entrochite Antonyms
No Synonyms and anytonyms found
Meaning of entrochite
Webster
entrochite (n.)
A fossil joint of a crinoid stem.
entrochite Sentence Examples
- The entrochite, a fossilized segment of a crinoid stem, is a common find in many sedimentary rock formations.
- Entrochites are typically cylindrical or disc-shaped, and can range in size from a few millimeters to several centimeters in length.
- The surface of an entrochite is often ornamented with fine ridges or grooves, which can help to identify the species of crinoid from which it came.
- Entrochites are formed when the calcareous material of a crinoid stem is replaced by minerals such as calcite or pyrite.
- This process of fossilization can occur over millions of years, and the resulting entrochites can be found in a variety of colors, including white, gray, brown, and black.
- Entrochites are often found in association with other crinoid fossils, such as calyxes (the cup-shaped body of the crinoid) and arms.
- These fossils can provide valuable information about the past environments in which crinoids lived, as well as the evolutionary history of this group of marine animals.
- Entrochites are also used as ornamental stones, and can be found in jewelry, carvings, and other decorative objects.
- The word "entrochite" comes from the Greek words "en" (inside) and "trochos" (wheel), referring to the wheel-like shape of these fossils.
- Entrochites are a fascinating and unique type of fossil, and can provide a glimpse into the ancient world of crinoids.
FAQs About the word entrochite
A fossil joint of a crinoid stem.
No synonyms found.
No antonyms found.
The entrochite, a fossilized segment of a crinoid stem, is a common find in many sedimentary rock formations.
Entrochites are typically cylindrical or disc-shaped, and can range in size from a few millimeters to several centimeters in length.
The surface of an entrochite is often ornamented with fine ridges or grooves, which can help to identify the species of crinoid from which it came.
Entrochites are formed when the calcareous material of a crinoid stem is replaced by minerals such as calcite or pyrite.
