the asthenosphere
lava
lava
Then fluid can travel through the rock, and the rock is said to be "permeable".
The saturation horizon refers to the depth in the subsurface where all the pore spaces in a rock are filled with fluid. Below this horizon, the rock is completely saturated with fluid, usually water or hydrocarbons, and any additional fluid injected will displace some of the existing fluid.
Transmission fluid leaked out of car very fast. After hitting large rock. Could it be the transmission pan is broke? That is a possibility
Hydraulic rock breakers are powerful percussion hammers. The rock breaker works on the principal of hydraulics, where putting pressure on one part of a fluid transfers pressure to all areas of the fluid, allowing a multiplication of force.
... the fluid state we call 'lava'.
Hot fluid dissolves materials and adds other materials :)
Molten rock that moves throgh crustal carbonate rock, That is heat the rock. Hot water as a form of steam or superheated fluid reats with crustal rock and other igneous material.
temperature, pressure, and fluid
It is played as a solumential guidence fluid that flows through the rock to give it its color
When the fluids enter the already hot mantle rock, the melting temperature of the hot rock decreases. As a result, the rock begins to melt.