Geologic History Vocabulary Test

Slides:



Advertisements
Similar presentations
Life and Geologic Time.
Advertisements

HOW OLD IS OLD? The Rock Record and Geologic Time Chapter 3
Fossils & History of the Earth
The Geologic Time Scale
Geologic Time Scale.
History of the Earth Too much time on my hands. Let’s go to the fossil record. That’s some radioactive decay you have on. Take up your super positions.
Define the following terms at the top of your notes for Ch 21!
Chapter 11 Fossils Fossil: evidence such as the remains, imprints, or traces of once living organisms preserved in rocks Many times dead.
SI. A) Relative age: the age of rock compared to the ages of other rocks above or below it in a sequence of rock layers.
Fossils and the Rock Record
Clues to the Earth’s Past. Paleontology The branch of biology that studies the forms of life that existed in former geologic periods, chiefly by studying.
Fossils and the Rock Record The Rock Record  Rocks record geological events and changing life forms of the past  Planet Earth was formed 4.6 billion.
Vocab. Fossil Remains, imprints, or traces of prehistoric organisms.
Fossils & The Geologic Time Scale. Fossils Preserved remains or traces of an organism that lived in the past. Fossils are formed when organisms die and.
Fossils are the remains, imprints, or traces of prehistoric organisms. Formation of Fossils Most fossils are the hard parts of organisms, such as fossil.
Chapter 13 Earth Science Clues to Earth’s Past. Words to Know – Section 1 Fossils fossil Permineralized remains Carbon film Mold Cast Index fossil.
How is geologic Time divided?.  I can distinguish the different geologic time periods.
HOW OLD IS OLD? The Rock Record and Deep Geologic Times.
Geologic Time. The Geologic Time Scale  A summary of major events in Earth’s past that are preserved in the rock record  Divisions of Geologic Time.
Lesson 1: Geologic Time Evidence That Earth Has Changed Geologists use the principle of superposition, which states that in rock layers that have not.
CHAPTER 17 THE HISTORY OF LIFE
Jeopardy Fossils Relative Aging Absolute Dating Geologic Time
Fossils and the Rock Record
Geologic Time   By examining layers of sedimentary rock, geologists developed a time scale for dividing up earth history. Earlier in the 20th century,
Chapter 6 Earth’s History
WARM-UP 85 The difference between relative dating and absolute dating is that relative dating is a method of sequencing events in the order in which they.
Section 21.1 Study Guide Section 21.1 Main Ideas
Chapter 14 Earth Science Geologic Time.
II. Why Do We Study Fossils Found in Rocks?
What are Fossils? Fossils are the evidence or remains of once-living plants or animals Fossils provide evidence of past existence of a wide variety of.
Geological Time 9.1.
Chapter 10 Geologic Time.
The Rock Record.
Earth History.
Geologic time Review.
Geologic Time Scale MYP 2.
Section 1: Geologic Time
Geological time, Fossils, & Dinosaurs
Chapter 12 Geologic Time.
GEOLOGIC TIME If it is in red, write it!.
Chapter 13 Clue’s to Earth’s Past.
Unit 2, Lesson 4 The Geologic Time Scale
The Fossil Record (Ch 19.1) Unit 5: Evolution.
Earth History Vocabulary.
The Fossil Record Section 3
Lesson 1 Fossil Evidence.
Earth History.
Fossil Evidence of Evolution
CHAPTER NEW CHAPTER Views of Earth’s Past the BIG idea
Geologic Principles Notes
Ch. 6 Vocabulary.
EARTH’S HISTORY.
Fossils SOL #10.
Unit 5: Geological Time Vocabulary
Stratigraphy, Fossils and Geologic Time
Fossils Fossil-remains, imprints or traces of prehistoric organisms. Only the hard parts of a plant or animal become fossils. Types of Preservation: --Mineral.
Chapter 4 Test Review What are fossils? What is a petrified fossil?
M&M Radioactive Decay Lab
Geologic Time   By examining layers of sedimentary rock, geologists developed a time scale for dividing up earth history. Earlier in the 20th century,
The Geologic Time Scale
Rock Dating.
The Rock and Fossil Record Review Game
Geologic Time Notes By studying the characteristics of rocks and the fossils within them geologists can… interpret the environments in which the rocks.
Fossils and the Rock Record
GEOLOGIC HISTORY, FOSSILS, & RELATIVE DATING
Earth’s History Created by Educational Technology Network
Earth’s History.
Fossils and the Rock Record
Fossils Remains, imprints, or traces of once living organisms.
Presentation transcript:

Geologic History Vocabulary Test Chapter 13 & 14

remains, imprints, or traces of once-living organisms #1 remains, imprints, or traces of once-living organisms

fossils of species that existed for short periods and were widespread #2 fossils of species that existed for short periods and were widespread

cavity in rock made when an organism decayed #3 cavity in rock made when an organism decayed

#4 method by which order of events or age of rocks is determined by examining the position of rocks in a layer

#5 formed when original materials in skeletal remains are replaced by minerals

#6 states that in a sequence of undisturbed rocks, the oldest rocks are on the bottom and the rocks become progressively younger toward the top

produced when sediments fill in a cavity made when an object decayed #7 produced when sediments fill in a cavity made when an object decayed

#8 process that uses the properties of atoms in rocks and other objects to determine their ages

fossil of thin layer of carbon atoms and molecules #9 fossil of thin layer of carbon atoms and molecules

#10 gaps in rock record made when agents of erosion remove existing rock layers

time it takes for half of an isotope's atoms to decay #11 time it takes for half of an isotope's atoms to decay

#12 method by which a geologist can calculate the absolute age of the rock by knowing the half-life of an isotope

#13 principle that earth's processes occurring today are similar to those that occurred in the past

#14 process that occurs when the number of protons in an atom is changed and a new element is formed

#15 one of four major subdivisions of geologic time-the longest subdivision (based upon the abundance of certain fossils)

division of Earth's history into smaller units #16 division of Earth's history into smaller units

#17 one of four major subdivisions of geologic time-characterized by the types of life existing worldwide at the time

#18 one of four major subdivisions of geologic time-second longest subdivision (marked by major, striking, worldwide changes in the types of fossils present

#19 one of four major subdivisions of geologic time-characterized by differences in life-forms which can vary from continent to continent

#20 used to study the passage of geologic time because of changes in their physical features through time

#21 a group of organisms that normally reproduces only with other members of their group

#22 blue-green algae thought to be one of the earliest forms of life on Earth

giant landmass or supercontinent meaning "all land" #23 giant landmass or supercontinent meaning "all land"

#24 longest part of Earth's history-includes the Hadean, Archean, and Proterozoic Eons (4.5 billion yrs. ago to about 544 million yrs. ago)

#25 (era of middle life) time of many changes on Earth (Pangaea)-from 248 million years ago to 65 million years ago

#26 (era of recent life) began about 65 million years ago and continues today

#27 (era of ancient life) began about 544 million years ago and ended about 248 million years ago