Sedimentary rocks are classified in a variety of ways:
1) by sediment clast size
2) by mineral composition
3) by their origin:
-
Lithogenous or terrigenous sedimentary rocks have formed from sediment that was primarily consisted of small fragments of preexisting rocks that have made their way to a final depositional setting. They have since undergone lithification (involving compaction and cementation).
-
Biogenous
sedimentary rocks have formed from living organisms, consisting of fragments of shell, bone, teeth, wood, microscopic skeletal remains, excerement, or other organic matter. These material can be preserved or undergo alteration or mineral replacement as they undergo lithification.
-
Hydrogenous
sedimentary rocks are rocks made up of minerals that have precipitated directly from water. This involves changes in the temperature and chemical composition of the fluid precipitating the mineral components.
- Cosmogenous sedimentary rocks consists of material that has come in from outer space: cosmic dust or meteoritic material. By comparison, this material is rare or a trace component in sedimentary rocks.
- A mix of the above components: Many sedimentary rocks fall into mixed categories (examples below). For instance, the cement that holds sedimentary particles together is typically precipitated or recrystallized in the presence of water. Carbonate sedimentary rocks have their own classification based on their biological and chemical components.
4) by unique characteristics of the sedimentary environment or setting in which they formed, or a mix of some or all of the above.
Click on images for a larger view. |
|