Lithification (from the Ancient Greek word lithos meaning 'rock' and the Latin-derived suffix -ific) is the process in which sediments compact under pressure, expel connate fluids, and gradually become solid rock. Essentially, lithification is a process of porosity destruction through compaction and cementation. Lithification includes all the processes which convert unconsolidated sediments into sedimentary rocks. Petrifaction, though often used as a synonym, is more specifically used to describe the replacement of organic material by silica in the formation of fossils.[1]
YouTube Encyclopedic
-
1/3Views:53 7303926 176
-
Sedimentary Rocks Introduction
-
Lithification Meaning
-
Sedimentary Rocks - Compaction and Cementation
Transcription
See also
- Concretion – Compact mass formed by precipitation of mineral cement between particles
- Diagenesis – Physico-chemical changes in sediments occurring after their deposition
- Lithology – Description of its physical characteristics of a rock unit
- Parent rock – Original rock substratum
- Petrifaction – Process of fossilisation
- Weathering – Deterioration of rocks and minerals through exposure to the elements
References
- ^ Monroe, J.S.; Wicander, R.; Hazlett, R.W. (2006). Physical Geology: Exploring the Earth (6th ed.). Belmont: Thomson. pp. 203–204. ISBN 9780495011484.
 | This article about geological processes is a stub. You can help Wikipedia by expanding it. |
 | This sedimentology article is a stub. You can help Wikipedia by expanding it. |
This page was last edited on 27 July 2023, at 12:27