Earth System History, Timeline of Earth Events, Geology Lesson PowerPoint

3. -Please make notes legible and use indentations when appropriate. -Example of indent. -Skip a line between topics -Don’t skip pages -Make visuals clear and well drawn.

4. • RED SLIDE: These are notes that are very important and should be recorded in your science journal. • BLACK SLIDE: Pay attention, follow directions, complete projects as described and answer required questions neatly. Copyright © 2010 Ryan P. Murphy

5. http://sciencepowerpoint.com/Website Link:

8. • Remember: Make the most with the time that you are given.

9. • Remember: Make the most with the time that you are given. Getting a strong education is worth the time.

10. • Remember: Make the most with the time that you are given. Getting a strong education is worth the time. The next few years have a huge impact on the rest of your life.

13. • Journal Question? – If the history of the earth from its formation 4.6 billion years ago until present was put into a 12 hour day…

14. • Journal Question? – If the history of the earth from its formation 4.6 billion years ago until present was put into a 12 hour day… • How many hours, minutes, or seconds have humans been around?

16. If the entire history of the earth was a 12 hour day.

17. Earth Forms

18. Layers of the earth Form

19. Earth Cools

20. Earth Cools

21. Earth Cools

22. Moon Forms

23. Earth Cools

24. Earth

26. Earliest Crystals

27. Earliest Rocks

28. Primitive Life Forms

37. Microbes Begin to produce Oxygen

38. First Cells with Nucleus

39. Explosion of Ocean Life

42. Shelled creatures in oceans

45. Primitive Fish

46. First Insects

47. Amphibians Colonize Land

48. Age of Amphibians

49. Age of Reptiles

50. First Mammals

51. Dinosaurs Dominate

52. First Flowering Plants

53. Extinction of the Dinosaurs

54. Age of Mammals

55. 11:59

56. 11:59 Humans

58. Human existence - The last few seconds of the last minute before midnight.

59. • Video Link! What does this 12 hour comparison sound like in one minute. – http://www.youtube.com/watch?v=YXSEyttblMI

68. What Big Idea does 4.68 Billion years represent?

70. The earth is very old, a lot has changed, and the processes of today happened billions of years ago.

71. “I am only a few thousand years old.” “Incredibly young in Earth’s very long history.”

84. • Earth system history has physical, chemical, and biological components. Copyright © 2010 Ryan P. Murphy Physical: Laws that affect matter, energy and their interaction. -Nature and properties of non-living matter and energy.

85. • Earth system history has physical, chemical, and biological components. Copyright © 2010 Ryan P. Murphy Physical: Laws that affect matter, energy and their interaction. -Nature and properties of non-living matter and energy.

86. • Earth system history has physical, chemical, and biological components. Copyright © 2010 Ryan P. Murphy Physical: Laws that affect matter, energy and their interaction. -Nature and properties of non-living matter and energy. - Matter:

87. • Earth system history has physical, chemical, and biological components. Copyright © 2010 Ryan P. Murphy Physical: Laws that affect matter, energy and their interaction. -Nature and properties of non-living matter and energy. - Matter: Anything that has mass and takes up space.

95. • Earth system history has physical, chemical, and biological components. Copyright © 2010 Ryan P. Murphy Summary: Earth has a group of elements working together. These elements include laws of matter, changes in atoms, and also includes living things. All of these parts working together make up earth the history of the earth.

107. • Laws of nature:

108. • Laws of nature: – How chemicals react?

109. • Laws of nature: – How chemicals react? – How water erodes materials?

110. • Laws of nature: – How chemicals react? – How water erodes materials? – Laws of physics?

111. • Laws of nature: – How chemicals react? – How water erodes materials? – Laws of physics? • These are things that don’t change. They occur today as they did Billions of years ago.

112. • Evolution has also occurred during the earths long history. – Gene Pools can change when… – Populations can shrink • Diseases, extinctions, introduction of new better adapted species, predators. – Non-random mating • Organisms choose strongest mate, ones in similar boundaries, – Mutations in the genes • Genes can change. Some are good, some are bad. • The environment will decide. – Movement in and out of the population • Immigration, gene flow. – Natural selection • Adaptations to the environment that do well replace poor ones. Usually an advancement.

113. • Evolution has also occurred during the earths long history. – Gene Pools can change when… – Populations can shrink • Diseases, extinctions, introduction of new better adapted species, predators. – Non-random mating • Organisms choose strongest mate, ones in similar boundaries, – Mutations in the genes • Genes can change. Some are good, some are bad. • The environment will decide. – Movement in and out of the population • Immigration, gene flow. – Natural selection • Adaptations to the environment that do well replace poor ones. Usually an advancement.

115. • Evolution is the change in the gene pool overtime. – Gene Pools can change when… – Populations can shrink • Diseases, extinctions, introduction of new better adapted species, predators. – Non-random mating • Organisms choose strongest mate, ones in similar boundaries, – Mutations in the genes • Genes can change. Some are good, some are bad. • The environment will decide. – Movement in and out of the population • Immigration, gene flow. – Natural selection • Adaptations to the environment that do well replace poor ones. Usually an advancement.

131.  Principle of superposition: Oldest rocks and fossil are on bottom, youngest on top.

140. Oldest Rock Layers

141. Youngest Rock Layers Oldest Rock Layers

162. • Which three layers of rock could have occurred after a major extinction event? Copyright © 2010 Ryan P. Murphy Extinction: No longer actively living. - Death of the last individual of a species.

163. • Which three layers of rock could have occurred after a major extinction event? Copyright © 2010 Ryan P. Murphy Extinction: No longer actively living. - Death of the last individual of a species.

172. • Activity! Principle of Superposition. – Stack books one at a time. – Teacher will place a playing card every so often into the pile. (From Complicated Top to Simple Bottom) – Unveil the rock layers and types of cards from the most recent (top) to the oldest (bottom). – Record a visual in journal with rocks layers and cards (fossils). Copyright © 2010 Ryan P. Murphy

207. What is longer, the Vendian Period or the Paleozoic Era?

210. What is longer, the Eocene Epoch or the Tertiary Period or the Paleozoic Era?

213. What is longer, the Mesozoic Era or the Proterozoic Eon?

216. The Jurassic Period belongs in what Era?

217. The Jurassic Period belongs in what Era? Answer: Mesozoic Era

218. The Pilocene Epoch belongs to this Period?

219. The Pliocene Epoch belongs to this Period?

220. The Pliocene Epoch belongs to this Period? Answer: Tertiary Period

221. The Tertiary Period belongs to this Era?

222. The Tertiary Period belongs to this Era?

223. The Tertiary Period belongs to this Era? Answer: Cenozoic Era

224. The Cenozoic Era belongs to this Eon?

225. The Cenozoic Era belongs to this Eon?

226. The Cenozoic Era belongs to this Eon? Answer: Phanerozoic Eon

227. Describe all of the units of time that the Cambrian is part of?

228. Describe all of the units of time that the Cambrian is part of?

229. Describe all of the units of time that the Cambrian is part of? Answer: Cambrian Period

230. Describe all of the units of time that the Cambrian is part of? Answer: Cambrian Period Paleozoic Era

231. Describe all of the units of time that the Cambrian is part of? Answer: Cambrian Period Paleozoic Era Phanerozoic Eon

232. Describe all of the units of time that the Pleistocene is part of?

233. Describe all of the units of time that the Pleistocene is part of? Pleistocene Epoch

234. Describe all of the units of time that the Pleistocene is part of? Pleistocene Epoch Quaternary Period

235. Describe all of the units of time that the Pleistocene is part of? Pleistocene Epoch Quaternary Period Cenozoic Era

236. Describe all of the units of time that the Pleistocene is part of? Pleistocene Epoch Quaternary Period Cenozoic Era Phanerzoic Eon

237. Which time unit makes up the most of Earth’s History?

238. Which time unit makes up the most of Earth’s History? The Precambrian Super-Eon

239. Certain events / changes on Earth mark the end of one time period, and the start of another.

240. Certain events / changes on Earth mark the end of one time period, and the start of another. Often these are extinction events.

254. The Earth is a fragile system that has…

255. The earth has changed many times and most species go extinct.

256. • Are you ready for the scary piece of knowledge on the next slide.

257. • Are you ready for the scary piece of knowledge on the next slide.

274. Where are the extinction events below?

307. “I’m waiting.” “99.5%”

308. “I’m waiting.” “99.5%” Learn more at http://www.bbc.co.uk/nature/history_of _the_earth

309. • Video Link! (Optional) Hank explains mass extinctions. – Preview for language – http://www.youtube.com/watch?v=FlUes_NPa6M

310. • You should be close to page 3 of your Earth System History homework.

317. • Activity! Making a timeline of Earth’s long history on a paper roll.

318. • Activity: Making a timeline of Earth System History. – http://serc.carleton.edu/quantskills/activities/c alculatortape.html

319. 4.56 meters

320. 4.56 meters

321. 4.56 meters

322. 4.56 meters

323. 4.56 meters

324. 4.56 meters

325. 4.56 meters 500 m.y. 500 m.y

326. 4.56 meters 500 m.y. 500 m.y

327. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250

328. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250

329. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 650 m.y.a

332. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Proteorzoic Eon Starts Here

333. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Archean Eon Starts Here

334. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Archean Eon Starts Here

335. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Set-up timeline so you can see screen over the next few days.

336. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250

337. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Proterozoic Eon Paleozoic Era Mesozoic Era Cenozoic Era

345. • Website to gather info / pictures for timeline: – http://www.totallydifferent.co.uk/fossils/Geologic al_Timeline.html

348. • Please draw pictures and include text on your timeline as we cover them in the slideshow. – Get your timeline ready, pencils, markers etc, sketch as we move down the timeline. – Your group must work together in a small space which is 75% of the challenge.

350. • Precambrian 4.5 to 3.8 billion years ago. Solar system forms

351. Planet forming disk around a star. (artistic)

358. • Video Link! (Optional) Star and planet formation. – http://www.youtube.com/watch?v=Uhy1fucSRQI

359. • Protoplanet: a hypothetical whirling gaseous mass within a giant cloud of gas and dust that rotates around a sun and is believed to give rise to a planet.

360. • Precambrian • Hadean, Archean, and Proterozoic Eon’s – - – - – - – - – -

370. • How did the moon get here / form?

371. • Theories on how moon was formed? – The Fission Theory: The Moon was once part of the Earth and somehow separated from the Earth early in the history of the Solar System. The present Pacific Ocean basin is the most popular site for the part of the Earth from which the Moon came. – The Capture Theory: The Moon was formed somewhere else, and was later captured by the gravitational field of the earth. – The Condensation Theory: The Moon and the Earth condensed together from the original nebula that formed the Solar System. – The Colliding Planetesimals Theory: The interaction of earth- orbiting and Sun-orbiting planetesimals (very large chunks of rocks like asteroids) early in the history of the Solar System led to their breakup. The Moon condensed from this debris. – The Ejected Ring Theory: A planetesimal the size of Mars struck the earth, ejecting large volumes of matter. A disk of orbiting material was formed, and this matter eventually condensed to form the Moon in orbit around the earth.

372. • Theories on how moon was formed? – The Fission Theory: The Moon was once part of the Earth and somehow separated from the Earth early in the history of the Solar System. The present Pacific Ocean basin is the most popular site for the part of the Earth from which the Moon came. – The Capture Theory: The Moon was formed somewhere else, and was later captured by the gravitational field of the earth. – The Condensation Theory: The Moon and the Earth condensed together from the original nebula that formed the Solar System. – The Colliding Planetesimals Theory: The interaction of earth- orbiting and Sun-orbiting planetesimals (very large chunks of rocks like asteroids) early in the history of the Solar System led to their breakup. The Moon condensed from this debris. – The Ejected Ring Theory: A planetesimal the size of Mars struck the earth, ejecting large volumes of matter. A disk of orbiting material was formed, and this matter eventually condensed to form the Moon in orbit around the earth.

402. Theories on moon formation, Learn more: http://www.universetoday.com/47996/how-was-the-moon- formed/

406. • Video Link! Formation of the moon. – http://www.youtube.com/watch?v=ibV4MdN5wo0

407. • Video Link! Formation of the Moon – Longer Version – http://www.youtube.com/watch?v=m8P5ujNwEwM

408. • It’s warmer in summer time because… – A.) The sun increases its energy during the summer. – B.) The earth is closer to the sun in the summer and further away in the winter. – C.) The greenhouse effect is intensified as plants grow more in the summer. – D.) The axial tilt of the planet at 23.5º causes the seasons as more direct light hits our area of the planet during this time. – E.) Ocean currents from the polar regions do not flow south during the summer.

412. • It’s warmer in summer time because… – A.) The sun increases its energy during the summer. – B.) The earth is closer to the sun in the summer and further away in the winter. – C.) The greenhouse effect is intensified as plants grow more in the summer. – D.) The axial tilt of the planet at 23.5º causes the seasons as more direct light hits our area of the planet during this time. – E.) Ocean currents from the polar regions do not flow south during the summer. “Thank you Protoplanet Theia for crashing into earth 4.533 Billion years ago.”

413. • Water molecules found inside salt crystals of meteorites.

414. • Water molecules found inside salt crystals of meteorites. – The earth was bombarded for billions of years, each meteorite carrying with it small amounts of liquid water.

415. • Amino acids, which are the building blocks of proteins have been found inside meteorites.

416. • Atmosphere originates (No oxygen yet).

419. • The first oceans…

420. • The first oceans…

421. • The first continents

422. • A long time goes by and then…

424. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Paleozoic Era Mesozoic Era Cenozoic Era

425. • Earliest life begins (primitive protocells).

426. • A long time goes by and then…

427. • Earth became frozen.

436. • Picture of earliest fossilized cyanobacteria at 3.4 billion years old. Copyright © 2010 Ryan P. Murphy Bacteria: Very small single celled organisms. -They reproduce by splitting in half. - Very primitive internal structure. No nucleus.

439. • Supercontinents form (Rodinia)

440. • Explosion of new animals (sea)

441. This black space represents the Precambrian Super-Eon of Earth’s History 87%

442. his black space represents the other 13% of ime. From the first multi-cellular life to now.

444. Human Species

458. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Proterozoic Eon

461. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Proterozoic Eon

462. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Proterozoic Eon Paleozoic Era Cenozoic Era

466. • Paleozoic Era – Vendian, Cambrian, Ordovican, Silurian, Devonian, Carboniferous, and Permian Periods. • - • - • - • - • - • - • -

475. • Video Link! Animation of Paleozoic Sea Life at Field Museum in Chicago. (Cambrian) – http://www.youtube.com/watch?v=LbhGWDjOkP0

486. • Activity! Making a fossil in the Burgess Shale. – Obtain a piece of clay. – Smooth it out so it is long and flat. – Press shells into it to make fossil imprints. – Pass to friend and record shapes in journal. Copyright © 2010 Ryan P. Murphy

505. Millions of Years

507. • Carboniferous swamps become our fossil fuels.

510. • First Reptiles

518. Most massive extinction event the planet had ever seen. Environmental change, impact event, volcanism, and sea floor methane release.

520. “99.5%”

521. • Video Link! The Arrival of Life (Optional) – http://www.youtube.com/watch?v=7dhSjKrLtPQ

522. • Video Link! Part 2 The Arrival – Lots of Info about Burgess Shale and Cambrian Explosion. – http://www.youtube.com/watch?v=-Ii-tGeuYCs

531. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Proterozoic Eon Paleozoic Era Cenozoic Era

532. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Proterozoic Eon Paleozoic Era Mesozoic Era

533. • Mesozoic Era – Triassic, Jurassic, Cretaceous Periods • - • - • - • - • -

547. “99.5%”

548. 20

549. 20

550. • The Supercontinent Pangea began to split in the middle / late Jurassic. (Plate Tectonics) 20

553. Some theories suggest that…. The reptiles used more of their energy for growing and less for keeping their bodies warm compared with some creatures. They were lukewarm blooded.

554. Some theories suggest that…. Also lots of oxygen, carbon dioxide, and a lush planet had lots of food. Learn more at… http://www.msnbc.msn.com/id/317 68901/ns/technology_and_science- science/t/why-dinosaurs-could- grow-so-big/#.ULJJm4Ytd8E

570. • An ornithologist is a scientist who studies birds.

571. • An ornithologist is a scientist who studies birds.

572. • Activity! Who is king of the dinosaurs in this class. – Each student gets an old cd. – Each slide will present two dinosaurs. – Choose the right dinosaur and you keep your token. – Choose the wrong dinosaur and you lose your token. – Who will be able to survive all of the rounds?

582. • Which is Dilophosaurus?

583. • Which is Dilophosaurus?

584. • Which is Dilophosaurus? Triceratops

597. • Which is a Theropod?

598. • Which is a Theropod?

599. • Which is a Velociraptor?

600. • Which is a Velociraptor?

601. • Which is a Pteradactyl?

602. • Which is a Pteradactyl?

604. • Which one is Spinosaurus?

605. • Which one is Spinosaurus?

606. • Which one is Spinosaurus? Tyrannosaurus TyrannosaurusTyrannosaurus

607. • Which one is Spinosaurus? Tyrannosaurus TyrannosaurusTyrannosaurus These two dinosaurs did not live during the same time period.

609. • Which is a Tylosaurus?

610. • Which is a Tylosaurus?

611. • This is the Frilled Shark – Alive on Earth today in the deeper waters of the ocean.

613. • Video Link! Walking with Dinosaurs, The Ballad of Big Al. – http://www.youtube.com/watch?v=cubdagTiRHE – http://www.youtube.com/watch?v=i9IjL2RCFoI – http://www.youtube.com/watch?v=r1yv7Pi78Og

614. • Video Link! Dinosaur Song. • http://www.youtube.com/watch?v=W0FOZ 0-VpcU

615. • First birds.

618. • Birds came from Theropods. – How are they similar and different?

626. • Similar – Three toed foot. – Walk on two legs. – Hollow bones. – Wishbone. – Backward pointing pelvis. – Theropods did have feathers. Copyright © 2010 Ryan P. Murphy Hollow bones are lightweight so birds can fly more efficiently.

631. • Different

632. • Different – Theropods arms are longer / no wings.

633. • Different – Theropods arms are longer / no wings. – Changes in wrist.

634. • Different – Theropods arms are longer / no wings. – Changes in wrist. – More pronounced feathers in modern birds?

635. • First mammals.

636. • First mammals. Early mammals. Learn more at… http://www.earthlife.net/mammals/evolution.html

646. • A layer of Iridium can be found across the globe in rock layers around 65 million years ago.

647. • A layer of Iridium can be found across the globe in rock layers around 65 million years ago.

648. • A layer of Iridium can be found across the globe in rock layers around 65 million years ago. – Iridium is found on Meteorites.

654. • A layer of Iridium can be found across the globe in rock layers around 65 million years ago. K-T Mass Extinction Event – Iridium is found on Meteorites.

657. • K-T mass extinction event...(Debate Exists) – Combination of Impact event. – Volcanism. – Disease.

658. • K-T mass extinction event...(Debate Exists) – Combination of Impact event. – Volcanism. – Disease. Learn more about the extinction of the dinosaurs at… http://www.pbs.org/wg bh/evolution/extinction /dinosaurs/asteroid.ht ml

659. • Optional PowerPoint. – Found in Activities folder – Asteroids, Impact Craters, and Torino Scale

660. • Without this extinction event, the odds are…

661. • The age of Mammals wouldn’t have happened.

662. • Age of Mammals wouldn’t have happened.

666. “I love a good Mammal.”

667. • The age of dinosaur dominance was over.

668. • The age of dinosaur dominance was over.

669. • The age of dinosaur dominance was over. 99.5%

670. • The age of dinosaur dominance was over. The age of mammals begins.

671. • The age of dinosaur dominance was over. The age of mammals begins.

672. “It’s nice not having all those dinosaurs around, now I can rise to power.”

673. “Hey Mammal!” 99.5% Read more about the extinction event at… http://www.ucmp.berkeley.edu/education/events/cowe n1b.html

674. • Last little bit about dinosaurs. – They ruled this planet for 183 million years. – That is a long time!

677. • Video Link! Building a Dinosaur – http://www.youtube.com/watch?v=dZMQOe9 RQ4Y

678. • Video Link! (Optional) Life After Dinosaurs – http://www.youtube.com/watch?v=b7QSwAhMuUY

679. 4.56 meters 500 m.y. 500 m.y 250 m.y. 250 Hadeon Eon Archean Eon Proterozoic Eon Paleozoic Era Mesozoic Era

681. • Cenozoic Era – Tertiary, and Quaternary Periods • - • - • - • - • - • -

685. • Mammals continued to radiate but still had to hide from the Terror Birds of the Cenozoic. – Phorusrhacids

686. • Mammals continued to radiate but still had to hide from the Terror Birds of the Cenozoic. – Phorusrhacids

689. Present Day Bird Species Size Comparison

696. “Imagine how cool it would be to have these Terror Birds running around today.”

701. • Eventually, Larger mammals evolved that were able to prey upon the Terror Birds and caused their extinction.

705. 47 million year old primate fossil. “Ida”

707. • Panama attaches South America to North America

708. • Panama attaches South America to North America

715. • Answer! Many animals species in S. America rush into N. America and vice versa.

716. • Answer! Many animals species in S. America rush into N. America and vice versa. – Increased competition causes many extinctions.

729. • First human hominids.

730. • Modern Man (Whoa)

731. • Early Clovis hunters found an abundance of animals to hunt during this time period.

732. • Early Clovis hunters found an abundance of animals to hunt during this time period. Many of these animals had never encountered human hunters.

733. • Early Clovis hunters found an abundance of animals to hunt during this time period. Many of these animals had never encountered human hunters. Many were an easy kill

734. • Early Clovis hunters found an abundance of animals to hunt during this time period. Many of these animals had never encountered human hunters. Many were an easy kill “kind of”.

735. • Early Clovis hunters found an abundance of animals to hunt during this time period. Many of these animals had never encountered human hunters. Many were an easy kill “kind of”. Humans thrived, and these animals became extinct. (Theory)

737. • A tar pit is a place where bitumen “form of crude oil” seeps to the surface. – Animals can become trapped and die.

738. • Tour of Megafuana from the past – Megafuana are large animals.

739. • Tour of Megafuana from the past – Megafuana are large animals. Our Tour 23 M.Y.A

740. • Tour of Megafuana from the past – Megafuana are large animals. Our Tour 23 M.Y.A

741. • Tour of Megafuana from the past – Megafuana are large animals. Extinction Event

742. • Giant Ground Sloth

743. • Giant Ground Sloth

744. • Giant Armadillo

745. • Giant Armadillo

746. • Dire Wolf

747. • Dire Wolf

748. • Short Faced Bear

749. • Short Faced Bear

750. • Short Faced Skunk

751. • Short Faced Skunk

752. • American Lion

753. • American Lion

754. • Saber-toothed Cats

755. • Saber-toothed Cats

756. • Smilodon – A specific Saber Toothed Cat

757. • Smilodon – A specific Saber Toothed Cat

758. • Giant Beaver

759. • Giant Beaver

760. • Hyaenodon

761. • Hyaenodon

762. • North American Horses

763. • North American Horses

764. Giant Beaver• North America Tapir

765. Giant Beaver• North America Tapir

766. • Peccaries

767. • Peccaries

768. • Stag Moose

769. • Stag Moose

770. • Wooly Rhino

773. • Moeritherium

774. • Moeritherium

775. • The Columbian Mammoth

776. • The Columbian Mammoth

777. • American Mastodon

778. • American Mastodon

779. • Wooly Mammoth

780. • Wooly Mammoth

782. Which is a Mammoth and which is a Mastodon?

785. Both about size of Asian Elephant

786. Both about size of Asian Elephant Thick Coat

787. Both about size of Asian Elephant Thick Coat and peaked forehead

788. Both about size of Asian Elephant Thick Coat and peaked forehead and hump and curved tusk

789. Both about size of Asian Elephant Thick Coat and peaked forehead and hump and curved tusks

790. • Baluchiterium -Largest mammal ever known

791. • Baluchiterium -Largest mammal ever known

792. • North American Camel.

793. • North American Camel.

794. • Giant Cheetah

795. • Giant Cheetah

796. • Dinohyus “Terrible Pig”

797. • Dinohyus “Terrible Pig”

798. • Bear Dog

799. • Bear Dog

800. • Bear Dog

801. • Dinictus

802. • Dinictus

803. • Andrewsarchus

804. • Andrewsarchus

805. • Chalicotherium

806. • Chalicotherium

807. • Uintatherium

808. • Uintatherium

809. • Doedicurus

810. • Doedicurus

811. • California Condor

812. • California Condor

813. • California Condor “All of the megafauna are gone..”

816. Woolly Rhino Coelodonta

817. Woolly Rhino Coelodonta

818. Woolly Rhino Coelodonta Mammoth

819. Woolly Rhino Coelodonta Mammoth

820. Woolly Rhino Coelodonta Mammoth Stag Moose

823. Giant Ground Sloth

824. Giant Ground Sloth

825. Giant Ground Sloth Giant Armadillo

826. Giant Ground Sloth Giant Armadillo

827. Giant Ground Sloth Giant Armadillo Mastodon or Mammoth

828. Giant Ground Sloth Giant Armadillo Mammoth

829. Giant Ground Sloth Giant Armadillo Mammoth

830. Giant Ground Sloth Giant Armadillo Mammoth Saber-toothed cats Smilodon

874. Learn more about ice age animals at… http://exhibits.museum.state.il.us/exhib its/larson/ice_age_animals.html

875. • Video Links! Walking with Prehistoric Giants, Many Large Mammals that were abundant during the Ice Age even though focus is earlier during the Olgiocene Epoch.

876. • Video Links! Walking with Prehistoric Giants, Many Large Mammals that were abundant during the Ice Age even though focus is earlier during the Olgiocene Epoch. • Caution! All videos are animations but some images may be disturbing.

877. • Video Links! (Optional) • Walking with Prehistoric Beasts – Part I:http://www.youtube.com/watch?v=jW9hO- KE1rU&feature=related – Part II: http://www.youtube.com/watch?v=CJcmfu2noFo&feature=fvwrel – Part III: http://www.youtube.com/watch?v=PCJHwZsFUso&feature=related

900. The Earth is a fragile system that has…

901. The earth has changed many times and most species go extinct.

933. “99.5% of all organisms from the very long history Of the earth have gone extinct.”

934. “I have your number strange primate mammal.”

935. • You should be close to the end of your Earth System History homework.

936. • You should be close to page 3 of your Earth System History homework.

937. • and page 4…

938. • Activity! (Optional) Dinosaur or other Paleo organism Project. – Each student is to pick a specific member organism from the past. – If you don’t know what to do, pick an organism from from a time period to get started. • Paleozoic Era: http://www.fossilmuseum.net/Paleobiology/Paleozoic_p aleobiology.htm • Dinosaurs: http://www.rareresource.com/a- z_dinosaurs_list.htm • Ice Age Mammals: http://exhibits.museum.state.il.us/exhibits/larson/ice_ag e_animals.html#

939. • Possible Projects – Poster board and research. – Video project? – Museum exhibit? – PowerPoint – Research paper. – Dramatic Skit – Board Game – Brochure – Song – Teach the class (Impressions?) – Others (See teacher)

952. Range that it lived and other neat facts. Physical / Anatomical Characteristics of your animal. Behavior / Diet. Describe interesting behaviors, how it finds food, etc. When did it live? Era, Period, Epoch

953. • Video Link! Earth History Crash Course. – Optional and Advanced. – http://www.youtube.com/watch?v=sjE-Pkjp3u4 Bring in your timeline sheet

954. • Earth System History Review Game Bring in your timeline sheet

955. • “AYE” Advance Your Exploration ELA and Literacy Opportunity Worksheet – Visit some of the many provided links or.. – Articles can be found at (w/ membership to NABT and NSTA) • http://www.nabt.org/websites/institution/index.php?p= 1 • http://learningcenter.nsta.org/browse_journals.aspx?j ournal=tst Please visit at least one of the “learn more” educational links provided in this unit and complete this worksheet

956. • “AYE” Advance Your Exploration ELA and Literacy Opportunity Worksheet – Visit some of the many provided links or.. – Articles can be found at (w/ membership to and NSTA) • http://www.earthmagazine.org/ • http://learningcenter.nsta.org/browse_journals.aspx?jo urnal=tst

959. • This part of the PowerPoint roadmap is just one small part of my Geology Topics Unit. This unit includes… • A six part 6,000 Slide PowerPoint Presentation / unit roadmap full of activities, review questions, games, video links, flashcards, materials list, and much more. • A 18 bundled homework package, modified version, 19 pages of unit notes, 6 PowerPoint Review Games of 100+ slides each, videos, rubrics, and much more that all chronologically follow the unit slideshow. • This is a fantastic unit for any Earth Science Class. • http://sciencepowerpoint.com/Geology_Unit.html

961. Areas of Focus within The Geology Topics Unit: -Areas of Focus within The Geology Topics Unit: Plate Tectonics, Evidence for Plate Tectonics, Pangea, Energy Waves, Layers of the Earth, Heat Transfer, Types of Crust, Plate Boundaries, Hot Spots, Volcanoes, Positives and Negatives of Volcanoes, Types of Volcanoes, Parts of a Volcano, Magma, Types of Lava, Viscosity, Earthquakes, Faults, Folds, Seismograph, Richter Scale, Seismograph, Tsunami’s, Rocks, Minerals, Crystals, Uses of Minerals, Types of Crystals, Physical Properties of Minerals, Rock Cycle, Common Igneous Rocks, Common Sedimentary Rocks, Common Metamorphic Rocks., Age of the Earth, Uniformitarianism, Principle of Superposition, Earth History, Time Units, Timeline of Events, Basic Evolution, Mass Extinction Events, Dinosaurs, Early Mammals, and more. Full Unit can be found at… http://sciencepowerpoint.com/Geology_U nit.html

968. • This was a very brief tour. Please visit the links below to learn more about each of the units in this curriculum package. – These units take me about four years to complete with my students in grades 5-10. Earth Science Units Extended Tour Link and Curriculum Guide Geology Topics Unit http://sciencepowerpoint.com/Geology_Unit.html Astronomy Topics Unit http://sciencepowerpoint.com/Astronomy_Unit.html Weather and Climate Unit http://sciencepowerpoint.com/Weather_Climate_Unit.html Soil Science, Weathering, More http://sciencepowerpoint.com/Soil_and_Glaciers_Unit.html Water Unit http://sciencepowerpoint.com/Water_Molecule_Unit.html Rivers Unit http://sciencepowerpoint.com/River_and_Water_Quality_Unit.html = Easier = More Difficult = Most Difficult 5th – 7th grade 6th – 8th grade 8th – 10th grade

969. Physical Science Units Extended Tour Link and Curriculum Guide Science Skills Unit http://sciencepowerpoint.com/Science_Introduction_Lab_Safety_Metric_Methods. html Motion and Machines Unit http://sciencepowerpoint.com/Newtons_Laws_Motion_Machines_Unit.html Matter, Energy, Envs. Unit http://sciencepowerpoint.com/Energy_Topics_Unit.html Atoms and Periodic Table Unit http://sciencepowerpoint.com/Atoms_Periodic_Table_of_Elements_Unit.html Life Science Units Extended Tour Link and Curriculum Guide Human Body / Health Topics http://sciencepowerpoint.com/Human_Body_Systems_and_Health_Topics_Unit.html DNA and Genetics Unit http://sciencepowerpoint.com/DNA_Genetics_Unit.html Cell Biology Unit http://sciencepowerpoint.com/Cellular_Biology_Unit.html Infectious Diseases Unit http://sciencepowerpoint.com/Infectious_Diseases_Unit.html Taxonomy and Classification Unit http://sciencepowerpoint.com/Taxonomy_Classification_Unit.html Evolution / Natural Selection Unit http://sciencepowerpoint.com/Evolution_Natural_Selection_Unit.html Botany Topics Unit http://sciencepowerpoint.com/Plant_Botany_Unit.html Ecology Feeding Levels Unit http://sciencepowerpoint.com/Ecology_Feeding_Levels_Unit.htm Ecology Interactions Unit http://sciencepowerpoint.com/Ecology_Interactions_Unit.html Ecology Abiotic Factors Unit http://sciencepowerpoint.com/Ecology_Abiotic_Factors_Unit.html

970. • More Units Available at… Earth Science: The Soil Science and Glaciers Unit, The Geology Topics Unit, The Astronomy Topics Unit, The Weather and Climate Unit, and The Rivers and Water Quality Unit, The Water Molecule Unit. Physical Science: The Laws of Motion and Machines Unit, The Atoms and Periodic Table Unit, The Energy and the Environment Unit, and Science Skills Unit. Life Science: The Diseases and Cells Unit, The DNA and Genetics Unit, The Life Topics Unit, The Plant Unit, The Taxonomy and Classification Unit, Ecology: Feeding Levels Unit, Ecology: Interactions Unit, Ecology: Abiotic Factors, The Evolution and Natural Selection Unit and The Human Body Systems and Health Topics Unit Copyright © 2010 Ryan P. Murphy

971. • The entire four year curriculum can be found at... http://sciencepowerpoint.com/ Please feel free to contact me with any questions you may have. Thank you for your interest in this curriculum. Sincerely, Ryan Murphy M.Ed www.sciencepowerpoint@gmail.com

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