PHYSIOGRAPHIC REGIONS OF THE LOWER 48 UNITED STATES
|
|
|
- Marjory Moore
- 6 years ago
- Views:
Transcription
1 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 section d. East Gulf Coastal Plain e. Mississippi Alluvial Plain f. West Gulf Coastal Plain APPALACHIAN HIGHLANDS 4. Piedmont province a. Piedmont Upland b. Piedmont Lowlands 5. Blue Ridge province a. Northern section b. Southern section 6. Valley and Ridge province a. Tennessee section b. Middle section c. Hudson Valley 7. St. Lawrence Valley a. Champlain section b. Northern section (not on map) 8. Appalachian Plateaus province a. Mohawk section b. Catskill section c. Southern New York section d. Allegheny Mountain section e. Kanawha section f. Cumberland Plateau section g. Cumberland Mountain section 9. New England Province a. Seaboard Lowland section b. New England Upland section c. White Mountain section d. Green Mountain section e. Taconic section 10. Adirondack province INTERIOR PLAINS 11. Interior Low Plateaus a. Highland Rim section b. Lexington Plain c. Nashville Basin 12. Central Lowland a. Eastern Lake section b. Western Lake section c. Wisconsin Driftless section d. Till Plains e. Dissected Till Plains f. Osage Plains 13. Great Plains province a. Missouri Plateau, glaciated b. Missouri Plateau, unglaciated c. Black Hills d. High Plains e. Plains Border f. Colorado Piedmont g. Raton section h. Pecos Valley i. Edwards Plateau j. Central Texas section INTERIOR HIGHLANDS 14. Ozark Plateaus a. Springfield-Salem plateaus b. Boston "Mountains" 15. Ouachita province a. Arkansas Valley b. Ouachita Mountains ROCKY MOUNTAIN SYSTEM 16. Southern Rocky Mountains 17. Wyoming Basin 18. Middle Rocky Mountains 19. Northern Rocky Mountains INTERMONTANE PLATEAUS 20. Columbia Plateau a. Walla Walla Plateau b. Blue Mountain section c. Payette section d. Snake River Plain e. Harney section 21. Colorado Plateaus a. High Plateaus of Utah b. Uinta Basin c. Canyon Lands d. Navajo section e. Grand Canyon section f. Datil section 22. Basin and Range province a. Great Basin b. Sonoran Desert c. Salton Trough d. Mexican Highland e. Sacramento section PACIFIC MOUNTAIN SYSTEM 23. Cascade-Sierra Mountains a. Northern Cascade Mountains b. Middle Cascade Mountains c. Southern Cascade Mountains d. Sierra Nevada 24. Pacific Border province a. Puget Trough b. Olympic Mountains c. Oregon Coast Range d. Klamath Mountains e. California Trough f. California Coast Ranges g. Los Angeles Ranges 25. Lower California province
2
3 \ A Tapestry of Time and Terrain: The Union of Two Maps - Geology and Topography
4 Rocks of Ages: An explanation of the legend Geologists subdivide time variously by eras (Precambrian to Cenozoic), periods (Cambrian to Quaternary), and epochs - only Pleistocene (early Quaternary) and Holocene (late Quaternary) are used here (see column at left). These units are quite uneven in elapsed time, the older intervals generally being of much longer duration. Rocks in the U.S. range in age from early Precambrian (2.6 billion years ago) to Holocene, which includes the present. The orderly sequence of Earth materials, from oldest to youngest, is represented by an equally well-ordered sequence of "prismatic" colors (based on the rainbow). To improve the color balance of the tapestry, the Holocene is represented by two hues, light gray in the East and beige in the West. The King and Beikman geologic map of the U.S. was compiled from many detailed maps that describe the rocks of smaller areas. The constituent maps were made by many individuals from field and laboratory observations. These geologic maps distinguish among types of rocks that form in different ways: igneous granite and basalt; sedimentary sandstone, shale, and limestone; and metamorphic slate, marble, gneiss, and schist. From several converging lines of evidence fossils, the layered sequence of strata, and the systematic radioactive decay of certain minerals - geologists have been able to place the rock formations in their correct time order, and from that arrangement construct a sequence of likely geologic events.
5
Topography of the conterminous United States
Topography of the conterminous United States Potential Natural Vegetation Geology Coastal Ranges physiographic province Cascade-Sierra Mountains Cascades Mount Hood California central valley Sierra-Nevada
Physiographic Provinces (West, Ch. 13)
Geology 229 Engineering Geology Lecture 13 Physiographic Provinces (West, Ch. 13) The definition of the term Physiography Physiography (n.) The science which treats of the earth's exterior physical features,
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
The United States & Canada. A Regional Study of Anglo America
A Regional Study of Anglo America Landform Regions of the United States & Canada world leaders in agricultural and industrial production because of... VAST LANDS stretch from the Atlantic Ocean on the
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
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
Basin & Range / Mojave Desert
Basin & Range / Mojave Desert Basin & Range vs. Great Basin 1 2/20/2016 An overview of the last horst Basin and Range / Mojave Desert Summary: Granitic, volcanic, marine sedimentary, non marine sedimentary,
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
TOPOGRAPHIC RELIEF MAP of NYS. LANDFORMS of NYS. Landforms. Creation of NYS Landforms 9/22/2011
TOPOGRAPHIC RELIEF MAP of NYS LANDFORMS of NYS Prof. Anthony Grande AFG 2011 Landforms The basis of present-day landforms (surface features) is the bedrock geology that has been worked on by the forces
PHYSICAL GEOGRAPHY: An overview. Definitions. Faulting. Folding GEOLOGIC PROCESSES 9/17/2013 TOPOGRAPHIC RELIEF
TOPOGRAPHIC RELIEF PHYSICAL GEOGRAPHY: An overview Prof. Anthony Grande AFG 0913 2 Definitions GEOLOGIC PROCESSES Geography: Study of people living on the surface of the earth. Geology: the study of the
LANDFORMS of NYS. Landforms. Exercise 4 9/13/2012. TOPOGRAPHIC RELIEF MAP of NYS. Physiographic map of NYS and vicinity showing Surface Features
TOPOGRAPHIC RELIEF MAP of NYS LANDFORMS of NYS Prof. Anthony Grande AFG 2012 Landforms REMINDER: The basis of present-day landforms (surface features) is the bedrock geology that has been worked on by
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
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
Geologic History. Earth is very, very old
Geologic History Earth is very, very old Earth s History The history of Earth and the ages of rocks can be investigated and understood by studying rocks and fossils. Evidence of ancient, often extinct
Geologic History of Texas: The Making of Texas Over 1.5 Billion Years
# 4 Geologic History of Texas: The Making of Texas Over 1.5 Billion Years Dr. Richard Kyle March 24, 2000 Produced by and for Hot Science - Cool Talks by the Environmental Science Institute. We request
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
Portion of the Grand Canyon
Landscapes Packet 9 Your Name Group Members Score Minutes Standard 4 Key Idea 2 Performance Indicator 2.1 Use the concepts of density and heat energy to explain observations of weather patterns, seasonal
C) use of nuclear power D) number of volcanic eruptions
3121-1 - Page 1 Name: 1) The graph below shows the change in carbon dioxide concentration in parts per million (ppm) in Earth's atmosphere from 1960 to 1990. The most likely cause of the overall change
NEW YORK S NATURAL WONDERS
Landscapes and Drainage Patterns NEW YORK S NATURAL WONDERS New York is not one of the largest states of the United States, nor does it have any large national parks to rival Yosemite or the Grand Canyon.
Module 10: Resources and Virginia Geology Topic 4 Content: Virginia Geology Notes
Virginia is composed of a very diverse landscape that extends from the beaches and barrier islands all of the way to the highly elevated Appalachian Plateau. Geologists have discovered ancient shallow
Unit 2. United States Physical Geography
Unit 2 United States Physical Geography Physical Geography U.S. extends from the Atlantic to Pacific U.S. is the 3rd largest country U.S. has fertile soils, vast forests, and variety of minerals All major
ENVI.2030L Geologic Time
Name ENVI.2030L Geologic Time I. Introduction There are two types of geologic time, relative and absolute. In the case of relative time geologic events are arranged in their order of occurrence. No attempt
LANDFORM REGIONS IN CANADA. Classroom Notes and Descriptions
LANDFORM REGIONS IN CANADA Classroom Notes and Descriptions Landform Regions in Canada There are eight distinct landforms in Canada: Western Cordillera Region Interior Plains Canadian Shield Hudson Bay
Structural Geology Lab. The Objectives are to gain experience
Geology 2 Structural Geology Lab The Objectives are to gain experience 1. Drawing cross sections from information given on geologic maps. 2. Recognizing folds and naming their parts on stereoscopic air
Name HW - Landscapes
Name HW - Landscapes 1. New York s Tug Hill landscape region is classified as a plateau because this region has a A) high elevation with distorted bedrock B) high elevation with nearly horizontal layers
Landforms in Canada. Canada is made up of three dis;nct types of landforms: Canadian Shield Highlands Lowlands
Canada s Landforms What is a Landform? A landform is any physical feature of the Earth s surface having a characteris;c, recognizable shape, produced by natural causes. Landforms include major features
Relative Age-dating -- Discovery of Important Stratigraphic Principles Y
R Steinberg DMC/4-08 EARTH HISTORY 1404 Example 1: Y S P Q Four different rock units (layers of different rock types), labeled Y, S, P, and Q, are seen in a road cut, as shown schematically above: 1) Are
LATITUDE. Latitude lines run to, but are measured & The 0 of latitude that circles the earth is called the?
LATITUDE Latitude lines run to, but are measured & The 0 of latitude that circles the earth is called the? LATITUDE 0 0 Latitude lines run east to west, but are measured north & south The 0 of latitude
MAPPING THE EARTH HOW DO YOU FIND A LOCATION ON THE EARTH?
MAPPING THE EARTH HOW DO YOU FIND A LOCATION ON THE EARTH? UNIT TOPICS TOPIC 1: LATITUDE & LONGITUDE TOPIC 2: FIELD MAPS TOPIC 3: TOPOGRAPHIC MAPS TOPIC 4: NYS LANDSCAPES TOPIC 1: LATITUDE & LONGITUDE
L.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP
L.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP 1. Unless a series of sedimentary rock layers has been overturned, the bottom rock layer
Evolution of Continents Chapter 20
Evolution of Continents Chapter 20 Does not contain complete lecture notes. Mountain belts Orogenesis the processes that collectively produce a mountain belt Includes folding, thrust faulting, metamorphism,
TIME. Does not give the. Places events in sequencee 1 st, 2 nd, 3 rd. Gives a. exact date of an event. event. Radioactive Dating.
Geologic History TIME Places events in sequencee 1 st, 2 nd, 3 rd Does not give the exact date of an event Gives a date or time of an event Uses the Law of Superposition Radioactive Dating Youngest Law
Structural Geology Lab. The Objectives are to gain experience
Geology 2 Structural Geology Lab The Objectives are to gain experience 1. Drawing cross sections from information given on geologic maps. 2. Recognizing folds and naming their parts on stereoscopic air
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
Earth History Exam. The remains of an early dinosaur could be found at reference point A. A B. B C. C D. D. page 1
Name: Date: 1. Base your answer(s) to the following question(s) on the Earth Science Reference Tables and your knowledge of Earth science. The accompanying cross section shows undisturbed sedimentary bedrock.
Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor
Earth s Continents and Seafloors GEOL100 Physical Geology Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types of crust Dense, thin,
Class Notes: Mapping the Earth
Name: Date: Period: Mapping the Earth The Physical Setting: Earth Science Class Notes: Mapping the Earth I. Latitude and Longitude Map -! Latitude -! Also called These lines intersect Equator -! The North
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
Introducing North America
Introducing North America I. Quick Stats Includes U.S. & Canada U.S consists of 50 States Federal Government Democracy 4 th in world w/ land area 3 rd in population Economic leader of free world II. Major
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
Guided Reading Activity
Guided Reading Activity Lesson 1 Physical Features Essential Question: How does geography influence the way people live? A Vast Land Directions: Read the lesson and use your text to decide whether each
Grade 7 History Mr. Norton
Grade 7 History Mr. Norton Section 1: Thinking Geographically Section 2: Land and Climates of the United States Section 3: The Tools of History Section 4: Economics and Other Social Sciences Grade 7 History
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
C) Trenton limestone
1. Base your answer to the following question on the Earth Science Reference Tables, the core section below, and your knowledge of Earth Science. The core section shows the subsurface bedrock geology for
Answers. Rocks. Year 8 Science Chapter 8
Answers Rocks Year 8 Science Chapter 8 p171 1 Rocks are made up of minerals such as quartz, feldspars, micas, and calcite. Different rocks are made up of different combinations of minerals. 2 Igneous,
Geology 200 North Cascades National Park
Geology 200 North Cascades National Park In our study of the geology of the national parks, as we move into the second unit we will progress from the predominately sedimentary rock sequences of the southwestern
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,
Fossils, Geologic Time, Absolute & Relative Dating, and Natural Resources. Chapters 5 & 6
Fossils, Geologic Time, Absolute & Relative Dating, and Natural Resources Chapters 5 & 6 How Do Fossils Form? Fossils are found in sedimentary rocks like sandstone, limestone, and shale In Virginia, most
UNIVERSITY OF SOUTH ALABAMA. GY 112: Earth History. Lecture 36: Plio-Pleistocene Geology. Instructor: Dr. Douglas W. Haywick
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 36: Plio-Pleistocene Geology Instructor: Dr. Douglas W. Haywick Last Time A) Cenozoic Overview and Tectonics Western North American tectonic provinces
The elevations on the interior plateau generally vary between 300 and 650 meters with
11 2. HYDROLOGICAL SETTING 2.1 Physical Features and Relief Labrador is bounded in the east by the Labrador Sea (Atlantic Ocean), in the west by the watershed divide, and in the south, for the most part,
Tectonic Framework of New York State
Tectonic Framework of New York State Kurt Hollocher Union College Geology Department Talk given for the UCALL program Union College, Schenectady, NY April 3, 2007 New York State Geological Highway Map.
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
Lab 7: Plate tectonics
Geology 115/History 150 Name(s): Lab 7: Plate tectonics Plate tectonics is the theory that is used to explain geological phenomena worldwide. For this reason, most of the useful maps that illustrate plate
A TRIP THROUGH VIRGINIA GEOLOGY FROM AN ENGINEER S PERSPECTIVE
A TRIP THROUGH VIRGINIA GEOLOGY FROM AN ENGINEER S PERSPECTIVE Bob Moss, PE Principal Engineer ECS Mid Atlantic, LLC The Engineer Parent WHY IS AN UNDERSTANDING OF LOCAL GEOLOGY IMPORTANT? It provides
Name Date Class. a. High elevation and high relief b. High elevation and level surface c. Flat land and low relief
Exploring Earth s Surface (pp. 21 27) This section describes factors that determine the shape of Earth s land surface. The section also describes how scientists divide Earth into four spheres. Use Target
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
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
Page 1. Name:
Name: Questions 1 through 3 refer to the following: The diagrams below represent two rock outcrops found several miles apart in New York State. Individual rock layers are lettered, and fossils and rock
Topics Laramide Orogeny: Late Cretaceous to Early Eocene Reading: GSA DNAG volume 3, Ch. 6
Topics Laramide Orogeny: Late Cretaceous to Early Eocene Reading: GSA DNAG volume 3, Ch. 6 Late Cretaceous to early Eocene New patterns developed 5 main regions Tectonic interpretations Post-Laramide events
Name: NYS Geology and Landscapes and some River stuff
Name: NYS Geology and Landscapes and some River stuff 1. Which types of surface bedrock are most likely found near Jamestown, New York? A) slate and marble B) quartzite and granite C) shale and sandstone
By Gil Brenner OLLI Geology Of New York State and NY City
By Gil Brenner OLLI 2013 Geology Of New York State and NY City Before We Start-- It s All in the PLATES! Geology of New York State including NYC CA. Active Margin A Passive Geologic Margin Gil Brenner
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
Chapter 3 Time and Geology
Chapter 3 Time and Geology Methods of Dating Rocks 1. Relative dating - Using fundamental principles of geology (Steno's Laws, Fossil Succession, etc.) to determine the relative ages of rocks (which rocks
Weather and Climate Summary and Forecast March 2018 Report
Weather and Climate Summary and Forecast March 2018 Report Gregory V. Jones Linfield College March 7, 2018 Summary: The ridge pattern that brought drier and warmer conditions from December through most
Unit 5: Earth s History Practice Problems
Name: Date: 1. Which bedrock would be most likely to contain fossils? A. Precambrian granite B. Cambrian shale C. Pleistocene basalt D. Middle-Proterozoic quartzite 6. Base your answer(s) to the following
Unconformities are depositional contacts that overlie rocks distinctly older than they are. They are often called gaps in the sedimentary record.
UNCONFORMITIES Unconformities are depositional contacts that overlie rocks distinctly older than they are. They are often called gaps in the sedimentary record. The contact represents time when no sediment
Variability Across Space
Variability and Vulnerability of Western US Snowpack Potential impacts of Climactic Change Mark Losleben, Kurt Chowanski Mountain Research Station, University of Colorado Introduction The Western United
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
Answers: Internal Processes and Structures (Isostasy)
Answers: Internal Processes and Structures (Isostasy) 1. Analyse the adjustment of the crust to changes in loads associated with volcanism, mountain building, erosion, and glaciation by using the concept
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
2. What type of rocks would you expect in this area, based on the topography? What is your reasoning?
Geology 101 Bonus Lab Name Topographic maps are useful in helping us interpret the history of the landscape of an area. The questions below are designed to help you learn to interpret topographic maps.
Weathering, Erosion, Deposition, and Landscape Development
Weathering, Erosion, Deposition, and Landscape Development I. Weathering - the breakdown of rocks into smaller particles, also called sediments, by natural processes. Weathering is further divided into
Chapter 1: America s Land Lesson 1: Land and Climate
Chapter 1: America s Land Lesson 1: Land and Climate Geography: Describe landforms and other physical features of the United States. Geography: Explain how and why climate varies throughout the United
Plan of Development Mountain Valley Pipeline Project. APPENDIX P Plan for Unanticipated Discovery of Paleontological Resources
APPENDIX P Plan for Unanticipated Discovery of Paleontological Resources Appendix P Plan for Unanticipated Discovery of Paleontological Resources Prepared by: TABLE OF CONTENTS 1.0 INTRODUCTION... 1 1.1
CHAPTER 1. Geo Challenges 1A to 1D. & World Map Activity
CHAPTER 1 Geo Challenges 1A to 1D & World Map Activity SELECT YOUR CHALLENGE World Map Activity Challenge 1A Challenge 1B Challenge 1C Challenge 1D Challenge 1A WS PG. 2 STEP #1 Label the largest continent
Name: Date: Period: Page 1
Name: Date: Period: Base your answers to questions 1 through 4 on the three bedrock outcrops below and on your knowledge of Earth science. The outcrops, labeled I, II, and III, are located within 15 kilometers
Groundwater Resources of Missouri. Cynthia Brookshire, R. G.
Groundwater Resources of Missouri Cynthia Brookshire, R. G. GROUNDWATER... Water beneath the Earth s surface within a zone of saturation AQUIFER... A geologic formation or group of formations that are
General Geologic Setting and Seismicity of the FHWA Project Site in the New Madrid Seismic Zone
General Geologic Setting and Seismicity of the FHWA Project Site in the New Madrid Seismic Zone David Hoffman University of Missouri Rolla Natural Hazards Mitigation Institute Civil, Architectural & Environmental
2011 Pearson Education, Inc. 1
1 An Introduction to Geology Earth, 10e - Chapter 1 Stan Hatfield Southwestern Illinois College 3 The Science of Geology Geology is the science that pursues an understanding of planet Earth. Physical geology
Weather and Climate Summary and Forecast Winter
Weather and Climate Summary and Forecast Winter 2016-17 Gregory V. Jones Southern Oregon University February 7, 2017 What a difference from last year at this time. Temperatures in January and February
In this lab, we will study and analyze geologic maps from a few regions, including the Grand Canyon, western Wyoming, and coastal California.
Name: Lab Section: work in groups, but each person turns in his/her own GEOSCIENCE 001 LAB UNDERSTANDING GEOLOGIC MAPS Geologic maps are colorful and even beautiful, but they also contain an amazing amount
Geology 101 Lab Worksheet: Geologic Time
Geology 101 Lab Worksheet: Geologic Time Name: Refer to the Geologic Time Lab for the information you need to complete this worksheet (http://commons.wvc.edu/rdawes/g101ocl/labs/geotimelab.html). All calculations
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
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 Time Grand Canyon National Park
Chapter 8: Geologic Time & the Grand Canyon Geologic Time Grand Canyon National Park Colorado Plateau nearly-horizontal rocks lifted feet above sea level River drains Mtns Who was John Wesley Powell? Label
Unit 1: Geography CLASS WEBSITE: QUIZLET GAMES: ONLINE RESOURCES
Unit 1: Geography ONLINE RESOURCES CLASS WEBSITE: HTTPS://MRYOUNGTMS.WEEBLY.COM/GEOGRAPHY.HTML QUIZLET GAMES: HTTPS://QUIZLET.COM/JOIN/MSFYY94T5 1 G e o g r a p h y Continents and Oceans The Seven Continents
Plate Tectonics. Chapter 17. Great Idea: The entire Earth is still changing, due to the slow convection of soft, hot rocks deep within the planet.
Plate Tectonics Chapter 17 Great Idea: The entire Earth is still changing, due to the slow convection of soft, hot rocks deep within the planet. 1 Chapter Outline The Dynamic Earth Plate Tectonics: A Unifying
Relative Age-dating -- Discovery of Important Stratigraphic Principles
Roger Steinberg Assistant Professor of Geology Del Mar College 101 Baldwin Corpus Christi, TX 78404 361-698-1665 rsteinb@delmaredu Abstract: When piecing together the geologic history of the Earth, geologists
Which landscape best represents the shape of the valleys occupied by glaciers? A) B) C) D)
1. Glaciers often form parallel scratches and grooves in bedrock because glaciers A) deposit sediment in unsorted piles B) deposit rounded sand in V-shaped valleys C) continually melt and refreeze D) drag
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
GEOL Introductory Geology: Exploring Planet Earth Fall 2010 Test #2 October 18, 2010
GEOL 101 - Introductory Geology: Exploring Planet Earth Fall 2010 Test #2 October 18, 2010 Name KEY ID# KEY Multiple choice questions (2 points each). 1. What type of metamorphic rock is formed over large
Thin, Widespread, Sedimentary Layers
Chapter 6 Thin, Widespread, Sedimentary Layers Many thin, widespread layers are evident in the sedimentary rocks. Thin of course is relative and depends upon the area the layer extends. A layer several
Physical Geography of the United States and Canada Chapter 5 A Land of Contrasts
Physical Geography of the United States and Canada Chapter 5 A Land of Contrasts Land Area Together the U.S. and Canada cover more than 7 million square miles. In total area, Canada ranks 2 nd and the
2011 Pearson Education, Inc. 1
1 Earth: An Introduction to Physical Geology, 10e Tarbuck & Lutgens An Introduction to Geology Earth, 10e - Chapter 1 Stan Hatfield Southwestern Illinois College 4 The Science of Geology Geology is the
Earth Science Regents Watersheds & Drainage Basins Lab
Name Earth Science Regents Watersheds & Drainage Basins Lab Copyright 2003 by Steve Kluge Lab # Period Part 1: New York State Drainage Exercise NOTE: You ll need pages 2 and 3 of your ESRT to complete
Review Questions- GEOL 10113
Review Questions- GEOL 10113 Dr. Morgan 1. Pangaea broke up at the end of which era? 2. Marble and quartzite are in which rock category? 3. Which rocks indicate high grade (temp) or low grade (temp) metamorphism?
Earth s Layers. Earth s Surface
CHAPTER 1 LESSON 3 Earth s Layers Earth s Surface Key Concepts What are Earth s major landforms and how do they compare? What are the major landform regions of the United States? What do you think? Read
Geology Test Review Answers
Name: Geology Test Review Answers Core: Fill in the blanks: 1. Sediments get compacted and cemented into sedimentary rock. 2. Igneous rocks can be intrusive or extrusive from a volcano. 3. Adding heat
Chapter 1: The Geography of the Western Hemisphere
Chapter 1: The Geography of the Western Hemisphere Chapter 1, Lesson 1: The Changing Earth Objectives: - You will be able to identify the major natural events that cause the earth to change. - You will
CANADA S LANDFORM REGIONS
CANADA S LANDFORM REGIONS Canada s Regions Canada is divided into Eight major regions. A Region is an area that is defined on the basis of the presence or absence of certain characteristics: Age of rock