PPT-FOSSILS Think About It . . .

Can you name any dinosaurs Do you know what they looked like or how they moved Scientists have been able to tell us many things about organisms such as dinosaurs that lived millions of years ago. WEBQUEST10. th. grade. Index. Background Information. Introduction. Task. Resources. Time. Process. Conclusion. Rubric. Games. Q. What do dinosaurs have that no other reptiles have?. Background Information. By Parker, Emma, Finn, Liam, and Nils. Introduction. A fossil is a mold of a old living thing. A fossil can also be an imprint of an animal. A fossil is not always a bone, a fossil is not always a stone.. If you were to put the following events in to a time sequence of first to last, how would you do it? What else would you add?. . Go to school. Wake up. Eat lunch. Put clothes on. WHAT’S IN THE ROCKS!. The . unweathered. rock that lies below the lowest layer of soil. Depostion. Bedrock. delta. The decayed remains of plants and animals. a. delta. b. soil. c. humus. A large mass of deposited sediments at the mouth of a river. Chapter 3. Our World in One . Minute!!`. http. ://. www.youtube.com/watch?v=ZSt9tm3RoUU. Section 1: Earth’s Story and Those Who First Listened. The Principle of Uniformitarianism. For 30 years a Scottish farmer and scientist named . Utah’s geology has changed over time. .. . Notice where North is in th. is p. icture.. . 550 Million Years Ago. Present Day. The Early Years: Paleozoic. Utah was at the edge of North America. The eastern part of the state was flat and low, close to sea level. Coral reefs became thick . Organism DNA. 1a. Some of the strongest evidence for evolutionary relationships comes from studying the DNA of different organisms.. 1b. The fact that all organisms use the same DNA molecule to code for genetic information suggests that these organisms share a distant ancestor.. Fossils can tell us about our biological (life) past…. We’d have to build stronger refrigerators.. FOSSILS can tell us about our. B. IOLOGICAL PAST.. How can fossils help tell us Earth’s . GEOLOGIC. Part II. Types . of Fossils:. Molds. . Casts. Trace fossils. Petrified . fossils. Body. Mold. . fossils. - . a visible empty . space . that was left after an . organism . was . buried in sediment and then . Where, How, and When. Webinar by Jayson . Kowinsky. (Fossilguy.com). 8.31.16 . Where are Fossils?. Florida?. Where are Fossils?. Kentucky?. Where are Fossils?. California?. Where are Fossils?. California?. Can you name any dinosaurs?. Do you know what they looked like or how they moved?. Scientists have been able to tell us many things about organisms (such as dinosaurs) that lived millions of years ago.. Fossils have helped determine approximately when life first appeared, when plants and animals arrived on land, and when organisms became extinct.. CONDITIONS NEEDED FOR FOSSIL FORMATION. Whether or not a dead organism becomes a fossil depends upon how well it is protected from scavengers and agents of physical destruction, such as waves and currents.. Fall 2012. Training Presentation. IA. Introduction. Tell Students:. The . Geologic Time Scale . covers Earth’s entire history. It is divided into 4 major time intervals called eons. The eons are not the same length, but are based on major events. BSc 4. th. Semester (Open Elective). Fundamentals . of Geology (BOE). OPEN ELECTIVE COURSE (OTHER THAN GEOLOGY MAIN STUDENTS. ). Dr Abdullah Khan. Associate . Professor . Department of Geology. AMU.