answersLogoWhite

0

Actually, that's mineralizaton. It happens in sedimentary rock as minute particles (not quite molecules, but too small to see) displace bits of tissue. It's common to hear the term "fossilization," but fossils are simply things that are unearthed, mineralized or not.

User Avatar

Wiki User

12y ago

What else can I help you with?

Related Questions

What is The condition when dead organisms are turned into rock by mineral rich water?

It's called 'petrification'.


How do you speed up the petrification process?

To speed up the petrification process, you can increase the temperature and pressure of the environment where petrification is taking place. Enhancing the mineral content of the surrounding solution can also accelerate the petrification. Additionally, exposing the object to catalysts or enzymes that promote mineral deposition can help speed up the petrification process.


What is the difference between petrifaction and permineralization?

Permineralization is the process of fossilization where mainly water mineral deposits take the form of the organism. The minerals harden with time and pressure from over laying deposits turning into rock. Petrification happens when silica binds with celulose of a plant and turns into stone often retaining the microstructure of the plant.


What is a common carbonate mineral that replaces a mineral in fossils?

Calcite is a common carbonate mineral that often replaces the original mineral in fossils during the fossilization process. Calcite can help preserve the structure of the fossil while replacing the original material.


What mineral is not involved in petrification?

Petrification is defined as the preservation of organic hard parts by mineral-bearing waters infiltrating the porous material after burial.The common preserving minerals are silica, calcite, and iron compounds.Fossils are not necessarily petrified.So, apart from the above minerals, the answer to your Q is wide open.


What causes a tree to become petrified?

Wood petrification is the process in which organic material is converted to stone by becoming impregnated with silica. The wood becomes soaked with mineral-laden water. The water evaporates at about the same rate as the wood decays and mineral crystals replace the wood.


Can a body petrify after fourteen years?

Yes, a body can undergo petrification, but this process typically takes much longer than fourteen years. Petrification, or the process of turning organic material into stone, usually occurs over thousands to millions of years through mineral replacement and fossilization. Factors such as environmental conditions, the presence of minerals, and the type of organic material all influence the rate of petrification. Therefore, while some decomposition can occur in fourteen years, complete petrification would generally require a significantly longer timeframe.


What is the process in which mineral matter replaces previously formed cartilage is called?

The process in which mineral matter replaces previously formed cartilage is called ossification or calcification. This process involves the deposition of calcium salts and other minerals to harden the cartilage into bone tissue.


What process in which mineral replaces previously formed cartilage is called?

The process in which mineral replaces previously formed cartilage is called endochondral ossification. This process is essential for the formation of bones during embryonic development and involves the gradual replacement of cartilage by bone tissue.


What is an example of of mineral replacement?

petrified wood


Does and organism have to be buried to become a fossil?

No, an organism does not have to be buried to become a fossil. Fossils can form through a variety of processes, such as compression, mineral replacement, or petrification, which can occur even without burial.


How Petrification Occurs?

Petrification occurs when organic matter is replaced by minerals, usually through a process called permineralization. This process involves the infiltration of minerals into the pores of the organic material, eventually solidifying and preserving it in a rock-like form. The original organic material is effectively turned into stone, creating a fossil.