Slide 1

Slide 2 Chapter 9, Section 1: Relative Dating Ahhh! Im not dating HER ! Shes my cousin! Eewww! No way! Slide 3 9.1 The beginnings of geology In 1666, Nicholas Steno, a Danish anatomist, studied a sharks head and noticed that the sharks teeth resembled mysterious stones called tonguestones. Slide 4 9.1 Evidence from Rock Steno theorized that tonguestones looked like sharks teeth because they actually were sharks teeth that had been buried and became fossils. Slide 5 Slide 6 What is relative dating? Stenos principles are used by geologists to determine the age of fossils and rocks in a process called relative dating. Relative dating is a method of sequencing events in the order they happened. Use relative dating to determine which event the foot step, the tire track, or the snow fall - happened first. Slide 7 The Present Explains the Past James Hutton (1726 1797) showed how processes today might explain what happened a long time ago. For example, when it rains really hard you might see flowing water washing away sediment. When the rain stops, you might see grooves left behind by the flowing water. Slide 8 Superposition Stenos ideas for relative dating include superposition, original horizontality, and lateral continuity. Superposition states that the bottom layer of sedimentary rock is older than the layer on top because the bottom layer formed first. A stack of newspapers illustrates superposition. The oldest newspaper is on the bottom of the stack and the more recent newspapers are piled on, with the most recent on top. Slide 9 Slide 10 The Fossil Record The fossil record is the ordering of fossils throughout geological time in layers of rock that accumulate and form. Slide 11 Faunal Succession Faunal succession uses fossils to identify the relative age of the layers of a rock formation. The organisms found in the top layers appeared after the organisms found in the layers below them. Use the illustration (above) to answer the following questions: Did human beings live at the same time as the dinosaurs? Did dinosaurs roam the earth at the same time as trilobites? Slide 12 Fossils and Earths changing surface Most of the land on Earth was part of a large landmass, called Pangaea, about 250 million years ago. Slide 13 Fossils provide evidence for how Earths surface has changed over time. Scientists map fossil locations. Understanding Earths past helps explain how similar plants and animals ended up in different locations. Slide 14 Did you know. that shark teeth are common fossils in Georgia and are the official state fossil? From the Cretaceous to the Miocene periods (approximately 10 to 70 million years ago) sharks hunted and stalked the coastal areas of Georgia. It is very rare to find a fossil of an actual carcass of these prehistoric sharks, but their teeth are found in sizable numbers due to the fact that sharks constantly lose and replace their teeth. Huh?