N: Geologic Time 1. Geologic History a. Fossils 3. Geologic Time Scale 4. Geologic Belts 5. NC Geologic History How do we know geologic history? Earth's History •Earth's history spans over a length of 4.5 billion years •Geologists have divided that time into units based on major geologic events and life forms Past Life Forms We discovered that some organisms only existed during certain time units, so when geologists find the remains, we know exactly which time unit a rock is from. Fossils are the clues Fossils are the preserved remains and traces of past life forms. They are found in sedimentary rocks. Ordering the Grand Canyon’s History Geologic Time Scale •The time scale was created to show the order of events in Earth's history of 4.5 billion years Divisions From smallest to largest, the units of geologic time are: 1. Epochs 2. Periods 3. Eras 4.Eons Each unit of time is recognized by the fossils it contains! Examples: 1. Age of Coal Swamps 2.Age of Reptiles 3.Age of Mammals 4.Age of Fishes M.Y.A = Million Years Ago Each division is represented by millions of years ago (mya) Geologic Belts Rocks with similar characteristics and history are grouped together in units called GEOLOGIC BELTS North Carolina's Geologic History In North Carolina, there are 11 different belts of igneous, sedimentary, and metamorphic rocks that have similar geologic history. North Carolina's Geologic History •We know that Wilmington is in the Coastal Plain Belt and some of the rocks here formed 66 million years ago! Let's find out more...... How and Why? 12.4 The Geologic Time Scale Structure of the Time Scale Eons represent the greatest expanses of time. Eons are divided into eras. Each era is subdivided into periods. Finally, periods are divided into smaller units called epochs. There are three eras within the Phanerozoic eon: the Paleozoic, which means “ancient life,” the Mesozoic, which means “middle life,” and the Cenozoic, which means “recent life.” 12.4 The Geologic Time Scale Structure of the Time Scale Each period within an era is characterized by somewhat less profound changes in life forms as compared with the changes that occur during an era. The periods of the Cenozoic era are divided into still smaller units called epochs, during which even less profound changes in life forms occur. 12.4 The Geologic Time Scale Precambrian Time During Precambrian time, there were fewer life forms. These life forms are more difficult to identify and the rocks have been disturbed often.