The process that occurs when pore spaces in bone or wood are filled with silica is called silicification. During this process, silica-rich fluids permeate the material, replacing the organic matter and filling the pore spaces, which leads to the preservation of the original structure.
Vacuoles are fluid-filled spaces in cells that store water, nutrients, and waste products. They help maintain turgor pressure in plant cells and can also act as storage compartments for food and other substances in various types of cells.
The air spaces within a leaf, known as intercellular spaces, allow for gas exchange to occur. This facilitates the entry of carbon dioxide needed for photosynthesis and the exit of oxygen produced during this process. Intercellular spaces also help in regulating water vapor and temperature within the leaf.
Intercostal spaces
When bones, or other dense living material is buried, over thousands of years as it decays it leaves spaces where minerals can gather. As the bone/ivory/shell/whatever, decays it is slowly replaced with mineral deposits that when the substance is fully decayed will fill in the hole that would have been left, and that mineral form is the fossil.
When substances harden and crystallize in the spaces between loose sediments, they form a type of rock called a crystalline sedimentary rock. This process involves the filling of pore spaces with mineral crystals, which bind the sediments together to create a solid rock matrix. Common examples of crystalline sedimentary rocks include limestone and dolomite.
The process that occurs when pore spaces in bone or wood are filled with silica is called silicification. During this process, silica-rich fluids permeate the material, replacing the organic matter and filling the pore spaces, which leads to the preservation of the original structure.
In geology, petrification or petrification is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals. So yeah the answer is petrification
water filling in the porous spaces of the Earth's lithosphere
The small spaces in between mineral grains are known as pore spaces. These spaces can be filled with air, water, or other fluids depending on the conditions in which the rock formed. Pore spaces play a crucial role in determining the porosity and permeability of the rock.
the particles of whatever you are using to colour in the space with
In geology, petrification or petrification is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals. So yeah the answer is petrification
Rarefaction
vesicular
Calcite hardens through a process called cementation, where mineral deposits fill in the spaces between individual calcite crystals. This process occurs over time as the calcite is exposed to pressure and moisture in the environment, leading to the formation of a solid and compact substance.
Because it's made of a porous material. Porous substances have microscopic spaces in them - the water simply fills these spaces.
percolation