UNIVERSITY OF SOUTH ALABAMA. GY 112: Earth History. Lecture 36: Plio-Pleistocene Geology. Instructor: Dr. Douglas W. Haywick
|
|
|
- Silvester Hancock
- 6 years ago
- Views:
Transcription
1 UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 36: Plio-Pleistocene Geology Instructor: Dr. Douglas W. Haywick
2 Last Time A) Cenozoic Overview and Tectonics Western North American tectonic provinces Plateaus and canyons
3 Cenozoic Time Frame Phanerozoic Era Cenozoic Mesozoic Paleozoic Years (0 to 65 MA) (65 to 245 MA) (245 to 550 MA)
4 Cenozoic Time Frame Period Quaternary (1.6-0 MA) Cenozoic Tertiary ( MA) Epoch Holocene (10,000 0 years) Pleistocene (1,600,000 10,000 years) Pliocene ( MA) Miocene ( MA) Oligocene (37-24 MA) Eocene (58-37 MA) Paleocene (65-58 MA) Introducing the Epochs (the smallest common divisions of geological time)
5 Mammals diversified Cenozoic Life Most modern orders present by Early Eocene
6 Cenozoic Life Primates modernized in Oligocene Monkeys Apelike primates Aegyptopithecus
7 Cenozoic Life Mammalian carnivores evolved by mid- Paleogene
8 Cenozoic Life Spread of C 4 grasses C 4 plants Incorporate more carbon 13 than C 3 grasses Five times more silica Wears down teeth of grazers
9 Cenozoic Deep Ocean Currents Chalk Board
10 Cenozoic Tectonic Events Final breakup of Gondwanna (Australia separated from Antarctica in the Latest Paleocene earliest Eocene epochs) India began to collide with Asia forming the Himalayan Mountain Range (Oligocene to Recent) Africa started to shift northward, gradually sliding under Europe and uplifting the Alps (Oligocene to Recent) Continued westward movement of North America and South America formed an on again off again land bridge between the two continents. This gave rise to some interesting animal exchanges (see evolutionary events below). North American orogenies become dominated by strike-slip faulting and uplift. Mountain building in the northern part of the Cordilleran mountains (mostly Canada) slows down stop during the Oligocene. Activity shifts to the southern part of the mountain chain (Colorado, Nevada etc.). Major late Tertiary flood basalt eruptions occur in Oregon and Washington state. Hot spot volcanism occurs in the area of Yellowstone (Pliocene to present). Composite volcanic eruptions (some incredibly explosive) periodically occurred and still do (e.g., Mt St Helen s).
11 Tectonic Events Cordilleran region Laramide orogeny New tectonic style
12 Cenozoic Tectonics Eocene Tectonic elements:
13 Cenozoic Tectonics Miocene Tectonic elements:
14 Cenozoic Tectonics Modern Tectonic elements:
15 Cenozoic Tectonics As North America drifts to the WNW, we eventually run over the leading edge of the East Pacific Rise Eocene
16 Cenozoic Tectonics As North America drifts to the WNW, we eventually run over the leading edge of the East Pacific Rise Oligocene
17 Cenozoic Tectonics Uplift As North America drifts to the WNW, we eventually run over the leading edge of the East Pacific Rise And uplift now affects the SW Today
18 Cenozoic Tectonics Key tectonic elements: 1) Farallon Plate (east of East Pacific Rise; east drift) 2) Pacific Plate (west of East Pacific Rise; west drift)
19 Cenozoic Tectonics Key tectonic elements: 1) Farallon Plate (east of East Pacific Rise; east drift) 2) Pacific Plate (west of East Pacific Rise; west drift) 3) Juan de Fuca Plate (east of East Pacific Rise; east drift) 4) Cocos Plate (east of East Pacific Rise; east drift)
20 Cenozoic Tectonics Key tectonic style: simple uplift Laramide Orogeny
21 Cenozoic Tectonics Important Basins 1) Green River Basin 2) Uinta Basin 3) Washakie/Sandwash Basins 4) Piceance Creek Basin All are rich in oil shale
22 Cenozoic Tectonics 1) Basin and Range
23 Cenozoic Tectonics 1) Basin and Range 2) Colorado Plateau 3) Columbia River Plateau Basin and Range
24 Cenozoic Tectonics Basin and Range: Uplifted deformed strata
25 Cenozoic Tectonics 1) Basin and Range 2) Colorado Plateau
26 Cenozoic Tectonics 1) Basin and Range 2) Colorado Plateau 3) Columbia River Plateau Colorado Plateau
27 Cenozoic Tectonics Colorado Plateau: Uplifted undeformed strata
28 Cenozoic Tectonics 1) Basin and Range 2) Colorado Plateau 3) Columbia River Plateau
29 Cenozoic Tectonics Miocene Columbia Plateau basalts Up to 5 km thick
30 Cenozoic Tectonics Columbia River Plateau: Basalt lava flow covered terrain
31 Cenozoic Tectonics 1) Basin and Range 2) Colorado Plateau 3) Columbia River Plateau 4) Rio Grande Rift
32 Cenozoic Tectonics Rio Grande Rift: Uplifted rifting strata
33 Today s Agenda A) Finish off Cenozoic Tectonics B) Cenozoic temperature and sea level shifts C) Plio-Pleistocene Glaciations (Milankovitch Orbital Variations) D) Sea level changes in our own back yard Web notes 37
34 Cenozoic Tectonics Other interesting Cenozoic (Recent) Tectonics: 1) Yellowstone
35 Cenozoic Tectonics Other interesting Cenozoic (Recent) Tectonics: 1) Yellowstone 2) Crater Lake
36 Cenozoic Tectonics Other interesting Cenozoic (Recent) Tectonics: 1) Yellowstone 2) Crater Lake 3) Composite Volcanoes
37 Cenozoic Tectonics
38 Plio-Pleistocene Is most notable for rapid, short duration shifts in temperature and ice volume.
39 Plio-Pleistocene Is most notable for rapid, short duration shifts in temperature and ice volume.
40 Plio-Pleistocene Is most notable for rapid, short duration shifts in temperature and ice volume. Why?
41 Plio-Pleistocene Glaciations started around 5 million years ago. Isthmus of Panama Emplaced M years ago Started modern circulation Gulf stream carries salty Atlantic north Cools, sinks Oceanic conveyor belt High latitudes cool
42 Milankovitch Cycles Three major changes in Earth s orbit are linked to glacial oscillations Eccentricity Obliquity Precession
43 Milankovitch Cycles When taken together, the 3 cycles are capable of dropping temperatures globally
44 Milankovitch Cycles When taken together, the 3 cycles are capable of dropping temperatures globally. These cycles have been confirmed via stable isotope analysis of deep sea foraminifera (ice volume).
45 Paleoclimate Phases We now recognize two major Earth climatic phases 1) Greenhouse Earth (no continental glaciers present) 2) Icehouse Earth (continental glaciers present)
46 Paleoclimate Phases Icehouse Earths fluctuate between 2 stages: a) Glacial stage (18 KA) b) Interglacial stage (Today)
47 The Present Ice House Earth Glacial/ interglacial stage Name of stage Time frame interglacial Holocene 0-10 KA glacial Wisconsinian KA interglacial Sangamon KA glacial Illinoisan KA interglacial Yarmouth KA glacial Kansan KA interglacial Aftonian KA glacial Nebraskan > 500 KA
48 The Ice Age Glacial Maximum Extent of continental glaciation Several lines of evidence 1) Erratic boulders
49 The Ice Age 2) Glacial till and basins associated with glaciation 3) Depression of the land Hudson Bay
50 The Ice Age Lowering of sea level Exposed continental shelves
51 The Ice Age Migration of species Mammals crossed Bering Strait on land corridors Vegetation changed in response to global changes
52 The Ice Age Ocean circulation changed during glaciation Glacier in NJ Tundra in Washington, D.C.
53 The Ice Age Great lakes Last glacial maximum 35,000-10,000 years ago Wisconsin Stage Remained when ice sheets melted back
54 The Ice Age Climate impacts were felt globally Steepened temperature gradients Increased aridity Exception: Great Basin Lakes Great Salt Lake
55 The Ice Age Climate impacts were felt globally Sahara expanded Rain forests restricted Isolated gorilla species
56 End of the Ice Age Glaciers began to retreat around 15,000 years ago Waters drained to lakes Sea level rose Tundra shifted northward Deciduous trees migrated northward
57 Transgression Sea Level Lagoonal complexes transgress over coastal plain sediments Regression High sediment supply is causing coast to move offshore Texas
58 In southern Alabama, regressions caused the shoreline to shift 100 miles south. Base level of rivers dropped by 300 feet. Sea Level The Mobile River carved a canyon, the remnants of which are still exposed along the Eastern Shore
59 In southern Alabama, regressions caused the shoreline to shift 100 miles south. Base level of rivers dropped by 300 feet. Sea Level The Mobile River carved a canyon, the remnants of which are still exposed along the Eastern Shore
60 The End
61 Today s Homework 1. Study for finals! 2. Time Chart 3 due now 3. Do the online class survey (1% bonus) 4. Rate my Professor.com Next Time 1. Final Exam
62 GY 112: Earth History Lecture 36: Plio-Pleistocene Instructor: Dr. Doug Haywick This is a free open access lecture, but not for commercial purposes. For personal use only.
Plio-Pleistocene Geology
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Plio-Pleistocene Geology Instructor: Dr. Douglas W. Haywick Last Time A) Cenozoic Tectonics Western North American tectonic provinces Plateaus and canyons
Last Time. Submarine Canyons and Fans. Turbidites. MAS 603: Geological Oceanography. Lecture 16: Greenhouse vs. Icehouse Earths
UNIVERSITY OF SOUTH ALABAMA Last Time MAS 603: Geological Oceanography Lecture 16: Greenhouse vs. Icehouse Earths Submarine Fans Definition and morphology Transport mechanisms (density currents) Submarine
Chapter 19. The Neogene World
Chapter 19 The Neogene World Guiding Questions How did marine life of Neogene time differ from that of Paelogene time? What happened to grasses and grasslands early in Neogene time? Why might we label
Quiz 12 Bonus 2 (9:30-9:35 AM)
Quiz 12 Bonus 2 (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lectures 32 and 33: Mesozoic Sedimentation Instructor: Dr. Douglas W. Haywick Last Time Mesozoic Tectonics A) The Triassic
GY 112: Earth History
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lectures 31: Mesozoic Tectonics Instructor: Dr. Douglas W. Haywick Last Time Mesozoic Overview A) The end of the Paleozoic B) Mesozoic time frame and evolutionary
Mesozoic Earth History Million years ago Triassic Jurassic Cretaceous
Mesozoic Earth History 245-65 Million years ago Triassic Jurassic Cretaceous Geologic Time Scale www.geo.ucalgary.ca/~macrae/timescale/time_scale.gif Main Happenings in Mesozoic Breakup of Pangaea Lots
Cenozoic Earth History I
Cenozoic Earth History I Cenozoic plate tectonics Tertiary, Quaternary, Paleogene, Neogene Tejas Transgression North America s east coast geology Laramide Orogeny Post-Laramide mountain building and volcanism
Unit 5 Possible Test Questions Mesozoic and Cenozoic Eras HISTORICAL GEOLOGY
Revised 8/16 Unit 5 Possible Test Questions Mesozoic and Cenozoic Eras HISTORICAL GEOLOGY Mesozoic Era Eons, Eras and Periods 1. List the Mesozoic periods in order (oldest to youngest). End of the Paleozoic
Cenozoic: Global Events Ma- Present
Cenozoic: Global Events 65.5 Ma- Present Major Tectonic Events The Rise of the Himalayas and Closure of the Tethyan Ocean Caused Climate Change Equatorial Ocean Closed Rifting in Western North America
Chapter 15 Cenozoic Events
Chapter 15 Cenozoic Events The Cenozoic Era 65.5 million years ago to the present Name "Cenozoic" = "new life" or "recent life" The Cenozoic Era followed a mass extinction of the dinosaurs and many other
Geologic Trips San Francisco and the Bay Area
Excerpt from Geologic Trips San Francisco and the Bay Area by Ted Konigsmark ISBN 0-9661316-4-9 GeoPress All rights reserved. No part of this book may be reproduced without written permission in writing,
Outline 23: The Ice Ages-Cenozoic Climatic History
Outline 23: The Ice Ages-Cenozoic Climatic History Continental Glacier in Antarctica Valley Glaciers in Alaska, note the moraines Valley Glaciers in Alaska, note the moraines Mendenhall Glacier, Juneau,
Ch. 19 The Neogene World
Ch. 19 The Neogene World Neogene Period includes Miocene, Pliocene and Pleistocene epochs Beginning of Holocene was approx. 12,000 years ago 12,000 years Cenozoic 1.8 5.3 Neogene 24 Paleogene 65 Holocene
Geos Orogeny-mountain building: existing mountain belts are the result of Cenozoic tectonics. Cenozoic tectonism and climate.
Geos 432-2 Cenozoic tectonism and climates; climate change Orogeny-mountain building: existing mountain belts are the result of Cenozoic tectonics Cenozoic tectonism and climate Movement of continents
Lecture Outlines PowerPoint. Chapter 12 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 12 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
discussion of North America s physical features, including its landforms and bodies of
Chapter 7 Natural Environments of North America Chapter 7 focuses on the natural environments of North America. The chapter opens with a discussion of North America s physical features, including its landforms
Phanerozoic (last 0.54 by) Tectonics Climate Life
Phanerozoic (last 0.54 by) Tectonics Climate Life Tools for Locating Past Continent Positions Fossils depending on climate Alignment of geological features Geometrical fit of continental margins Similarity
Geologic Time. The Cenozoic Era. 7. Mammals evolved after dinosaurs became extinct.
Geologic Time The Cenozoic Era Key Concepts What major geologic events occurred during the Cenozoic era? What does fossil evidence reveal about the Cenozoic era? What do you think? Read the two statements
ATOC OUR CHANGING ENVIRONMENT
ATOC 1060-002 OUR CHANGING ENVIRONMENT Class 22 (Chp 15, Chp 14 Pages 288-290) Objectives of Today s Class Chp 15 Global Warming, Part 1: Recent and Future Climate: Recent climate: The Holocene Climate
Earth s Changing Continents
2 What You Will Learn Earth s continents have moved around Earth s surface throughout Earth s history and have only recently arrived at their current locations. Rocks and fossils provide evidence of continental
12. The diagram below shows the collision of an oceanic plate and a continental plate.
Review 1. Base your answer to the following question on the cross section below, which shows the boundary between two lithospheric plates. Point X is a location in the continental lithosphere. The depth
Physical Geography. Physical Geography. Physical Landscape I of the United States and Canada. Definitions. Physical Geography GEOLOGIC PROCESSES
Physical Landscape I of the United States and Canada Physical Geography Physical landscape (natural environment) sets the stage for human use (the cultural landscape). Prof. Anthony Grande AFG 2016 Landforms
Lecture 18 Paleoceanography 2
Lecture 18 Paleoceanography 2 May 26, 2010 Trend and Events Climatic evolution in Tertiary Overall drop of sea level General cooling (Figure 9-11) High latitude (deep-water) feature Two major step Middle
Physical Geology, 15/e
Lecture Outlines Physical Geology, 15/e Plummer, Carlson & Hammersley Plate Tectonics: The Unifying Theory Physical Geology 15/e, Chapter 19 Plate Tectonics Plate Tectonics Earth s surface is composed
Movement of the Earth s Crust: Formation of: Mountain s Plateau's and Dome s
Movement of the Earth s Crust: Formation of: Mountain s Plateau's and Dome s References Information taken from several places including Prentice Hall Earth Science: @ http://www.eram.k12.ny.us/education/components/docmgr/default.php?sectiondetaili
COOLING DRYING 19 4 CT WT CT AR. mean global temperature levels of aridity latitudinal stratification have all changed appreciably
as we have seen. BIOMES are the biota's adaptive response to earth's climate zones but climate too has a history - - it has evolved through time mean global temperature levels of aridity latitudinal stratification
How do glaciers form?
Glaciers What is a Glacier? A large mass of moving ice that exists year round is called a glacier. Glaciers are formed when snowfall exceeds snow melt year after year Snow and ice remain on the ground
Geologic Time. What have scientists learned about Earth s past by studying rocks and fossils?
Name Geologic Time What have scientists learned about Earth s past by studying rocks and fossils? Before You Read Before you read the chapter, think about what you know about geologic time Record your
Development of the Global Environment
Development of the Global Environment G302: Spring 2004 A course focused on exploration of changes in the Earth system through geological history Simon C. Brassell Geological Sciences simon@indiana.edu
3/5/05 Dr. Stewart 1
I. Physiography of Appalachian Mountains A. Introduction 1. These mountains extend from NE Canada to Georgia 2. They are the remains of a deeply eroded, ancient mountain chain once larger than the Himalayans
Terrain Units PALEOGEOGRAPHY: LANDFORM CREATION. Present Geology of NYS. Detailed Geologic Map of NYS
NYS TOPOGRAPHY Why so? PALEOGEOGRAPHY: LANDFORM CREATION Prof. Anthony Grande AFG 014 Present Geology of NYS Detailed Geologic Map of NYS Generalized Geology Detailed Geology Hot links to the fold out
4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times?
Name Class CHAPTER 3 Date Climate 4 Changes in Climate SECTION National Science Education Standards BEFORE YOU READ After you read this section, you should be able to answer these questions: ES 1k, 2a
GY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 21: Rock Deformation Instructor: Dr. Douglas W. Haywick Last Time A) How long is long? B) Geological time divisions Web notes 20 Geological
Plate Tectonics CHAPTER 17
Plate Tectonics CHAPTER 17 Layers of the Earth A. Crust- solid, 5-70 km thick Moho Two Types of Crust: Oceanic- ocean floor, more dense then because of more iron Continental-dry land (mostly silicates
The Great Ice Ages. Copyright abcteach.com 2001 Graphics from Art Today
The Great Ice Ages The Great Ice Ages occurred during the Pleistocene epoch. The word epoch means time period. This period began about 2.5 million years ago and ended roughly 10,000 years ago. During the
Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education
Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education Tibetan Plateau and Himalaya -southern Asia 11.00.a VE 10X
Mesozoic Era 251 m.y.a 65.5 m.y.a
Mesozoic Cenozoic notes.notebook Mesozoic & Cenozoic 251 m.y.a Present at the end of the Permian, 90% of marine organisms and more than 70% of land organisms died. because resources and space were readily
Directed Reading. Section: How Mountains Form MOUNTAIN RANGES AND SYSTEMS. Skills Worksheet
Skills Worksheet Directed Reading Section: How Mountains Form 1. How high is Mount Everest? a. about 1980 km above sea level b. more than 8 km below sea level c. more than 8 km above sea level d. more
The Pleistocene Ice Ages
The Pleistocene Ice Ages 5 15 25 35 45 55 65 EPOCH QART PLIO CRETACEOUS PALEOCENE EOCENE OLIGOCENE MIOCENE Nalma * Irving./RLB Blancan Hemphillian Clarendonian Barstovian Hemingfordian Arikareean Whitneyan
Physical Geography. Physical Landscape I of the United States and Canada. Definitions. Physical Geography. Physical Geography GEOLOGIC PROCESSES
Physical Landscape I of the United States and Canada Prof. Anthony Grande AFG 2017 Physical Geography Landforms and geologic processes Physical landscape (natural environment) sets the stage for human
The Mesozoic. Wednesday, November 30, 11
The Mesozoic Periods of the Mesozoic Triassic- First period of the Mesozoic era Jurassic Cretaceous- Last period of the Mesozoic era Breakup of Pangaea Stage one (Triassic) Rifting and volcanism, normal
Before Plate Tectonics: Theory of Continental Drift
Before Plate Tectonics: Theory of Continental Drift Predecessor to modern plate tectonics Shape and fit of the continents was the initial evidence Snider-Pelligrini (1858) Taylor (1908) Wegner (1915) Fig.
Unit 1: Geography. For additional information, refer to this website: 1 G e o g r a p h y
Unit 1: Geography For additional information, refer to this website: http://mryoungtms.weebly.com/ 1 G e o g r a p h y Continents and Oceans SOL USI. 2a Essential Understanding: Continents are large land
6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind
Multiple Choice. 1. Heinrich Events a. Show increased abundance of warm-water species of planktic foraminifera b. Show greater intensity since the last deglaciation c. Show increased accumulation of ice-rafted
Chapter 1 Section 2. Land, Water, and Climate
Chapter 1 Section 2 Land, Water, and Climate Vocabulary 1. Landforms- natural features of the Earth s land surface 2. Elevation- height above sea level 3. Relief- changes in height 4. Core- most inner
Mesozoic Earth History
Mesozoic Earth History The Mesozoic Era 251-66 MYA Breakup of Pangea Changes in air and oceanic currents Evolution of new terrestrial and marine life Opening of the Atlantic Ocean Basin Rocky Mountains
In the space provided, write the letter of the definition that best matches the term or phrase.
Skills Worksheet Directed Reading Section: The Changing Continents 1. What is the result of slow movements of tectonic plates? RESHAPING EARTH S CRUST In the space provided, write the letter of the definition
The Building of the NYC Region
The Building of the NYC Region Definitions Fall Line marks the area where an upland region (continental bedrock) and a coastal plain meet Piedmont the plateau region of the eastern United States which
NATS 101 Section 13: Lecture 32. Paleoclimate
NATS 101 Section 13: Lecture 32 Paleoclimate Natural changes in the Earth s climate also occur at much longer timescales The study of prehistoric climates and their variability is called paleoclimate.
Chapter 6, Part Colonizers arriving in North America found extremely landscapes. It looked different to region showing great.
Social Studies 9 Unit 1 Worksheet Chapter 6, Part 1. 1. Colonizers arriving in North America found extremely landscapes. It looked different to region showing great. 2. The Earth is years old and is composed
Lecture 21: Glaciers and Paleoclimate Read: Chapter 15 Homework due Thursday Nov. 12. What we ll learn today:! Learning Objectives (LO)
Learning Objectives (LO) Lecture 21: Glaciers and Paleoclimate Read: Chapter 15 Homework due Thursday Nov. 12 What we ll learn today:! 1. 1. Glaciers and where they occur! 2. 2. Compare depositional and
EQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles.
EQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles. Places & Terms for Discussion Appalachian Mountains Great Plains Canadian Shield
USU 1360 TECTONICS / PROCESSES
USU 1360 TECTONICS / PROCESSES Observe the world map and each enlargement Pacific Northwest Tibet South America Japan 03.00.a1 South Atlantic Arabian Peninsula Observe features near the Pacific Northwest
History. Late 18 th /early 19 th century Europeans observed that erratic boulders dispersed due to the retention of glaciers caused by climate chance
Ice ages What is an ice age? Geological period of long-term reduction in the temperature of the Earth's surface and atmosphere which results in the formation and expansion of continental ice sheets, polar
Continental Landscapes
Continental Landscapes Landscape influenced by tectonics, climate & differential weathering Most landforms developed within the last 2 million years System moves toward an equilibrium Continental Landscapes
8. Climate changes Short-term regional variations
8. Climate changes 8.1. Short-term regional variations By short-term climate changes, we refer here to changes occurring over years to decades. Over this timescale, climate is influenced by interactions
Paleoceanography II Telluric Effects on Oceanography
Paleoceanography II Telluric Effects on Oceanography Geological Oceanography OCN 622 Gary McMurtry Telluric Effects Tellus = Earth Distribution of Continents at 100 Ma BP and Present Comparison of Earth
Lecture Outlines PowerPoint. Chapter 6 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 6 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
Chapter 02 The Sea Floor
Chapter 02 The Sea Floor Multiple Choice Questions 1. One of the following is not one of the world's major ocean basins: A. Atlantic Ocean B. Arctic Ocean C. Indian Ocean D. Antarctic Ocean E. Pacific
Today we will discuss global climate: how it has changed in the past, and how the current status and possible future look.
Global Climate Change Today we will discuss global climate: how it has changed in the past, and how the current status and possible future look. If you live in an area such as the Mississippi delta (pictured)
Reading Material. See class website. Sediments, from Oceanography M.G. Gross, Prentice-Hall
Reading Material See class website Sediments, from Oceanography M.G. Gross, Prentice-Hall Materials filling ocean basins Dissolved chemicals especially from rivers and mid-ocean ridges (volcanic eruptions)
Social Studies. Chapter 2 Canada s Physical Landscape
Social Studies Chapter 2 Canada s Physical Landscape Introduction Canada s geography its landforms and climate - has a great impact on Canadians sense of identity. Planet Earth The earth is divided into
Science 10 PROVINCIAL EXAM STUDY BOOKLET. Unit 4. Earth Science
Science 10 PROVNCAL EXAM STUDY BOOKLET Unit 4 Earth Science Student nstructions 1. Ensure that you have blank paper and a Data Booklet. 2. Record all answers on a separate piece of paper. 3. Answer keys
Chapter 5: Glaciers and Deserts
I. Glaciers and Glaciation Chapter 5: Glaciers and Deserts A. A thick mass of ice that forms over land from the compaction and recrystallization of snow and shows evidence of past or present flow B. Types
Plate Tectonics. Essentials of Geology, 11 th edition Chapter 15
1 Plate Tectonics Essentials of Geology, 11 th edition Chapter 15 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Plate Tectonics: summary in haiku form Alfred Wegener gave us Continental Drift. Fifty years later...
Unit 1: Basics of Geography Test Review
Name Date Period Unit 1: Basics of Geography Test Review Directions: Reading the following sections and complete the questions, charts, and diagrams. Types of Maps Maps that have a particular theme are
Plate Tectonics GEOL 101 Lecture 22 How Are Mountains Built?
Plate Tectonics GEOL 101 Lecture 22 How Are Mountains Built? The Grand Tetons, Wyoming First a Brief Review of Sea Floor Spreading Prop: Test 3 Invitations Break-Up of a Continent and Origin of an Ocean
Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn
Plate Tectonics By Destiny, Jarrek, Kaidence, and Autumn .The Denali Fault and San Andreas Fault - The San Andreas Fault is a continental transform fault that extends roughly 1300 km (810 miles) through
Parts of the Sevier/ Laramide Orogeny
Parts of the Sevier/ Laramide Orogeny AA. Accretionary Prism BB. Forearc Basin Sediment scraped off of subducting plate Sediment derived from the volcanic arc CC. Volcanic Arc Magmatic intrusion into the
AP Environmental Science. Earth Systems: Part 3
AP Environmental Science Earth Systems: Part 3 River Deep, Mountain High Geomorphology-the scientific study of landforms and the processes that shape them Water, water everywhere.. Oceans Arctic Ocean
11 Plate Tectonics Abridged. Japan GEOG /10/2013. Instructor: Pesses 1. Part III Earth s Changing Landscapes
11 Plate Tectonics Abridged Part III Earth s Changing Landscapes Geography 101 Physical Geography: Earth s Surface Landscapes M. Pesses, Antelope Valley College Japan Pictures provided by Prof. Lori Dengler,
Section 1: How Did Life Begin? Chapter 19: History of Life on Earth. Section 2: The Age of Earth
Chapter 19: History of Life on Earth Section 1: How Did Life Begin? I. The Basic Chemicals of Life A. 1920s B. Earth s early oceans contained large amounts of organic molecules C. Molecules formed spontaneously
Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building
Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building 1) A(n) fault has little or no vertical movements of the two blocks. A) stick slip B) oblique slip C) strike slip D) dip slip 2) In a(n) fault,
3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.
1. The map below shows the present-day locations of South America and Africa. Remains of Mesosaurus, an extinct freshwater reptile, have been found in similarly aged bedrock formed from lake sediments
Science 20. Unit C: The Changing Earth. Assignment Booklet C3
Science 20 Unit C: The Changing Earth Assignment Booklet C3 FOR TEACHER S USE ONLY Summary Teacher s Comments Chapter 3 Assignment Total Possible Marks 45 Your Mark Science 20 Unit C: The Changing Earth
Earth s Evolution Through Time
1 2 3 4 5 6 7 8 9 10 11 12 13 14 Earth s Evolution Through Time Earth 9 th edition Chapter 22 Earth s evolution: summary in haiku form Super-continents have come and gone many times: giant bumper cars.
Late Tertiary Volcanism. North Washington. Other Andesite Volcanoes. Southern Washington. High Cascades. High Cascades. Mid-Miocene Miocene to present
Miocene to Present Late Tertiary Volcanism Mid-Miocene Miocene to present Reading: DNAG volume G3, Ch. 7 High Cascade Range Columbia River Snake River Plain Basin and Range Southwestern California Sierra
Name Class Date. In the space provided, write the letter of the definition that best matches the term or phrase.
Skills Worksheet Directed Reading Section: The Changing Continents 1. What is the result of slow movements of tectonic plates? RESHAPING EARTH S CRUST In the space provided, write the letter of the definition
SAMPLE PAGE. pulses. The Ice Age By: Sue Peterson
Page 61 Objective sight words (pulses, intermittent, isotopes, chronicle, methane, tectonic plates, volcanism, configurations, land-locked, erratic); concepts (geological evidence and specific terminology
Glaciers. (Shaping Earth s Surface, Part 6) Science 330 Summer 2005
Glaciers (Shaping Earth s Surface, Part 6) Science 330 Summer 2005 1 Glaciers Glaciers are parts of two basic cycles Hydrologic cycle Rock cycle Glacier a thick mass of ice that originates on land from
Lecture 24: Paleozoic 1:
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 24: Paleozoic 1: Laurentia Instructor: Dr. Douglas W. Haywick Last Time (before the exam) The Cambrian Explosion A) Why a Cambrian explosion B)
PHYSIOGRAPHIC REGIONS OF THE LOWER 48 UNITED STATES
PHYSIOGRAPHIC REGIONS OF THE LOWER 48 UNITED STATES LAURENTIAN UPLAND 1. Superior Upland ATLANTIC PLAIN 2. Continental Shelf (not on map) 3. Coastal Plain a. Embayed section b. Sea Island section c. Floridian
Summary. The Ice Ages and Global Climate
The Ice Ages and Global Climate Summary Earth s climate system involves the atmosphere, hydrosphere, lithosphere, and biosphere. Changes affecting it operate on time scales ranging from decades to millions
Ch. 17 Review. Life in the Cretaceous
Ch. 17 Review Life in the Cretaceous Diversification of diatoms, planktonic forams, calcareous nannoplankton Diversification of mobile predators (especially mollusks and teleost fishes) Origin of the angiosperms
The Proterozoic Part 1
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History The Proterozoic Part 1 Lectures 18/19: Tectonics Instructor: Dr. Douglas W. Haywick Last Time 1) The Early Atmosphere 2) The Oceans and Hydrosphere 3)
Glaciers. Valley and Piedmont Glaciers. Glaciers, Gloobal Warming El Niño and the Southern Oscillation. Ice Age Sea Level on North America
Glaciers, Gloobal Warming El Niño and the Southern Oscillation Glaciers Earth Science: Ch 20, p. 573-581 STM: Ch 25, p. 545-568 Earth Science Chapter 6 p. 154-159, 168-173 Southern Hemisphere Northern
Glaciers Earth 9th Edition Chapter 18 Glaciers: summary in haiku form Key Concepts Glaciers Glaciers Glaciers Glaciers
1 2 3 4 5 6 7 8 9 10 11 12 13 14 Earth 9 th Edition Chapter 18 : summary in haiku form Ten thousand years thence big glaciers began to melt - called "global warming." Key Concepts and types of glaciers.
The Geology of the Cenozoic Era
223 Chapter 25 The Geology of the Cenozoic Era GUIDED STUDY The text chapter should be studied one section at a time. Before you read, preview each section by skimming it, noting headings and boldface
Mt St Helens was know to have entered into active periods that lasted from years once every years over the last 500 years, (Figure 5).
Lecture #8 notes; Geology 3950, Spring 2006; CR Stern May 1980 eruption of Mt St Helens volcano (text pages 183-192 in the 4 th edition and 206-222 in the 5 th edition) Mt St Helens in southwest Washington
Earth Science Lesson 3 Dynamic Earth Processes (Grades 8-12 ) Instruction 3-3 Plate Boundaries
As we told you in a recent Instruction, much of the Earth's lithosphere (its Crust and the top layer of its Outer Mantle) is made up of moving masses of rock called tectonic plates (tectonic means moving).
The Phanerozoic Eon. 542 mya Present. Divided into 3 Eras The Paleozoic, Mesozoic, and Cenozoic Eras
542 mya Present The Phanerozoic Eon Divided into 3 Eras The Paleozoic, Mesozoic, and Cenozoic Eras The ends of the Paleozoic and Mesozoic Eras were marked by mass extinctions The Cenozoic Era is still
Continental Drift. & Plate Tectonics
Continental Drift & Plate Tectonics Alfred Wegener, a German scientist, proposed the hypothesis of CONTINENTAL DRIFT, in 1912. Hypothesis stated: All Earth s continents were once a single landmass (Pangaea)
2 Earth s Changing Continents
CHAPTER 9 SECTION The History of Life on Earth 2 Earth s Changing Continents California Science Standards 7.4.a, 7.4.e, 7.4.f BEFORE YOU READ After you read this section, you should be able to answer these
Climate and Environment
Climate and Environment Oxygen Isotope Fractionation and Measuring Ancient Temperatures Oxygen Isotope Ratio Cycles Oxygen isotope ratio cycles are cyclical variations in the ratio of the mass of oxygen
Question #1: What are some ways that you think the climate may have changed in the area where you live over the past million years?
Reading 5.2 Environmental Change Think about the area where you live. You may see changes in the landscape in that area over a year. Some of those changes are weather related. Others are due to how the
PALEOGEOGRAPHY of NYS. Definitions GEOLOGIC PROCESSES. Faulting. Folding 9/6/2012. TOPOGRAPHIC RELIEF MAP of NYS GRADATIONAL TECTONIC
TOPOGRAPHIC RELIEF MAP of NYS PALEOGEOGRAPHY of NYS Prof. Anthony Grande AFG 2012 Definitions GEOLOGIC PROCESSES Geography: study of people living on the surface of the earth. Geology: the scientific study
A) B) C) D) 4. Which diagram below best represents the pattern of magnetic orientation in the seafloor on the west (left) side of the ocean ridge?
1. Crustal formation, which may cause the widening of an ocean, is most likely occurring at the boundary between the A) African Plate and the Eurasian Plate B) Pacific Plate and the Philippine Plate C)
Mountain Building. Mountain Building
Mountain Building Mountain building has occurred during the recent geologic past American Cordillera the western margin of the Americas from Cape Horn to Alaska Includes the Andes and Rocky Mountains Alpine
The Geology of Sebago Lake State Park
Maine Geologic Facts and Localities September, 2002 43 55 17.46 N, 70 34 13.07 W Text by Robert Johnston, Department of Agriculture, Conservation & Forestry 1 Map by Robert Johnston Introduction Sebago
ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017
ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 Why is there no oceanic crust older than 200 million years? SUBDUCTION If new oceanic crust is being continuously created along the earth