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13y ago

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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.


How does calcite harden?

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.


Uplift replaces rocks on Earth's surface lost to the process of what?

Uplift replaces rocks on Earth's surface lost the process of erosion.


Rocks containing calcite are most easily weathered by the chemical process of what?

Rocks containing calcite are most easily weathered by the chemical process of dissolution, where calcite is dissolved by acidic water. This process is facilitated by the weakly acidic nature of rainwater, which reacts with calcite to form dissolved ions that are easily carried away by water.


Bird replaces feather in a process?

sheeding


Process in which one generation replaces another?

Reproduction.


What process replaces dead and damaged cells?

Meiosis


What does calcite turn into?

Calcite does not undergo a chemical change under normal environmental conditions. However, if exposed to heat, pressure, or chemical alteration, calcite can potentially transform into other minerals such as marble through a process called metamorphism.


Windows vista installation process replaces dos boot with?

HCL


The process by which one slide replaces the other is called a.?

its called a transition =]


What is the process called when embryonic cartilage is replaces by bone cells?

ossificaton!


Does petrified wood contain many minerals?

Yes, petrified wood does contain minerals. During the petrification process, the organic materials of the wood are replaced by minerals such as quartz, calcite, and pyrite, resulting in a fossilized form of the original wood structure.