Come with us and travel back in time to the geologic period known as the Cambrian Explosion Time Machine Travel Bureau.

Slides:



Advertisements
Similar presentations
Earth Science 13.2A Paleozoic Era : Life explodes
Advertisements

Theory that all of the continents were once one large landmass (Pangaea) that has broken up and drifted apart. –Alfred Wegener Evidence –Continents fit.
Ch Restless Continents
Restless Continents.
The Restless Continents
Geology of Idaho The Northern Rockies. Northern Rockies Basin & Range Middle Rockies The 3 mountainous regions of Idaho.
The Dynamic Interior of the Earth
The geologic time scale shows Earth’s past.
The Geologic Time Scale. Geologic Time Scale : Scientists have formed a chronology of Earth’s history based on evidence from the Earth’s rocks and fossils.
Canada UNIT 2: Physical diversity Chapter 4:Geologic History.
4.1 & 4.2 Plate Tectonics. As explorers began bringing back information about the world, map makers began to notice the coastlines of continents could.
The past, present, and future of our planet and the life on it.
Plate Tectonics The Dynamic Interior of the Earth.
Evolution of Australian Biota Identify and describe evidence that Australia was once part of Gondwana.
Has the continents always looked as they do now on the map, or have they changed shape or location throughout Earth's history? Write your ideas on a sheet.
If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle…..the shapes of the coastlines.
The Earth’s Layers The earth is about 24,900 miles in circumference.
Section 2: Precambrian Time and the Paleozoic Era
Thurs, Nov 17 th CW: Geologic Time HW: Study for quiz Why are there no fossils in layer F?
Earth Science 13.2B Paleozoic Era : Life explodes
Earth History: Geologic Time
History of Earth. Slide 38 - Geologic Time Scale Sequence of events from Earth’s birth to present-day (now). Each Era begins after a mass extinction of.
Overview of natural history Breakdown of time Different periods of Earth’s history are broken into sets of time –just like a year is broken into months,
Plate Tectonics. Earth’s Interior lithosphere Earth ’ s thinnest layer Earth ’ s thinnest layer divided into about 30 huge, moving divided into about.
Agenda: 1.WarmUp 2.How It’s Made 3.Lottery 4.Timeline 5.Video.
Scientists have developed a model of the history of life on Earth called the geologic time scale. The geological time scale is based on studies of Earth’s.
Grade 5 – Unit 6, Lesson 2 Lesson Synopis In this lesson, students will focus on how fossils are evidence of past life rather than creating models of fossils.
Plate Tectonics. History of the Theory First proposed by Alfred Wegener in 1912 Not widely accepted until the 1960s Proposes that Earth’s outer layer.
Zach Holtslander & Steven Weber. Time Period The Devonian period took place during the Paleozoic era, and lasted from 416 to million years ago.
What is the Earth’s time scale? The Geological time scale is a record of the life forms and geological events in Earth’s history. Scientists developed.
Events in Your Life ___When you started second grade ___When you were born ___ When you started kindergarten ___When you learned to ride a bike. ___ When.
Earth has several layers ► Ch. 3, section 1-unit B ► learn:  Different properties of earth’s layers  About plates that make up the outer most layer of.
Earth Science Essentials North Farmington High School
Chapter 8: Plate TectonicsChapter 8: Plate Tectonics 8.1: Earth has several layers 8.2: Continents change position over time 8.3: Plates move apart 8.4:
- By carefully analyzing landforms, rocks and fossils - A fossil of an animal that was around on earth at a particular time in history.
Plate Tectonics. Earth’s Layers The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. This crust is not a solid.
The Geological Time Scale Apes Topic Outline Earth Systems and Resources (10–15%) Earth Science Concepts (Geologic time scale; plate tectonics, earthquakes,
The Geological Time Scale Events in Your Life ___When you started second grade ___When you were born ___ When you started kindergarten ___When you learned.
Handout 2 Standard 2-2 Geologic Record. Chapter 10 Section 3 EFFECTS OF CONTINENTAL CHANGE.
Northern Highlands Region Wisconsin.  The Geology of Wisconsin  Did you know northern Wisconsin once featured mountains similar to the Alps and the.
The Geological Time Scale
8. 2 Continents change position over time. Learning Goals Students will: -explain how the continental drift hypothesis was developed. -explain evidence.
Drifting Continents 8 th Grade Earth & Space Science Class Notes.
6/23/2016AF Carpinelli 1 The Paleozoic World Life Takes Hold…
Precambrian Time and the Paleozoic Era
Tectonics from the Cambrian into the Future
Evidence for Plate Tectonics
Continental Drift.
Plate Tectonics A Giant Jigsaw Puzzle and Continental Drift
Overview of natural history
Chapter 14: Geologic Time
Section 2: Precambrian Time and the Paleozoic Era
Geologic History.
Section 2: Precambrian Time and the Paleozoic Era
Section 2: Precambrian Time and the Paleozoic Era
GEOLOGIC TIME SCALE. GEOLOGIC TIME SCALE The GEOLOGIC TIME SCALE is a record of the history of the Earth, based major geologic & biologic events.

A Trip Through Geologic Time
Chapter 10 Plate Tectonics.
The Geological Time Scale
And changes in organisms
Geologic Time.
Section 2: Precambrian Time and the Paleozoic Era
The Geological Time Scale
How We Know About Our Past
How do fossils teach us about the environment in ancient times?
Geologic Time Scale.
The Geological Time Scale
Continental Drift (17.2) As people began to draw more accurate maps of the world they were curious about the shape of the continents. It looked as if many.
Journal #62 After putting the continental pieces together on Friday, what did you notice about the continents? What did you notice about the fossils?
Presentation transcript:

Come with us and travel back in time to the geologic period known as the Cambrian Explosion Time Machine Travel Bureau

Pack your bags: it will be cool to start but it will warm up so layering is best. The ocean is huge so if you bring environmentally friendly soap laundry will not be a problem.

Continents are forming so “tourist attractions” are all about nature. In the beginning you will see few plants and animals but once things get started: WOW!!!! When you arrive you will not recognize the place! You will notice that the tectonic plates have gathered together into a continent known as GONDWANA.

The seas are a good place for species to live while the continents are still forming. The sponges and the gastropods are fantastic!

Just look at some of what you may see!

What else will you need? With more ocean than land, sleeping in a raft will be an adventure! A fishing net and pole would be useful. You may be bigger than anything you see, so you should be safe!

The cynobacteria will cause the oxygen levels to increase and make photosynthesis possible so eventually your ability to breathe will increase. Until that time you will be happy that you packed some oxygen.

Just a little history before you leave: Adam Sedgwick named the Cambrian in He derived the name from “Cambria”, the Roman name for Wales. This site had shale and sandstone.

Rocks of this period are in the basins and ranges throughout the western part of the US, the Rocky and Appalachian Mountains, in New England and Wisconsin. But when you go back in time you will see where it all began.

The Middle Cambrian years are known for their Burgess Shale

So make your reservations now! Take the trip of this lifetime (or any other lifetime) Seating is limited.

Sources: