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Fossils SOL #10.

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Presentation on theme: "Fossils SOL #10."— Presentation transcript:

1 Fossils SOL #10

2 Fossil Remains, impression, or other evidence preserved from preexisting life Hard parts of organism are more likely to fossilize than soft parts Most are found in sedimentary rock

3 Types of Fossils Mineral replacement Carbon film Mold & cast
Minerals in soil replace soft parts in bones, teeth, or shells Carbon film Carbon imprint of item left behind Mold & cast Imprint in ground that gets filled in by sediment to form a cast Original remain Soft parts of item preserved Trace fossil Evidence of an organism (footprints) Trails & burrow Type of trace fossil

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5 Index Fossils Fossils from species that were only around for a short period of time

6 Dating Fossils Relative age Absolute age
Comparing ages (X is older than Z) Law of superposition-undisturbed layers of rock=older on bottom, younger on top Absolute age Age in # of years Radioactive decay

7 Radioactive Decay Break down of isotopes Alpha/Beta decay Half life
Beta loose electron: alpha loose 2 n & 2 p Half life Time it takes for ½ atoms to decay Radiocarbon Dating Using C-14 to determine age of item

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9 Unconformities Gaps in rocks
Due to erosion or periods of time where no deposition occurred

10 Fossils in VA Mainly in Coastal Plains, Valley & Ridge, and App. Plateau Most are marine org. Paleozoic, Mesozoic, & Cenozoic Eras

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