1. Unit 3: Geologic Time, the Evolution of the Biosphere & Human Impact

2. Part 1: Construction of the Geologic Time Scale and Reading the Rock Record

3. Scale of Geologic Time Time is so vast compared to human experience need metaphors to help comprehend –Ex. 4.6 billion years = 1 calendar year –Ozmandias How do we know??? –Geologists can read the rock record for clues to earth history and dates

6. Reading the Rock Record Type of rock tells about environment of formation –sedimentary vs. igneous, limestone vs. conglomerate) Relative and absolute dating techniques can give date of rock layer –543 mya vs. older than this Fossils within the rock or presence of certain minerals or structures can tell about the environment and biosphere at the time of the rock formation –Fern vs. coral, oxidized minerals vs. unoxidized

9. Sedimentary Rocks What does this Rock Tell you??? Psst…Listen up Bucko, Back in my day…

10. Sedimentary Rocks and their environments Limestone = ocean, shallow or deep depending on types of fossils Sandstone = coastline, stream or lake edge, desert Shale = quiet deep ocean or lake bottom Coal = swamp Conglomerate = fast moving stream, active coastline, glacial deposit

12. Igneous Rocks and their environments Coarse-grained igneous (ex. Granite)= cools deep underground Fine-grained igneous (ex. Rhyolite, Basalt)= cooled rapidly at surface Gassy/glassy igneous (ex. Obsidian, pumice)= cooled instantly in air Ash=volcanic event

13. Metamorphic & Other Rocks and their environments Localized metamorphic rocks= heat from volcanic activity or fluids Regional metamorphism= pressure from tectonic forces (direction can be determined from foliation) Shocked quartz, iridium spikes, metallic sediment= meteor impact Unsorted, angular sediment sedimentary rock=glacial deposit

14. Fossils and Structures Fossils indicative of environment (ex. Fern vs. coral) Fossils help with dating and correlations based on principle of fossil succession: fossils succeed one another in a definite order, and therefore any time period can be recognized by its fossils Fossil structures such as ripples, footprints, burrows, crossbedding give evidence of environment

17. Correlation and Dating using fossils Fossil succession Idex fossils vs. groups of fossils

18. Relative Dating: Key Terms Uniformitarianism vs. Catastrophism Law of Superposition Principle of Original Horizontality Principle of Cross-cutting Relationships Inclusions Unconformities