1/18
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai |
|---|
No analytics yet
Send a link to your students to track their progress
Petrification / permineralization
Sequence of events that turn the remains of organisms into a cast made of stone.
Step 1 of Petrification
Animals or plants die and get covered with sediment.
Step 2 of Petrification
The soft parts are decomposed by bacteria, but hard parts remain.
Step 3 of Petrification
Sediment covering becomes compacted into rock, and water drains down through sediments bringing dissolved minerals.
Step 4 of Petrification
Dissolved minerals replace other materials in bones and hard parts but maintain the shape of the material.
Where to find fossils?
Sedimentary rock layers such as limestone, shale, and sandstone, often exposed by erosion.
How are fossils created?
Dead organisms are rapidly buried by sediment to prevent decomposition.
Ideal place for fossil formation
Bottom of a quiet area of a lake, safe from damage.
Relative dating
Determines chronological order of fossils as older or younger based on position in rock layers without a specific age.
Absolute dating
Calculates actual age in years using methods such as radiometric dating.
Crinoids
Marine invertebrates, such as starfish, sea urchins, and scallops, are characterized by circular, stacked disc-shaped columnals.
Trilobites
Extinct marine arthropods with three-lobed bodies were abundant during the Cambrian period.
Coprolites
Fossilized poop that provides evidence of prehistoric animal diets and behaviors, classified as trace fossils.
Amber
Fossilized tree sap containing preserved insects or plant matter.
Brachiopods
Preserved shells of marine invertebrates that look like clams.
Fossilized teeth
Mineralized remains of teeth from sharks, dinosaurs, or other vertebrates.
Petrified wood
Wood that has turned into stone through the process of permineralization, where minerals replace the structure.
Mold
Imprint in wet mud or sand that hardens. (into stone)
Cast
Models formed from sediment or minerals filling a mold or decomposing organism replaced by minerals. (turned into stone)