PDF-Rocks, fossils, and original remains ou have read about mountain forma
Author : briana-ranney | Published Date : 2016-04-16
2 1 MATERIALS OUTLINE Remember to take notes onthis section in outline form I Main ideaA Supporting idea1 Detail2 Detail pp ortin g idea FCAT VOCABULARYVOCABULARYoriginal
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Rocks, fossils, and original remains ou have read about mountain forma: Transcript
2 1 MATERIALS OUTLINE Remember to take notes onthis section in outline form I Main ideaA Supporting idea1 Detail2 Detail pp ortin g idea FCAT VOCABULARYVOCABULARYoriginal remainsice core nditions. What are fossils?. FOSSILS. . are. . the . preserved remains or . traces. of animals, plants, and other organisms . that lived long ago.. When an organism dies, hard parts of the animal (bones, teeth, shells, etc.) can be preserved in rock.. Grade 3 . SS3E2 Students will investigate fossils as evidence of organisms that lived long ago. What is weathering?. Weathering is the slow breaking apart or wearing away of rock into smaller pieces.. Stratigraphy. B. Natalin. 2. Prof. Dr. Boris . Alekseevich. Natalin, . Office – E 502. Phone – 285 6221, . e-mail: . natalin@itu.edu.tr . Website: . http://web.itu.edu.tr/~natalin/. . Assistant: Ali . 1. THE EARTH THROUGH TIME. TENTH EDITION. H A R O L D L. L E V I N. Chapter 9 . Proterozoic. : Dawn of a More Modern World. Proterozoic. Eon. 2.5 billion years to 542 million years ago. Comprises 42% of Earth history . WHAT IS A FOSSIL?. WHAT IS A FOSSIL?. WHAT IS A FOSSIL?. WHAT IS A FOSSIL?. TRACE . or. REMAINS of something that lived LONG AGO!. That exposes us to Earth’s BIOLOGICAL (_ _ _ _) PAST.. That . exposes us to Earth’s BIOLOGICAL (. 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 . . Palaeontology. Palaeontology is . the . branch of science concerned . with. . fossil. Palaeontology is . the. study of fossils as a . way of getting. . information. . about: . the history. Earth is very, very old…. Earth’s History. The history of Earth and the ages of rocks can be investigated and understood by studying rocks and fossils.. Evidence of ancient, often extinct life is preserved in many sedimentary rocks.. 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.. Chapter 10. Section 1- Fossils. Fossils are the preserved remains or traces of living things.. Fossils provide evidence of how life has changed over time. How Fossils Form. Most fossils form when living things die and are buried by sediments.. Section 12.1 Discovering earth’s history. Uniformitarianism – the idea that physical, chemical, and biological laws that operate today also operated in the past; the present is the key to the past.. 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. 8. th. grade. Compare . fossils found in sedimentary rock to determine their relative age. . . http://www.brainpop.com/science/diversityoflife/fossils. /. . Standard for this lesson: . How can we tell what lived when?. ASSISTANT PROFESSOR. Department of Zoology. Nilkantharo. . Shinde. Science and Arts College, . Bhadrawati. Fossils. – . Sir Charles Lyell. Fossil can be defined as . “Any body or traces of body, animal or plant buried and preserved by natural cause”..
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