Clues to Earths Past Fossils Remains imprints or
- Slides: 20
Clues to Earth’s Past
Fossils �Remains, imprints, or traces of prehistoric organism.
Permineralized remains �Fossils where the spaces inside are filled with minerals
Carbon Film �A flim of carbon can form around an organism creating a silhouette
Mold-Cast �Mold- imprint left after hard parts of organism decay �Cast- a copy of organism made from the mold
Trace Fossils �Fossils that are evidence of organisms activity (not organism itself) �Such as: � Tracks/footprints � Burrows � Trails
Index Fossils �Abundant, widespread organisms that existed for a SHORT period of time.
Principle of Superposition �In undisturbed layers of rock, the oldest rocks are found at the bottom, with the rocks becoming younger towards the top.
Relative Age �Relative age is how old a rock or fossil is in COMPARISON to the ages of other things.
Igneous Intrusion �when an igneous intrusion cuts across a formation of rock, it can be determined that the igneous intrusion is younger than the rock it’s cutting through.
Unconformities �Unconformities are when layers of rock are missing �Unconformities develop when running water or glaciers remove rock layers
Angular �When rock layers are tilted and younger sediment layers are deposited horizontally on top of the eroded and tilted layers
Disconformity �When a layer of horizontal rock is exposed and eroded before younger rocks form over it
Nonconformity �When sedimentary rock forms over eroded metamorphic or igneous rock
When the layers are too disturbed: �The same rock layers can be found in different locations; FOSSILS must be used to prove that the layers match up
Absolute Dating �Calculating the absolute age of a rock by measuring the amounts of materials in a rock and knowing the material’s half life.
Half-Life: Time it takes for half of the atoms in an isotope to decay
Radioactive Decay �Breaking down of an atom into a proton and an electron.
Radiometric Dating �Uses the properties of atoms in rocks and other object to determine their ages.
Uniformitarianism �Principle that Earth’s processes occurring today are similar to those that occurred in the past.
- Remains, imprints or traces of once-living organisms
- All types of fossils
- Imprints 12
- Boda boda types of clues
- What do fossils tell us about the past
- What do fossils tell us about the past
- Why would humans be a good index fossil
- Fossils evidence of past life
- Whats the name of earths moon
- Earths early atmosphere contained
- Spring earth tilt
- Earths layers foldable
- Arch of constantine frieze
- Brown earths
- What is the most abundant element on earth
- Earths mantle
- Lithosphere
- Layers of the atmosphere definitions
- Earths roation
- What does earths tilt do
- Study of earth's physical features