The Rocks of Harriman State Park
|
|
- Camron Walters
- 5 years ago
- Views:
Transcription
1 The Rocks of Harriman State Park Talk with the Experts American Canoe Association Bill Menke Lamont-Doherty Earth Observatory Columbia University July 23, 2016
2 Part 1 Everything Changes
3 Very Old
4 Great Pyramid at Giza roughly 5000 years old
5 1 pyramid 5000 years
6 Imagine what Harriman State Park was like 4 Pyramids Ago? (20,000 years)
7 Whitetail Deer
8 Whitetail Deer
9 Greenland Ice Sheet
10 Absolutely nothing lived in the Harriman Park 20,000 years ago
11
12 Harriman State Park
13 Twenty Thousand Years not all that long ago
14 200 pyramids = One Million Years
15 One Million Years
16 Death of the Dinosaurs 65 Million Years ago 65 boxes of 200 pyramids
17 Part 2 Rocks tell a Story
18 but an incomplete story
19 Erosion destroys rocks but also brings them to the Earth s surface
20 Erosion destroys rocks Bad for Geologists but also brings them to the Earth s surface Good for Geologists
21 2 inches in 20,000 years 40,000 inches in 400 Million Years
22 2 inches in 20,000 years 100,000 inches in 1000 Million Years About a mile and a half!
23 How can you erode a half mile off the land without it being underwater?
24
25
26
27
28
29 Part 3 The Age of Bacteria (and not much else) 1000 million years ago
30 Era when most of Harriman Park rocks were formed Two major rock types
31
32 Gneiss
33
34 Granite
35 Gneiss A Metamorphic Rock Banded Brown or Grey in Color Layers of sand and clay Deeply buried and cooked (metamorphosed) by heat and pressure Granite An Igneous Rock No bands White or beige in Color Solidified molten rock Very hard to erode so tends to form hilltops (Bear Mountain, Popolopen Torne, etc)
36 Originally layers of sand and clay. Formed at surface of earth Gneiss Might there have been living things?
37 Graphite (pure carbon) all that s left of life
38 Gneiss
39 Gneiss Folds
40 solid rock. acting like dough
41 Needs to be deeply buried say 5 miles to get hot enough to be metamorphosed and folded Gneiss when was it buried?
42 Granite An Igneous Rock Very hot conditions think volcano Which is older? Gneiss, or Granite?
43 Claudius Smith Den
44
45
46
47 Granite Geological Logic The granite cuts the gneiss so the gneiss is the older Gneiss furthermore the fold were already formed when the granite was emplaced so the gneiss was already deep underground before the granite was formed
48 Geologists have been able to determine the age of the granite about 1000 million years so the sediments that formed the gneiss are older than that
49 Part 4 The Age of Dinosaurs (and many other animals) 200 Million years ago
50 Aerial view of Harriman State Park
51 Lake Tiorati Lake Welch Stony Point Tuxedo Park ACA Pomona Sloatsburg
52 do you see the lines? of hills and valleys?
53
54 Lines are Geological Faults
55 Right-most is the Ramapo Fault
56 With some effort you can work out the direction the land moved
57
58
59
60 Slickenslides grooves from fault motion
61 When was the faulting?
62
63 Boulders in sandstone
64 rock debris coming out of a steep stream valley into a low lying area
65 look what else you find in the sandstones
66 so the faulting looks to have occurred during the age of the dinosaurs 200 million years ago
67 so the faulting looks to have occurred during the age of the dinosaurs 200 million years ago
68 Part 5 The Ice Age which ended 20,000 years ago
69 Glacier in Iceland
70 Glacial scratches
71
72
73
74
75
76 Boulder carried by glacier Erratic Boulders
77 Harriman State Park
78 Do you recognize this rock?
79 Bearford Mountain
80
81 Fort Lee Historic Little Park Tor
82 Looks like granite from Harriman park Fort Lee Historic Little Park Tor
83 Harriman Park as Fort seen Lee from Historic Little Park Tor
84
85 Steep downstream slope Glacially Plucked Cliff
86 Steep downstream slope Glacier in Iceland
87 Claudius Smith Den
88 Pine Meadow Lake
89 The Kitchen Stairs
90 So when you walk around the Park Listen to the Story told by the Rocks!
91 and great talking with you!
92 Addendum There s gold in them there hills!
93 Addendum There s gold in them there hills! iron
94 Southfield Iron Furnace
95 Carbon Dioxide Iron Ore Limestone Charcoal fill up the furnace Set it afire! Molten Slag Molten Iron
96 Hudson River Chain, Revoutionary War
97 Magnetite (Iron Ore)
98 The magnetite occurs in small veins usually near the granites geologists are not sure why it formed
99 Slag (waste product of refining process)
100 Tailings Pile of Black Ash Mine
101 Black Ash Mine
Earth s Resources. Earth s Surface
Earth s Resources Earth s Surface Earth s surface is made up of a layer of rock called the crust. The crust covers all of Earth. It is several miles thick. Most of the crust is under water. The upper part
More informationTEACHER BACKGROUND KNOWLEDGE. Surface Processes: Weathering and Erosion
TEACHER BACKGROUND KNOWLEDGE Surface Processes: Weathering and Erosion Core Concepts Precipitation (caused by the water cycle) and wind cause rocks to be broken into smaller pieces in the process called
More informationWriting Earth s History
Earths History Writing Earth s History How is Earths History like writing in your Journal? Everyday, something happens and, with a pen, it is written down in the pages of your journal. As you continue,
More informationName: Mid-Year Review #2 SAR
Name: Mid-Year Review #2 SAR Base your answers to questions 1 through 3 on on the diagram below, which shows laboratory materials used for an investigation of the effects of sediment size on permeability,
More informationLAB - Rock Classification
NAME: LAB - Rock Classification Date: Introduction: A rock is any naturally occurring aggregate of minerals, mineral-like solids, glass, or organic particles. The properties that can be observed in a rock
More information1. In the block diagram shown here, which is the oldest rock unit?
Pre/Post GCI Name (print) 1. In the block diagram shown here, which is the oldest rock unit? 2. Referring to the same diagram as the previous question, which of the labeled rock units is the youngest?
More informationRocks: Stony Stalwarts: Adapted from:
Rocks: Stony Stalwarts: Adapted from: http://science.nationalgeographic.com/science/earth/inside-the-earth/rocks-article/ Rocks are so common that most of us take them for granted cursing when we hit them
More informationQuestion #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
More informationSCI-5 KES 5.7 Geology Post-test Exam not valid for Paper Pencil Test Sessions
SCI-5 KES 5.7 Geology Post-test Exam not valid for Paper Pencil Test Sessions [Exam ID:1D5NLH 1 Earth's crust is made of plates that move slowly. This movement changes the appearance of the Earth's crust
More informationIntroduction to Landform Study Chapter 13
Introduction to Landform Study Chapter 13 Geomorphology The study of the characteristics, origin, and development of landforms 58 million square miles of land 7 continents Wide latitudinal range and environmental
More informationEarth s Dynamic Surface
Earth s Dynamic Surface Key Concepts What is the difference between physical and chemical weathering? How do water, ice, and wind change Earth s surface? Changing Earth s Surface What do you think? Read
More informationPractice Test Rocks and Minerals. Name. Page 1
Name Practice Test Rocks and Minerals 1. Which rock would be the best source of the mineral garnet? A) basalt B) limestone C) schist D) slate 2. Which mineral is mined for its iron content? A) hematite
More informationChanges to Land 5.7B. landforms: features on the surface of Earth such as mountains, hills, dunes, oceans and rivers
All the landforms on Earth have changed over time and continue to change. Many of the changes were caused by wind, moving water, and moving ice. Mountains have grown and shrunk. Rivers have cut away land
More informationThink about the landforms where you live. How do you think they have changed over time? How do you think they will change in the future?
reflect All the landforms on Earth have changed over time and continue to change. Many of the changes were caused by wind, moving water, and moving ice. Mountains have grown and shrunk. Rivers have cut
More informationFigure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant?
1. In which type of climate does chemical weathering usually occur most rapidly? 1. hot and dry 3. cold and dry 2. hot and wet 4. cold and wet 2. Figure 1 The map shows the top view of a meandering stream
More informationName. 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different soil horizons, A, B, C, and D, are shown.
Name 1. In the cross section of the hill shown below, which rock units are probably most resistant to weathering? 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different
More informationGeohistory Review. Things you need to know:
Geohistory Review Things you need to know: a) The earth and the solar system are 4.5 billion years old (4.5 X 10 9 ) b) Law of original horizontality: Sedimentary rock layers are always deposited as horizontal
More informationabrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG)
FOSS Soils, Rocks, and Landforms Module Glossary 3 rd Edition 2012 abrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG) acid a substance that geologists use to
More informationSection 5. Rock Units and Your Community. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 3 Minerals, Rocks, and Structures Section 5 Rock Units and Your Community What Do You See? Learning Outcomes In this section, you will Recognize that rocks are arranged in Earth s crust as well-defined
More informationModeling the Rock Cycle
P a g e 1 Name Modeling the Rock Cycle Background Information: Like the Earth itself, rocks are in a constant state of change. Rocks are solids made up of different minerals. Scientists usually classify
More informationRocks & Minerals. Lesson 1 Properties of Minerals. What is a mineral? What is a mineral?
Rocks & Minerals What is a mineral? A mineral must have 5 specific characteristics to be considered a mineral a. b. c. d. e. Naturally occurring - formed by natural processes. Solid - must have a definite
More informationLandscape. Review Note Cards
Landscape Review Note Cards Last Ice Age Pleistocene Epoch that occurred about 22,000 Years ago Glacier A large, long lasting mass of ice which forms on land and moves downhill because of gravity. Continental
More informationENVI.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
More informationRock Cycle Reader s Theater
Rock Cycle Reader s Theater Characters Teacher1 Teacher 2 Student 1 Student 2 Student 3 Sedimentary Rock Crust Wind Water Ice Sediment 1 Sediment 2 Sediment 3 Metamorphic Rock The Rock Cycle Mantel Magma
More informationRock Cycle. Presented by Kesler Science
Presented by Kesler Science Essential Questions: What processes are involved in the formation and classification of metamorphic, sedimentary, and igneous rocks? Sediments A model that describes the formation,
More informationC) 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
More informationEarth History: Record in the Rocks
Earth History: Record in the Rocks The geologic history of Earth can be read from rocks if you know what to look for. In this presentation, you will see examples of many types of clues, stored in rocks.
More informationTectonic 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.
More information1. The diagram below shows the stump of a tree whose root grew into a small crack in bedrock and split the rock apart.
1. The diagram below shows the stump of a tree whose root grew into a small crack in bedrock and split the rock apart. 4. Which process involves either a physical or chemical breakdown of earth materials?
More informationUnit E: Planet Earth Topic 1: Scientific Study Helps Us Understand the Earth
Unit E: Planet Earth Topic 1: Scientific Study Helps Us Understand the Earth 1 1.1 A Model for Earth A. Our Ancient Past 1. Geologists estimate that the Earth is about billion years old 2. Humans appeared
More informationGEOMORPHOLOGY WHAT AM I EXECTED TO LEARN?
GEOMORPHOLOGY WHAT AM I EXECTED TO LEARN? Define rock. List and recognize clear examples of the three primary rocks types. Explain the difference between the three different ways sedimentary rocks are
More informationRead Across America. Listen as I read for facts about Volcanoes. In the Shadow of the Volcano
Read Across America Listen as I read for facts about Volcanoes. In the Shadow of the Volcano Constructive & Destructive Processes Earth s surface is always changing. Blowing wind and flowing water causes
More information3 Erosion and Deposition by Ice
CHAPTER 12 3 Erosion and Deposition by Ice SECTION Agents of Erosion and Deposition BEFORE YOU READ After you read this section, you should be able to answer these questions: What are glaciers? How do
More informationPotential short answer questions: What is Pangea? Describe at least 4 pieces of evidence that led Wegener to suggest the theory of Continental Drift.
6th Grade Earth Science Fall Semester Mid-Term Study Guide The mid-term may include: 4 short answer questions,1-2 sketches to draw and/or label, 4 partially filled charts which you should complete, 30
More informationIntroduction to Prospecting. Session Two Geology
Introduction to Prospecting Session Two Geology The Earth Earth is 4.6 billion years old (Ba). Bacteria & algae +3.5 Ba. Microscopic animals ~2 Ba. Animals ~600 million years (Ma) old. Mankind about 100,000
More informationThe Norwood Science Center. Geology (Minerals) Grade 4
The Norwood Science Center Geology (Minerals) Grade 4 Background Information: Where do rocks come from? At first you might think the answer to this question is simple. Igneous rock comes from either magma
More informationEARTH S CHANGING SURFACE
EARTH S CHANGING SURFACE Weathering Together, weathering and erosion work continuously to wear down the material on Earth s surface. weathering process that breaks down rock and other substances of Earth
More informationGuided Notes Surface Processes. Erosion & Deposition By: Glaciers
Guided Notes Surface Processes Erosion & Deposition By: Glaciers K. Coder 2015 26) How does moving ice erode and deposit sediments? Glaciers (Movement of Ice): a naturally formed mass of ice and snow that
More informationFIREPLACE GEOLOGY. Dining Hall
FIREPLACE GEOLOGY Dining Hall The Dining Hall fireplace represents a slice through a Cascade Mountain volcano. Volcanoes are formed from molten magma rising up from within the Earth s crust. Magma that
More informationabrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG)
FOSS Soils, Rocks, and Landforms Module Glossary NGSS Edition 2019 abrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG) acid a substance that geologists use to
More informationtest date Name date Review: Geologic Time & Geologic Procesess-: You will record 1-38 answers on the scan sheet! These are worth 1.
Review: Geologic Time & Geologic Procesess-: You will record 1-38 answers on the scan sheet! These are worth 1.5 points each Use your EARTH HISTORY CHART Part I. Matching All of the statements match to
More informationA Geological Tour of Tumbledown Mountain, Maine
Maine Geologic Facts and Localities April, 1998 A Geological Tour of Tumbledown Mountain, Maine 44 45 3.21 N, 70 32 50.24 W Text by Robert G. Marvinney, Department of Agriculture, Conservation & Forestry
More information4 th Grade PSI. Slide 1 / 107 Slide 2 / 107. Slide 3 / 107. Slide 4 / 107. Slide 5 / 107. Slide 6 / 107. The History of Planet Earth
Slide 1 / 107 Slide 2 / 107 4 th Grade PSI The History of Planet Earth 2015-11-10 www.njctl.org Slide 3 / 107 Slide 4 / 107 The History of Planet Earth The Structure of Earth Rock Layers Fossils and Relative
More informationGeologic History Unit Notes. Relative age - general age statement like older, younger more recent
Geologic History Unit Notes Relative age - general age statement like older, younger more recent Absolute age - specific age like 4,600 million years old Fundamental Principles of Relative Dating 1. Uniformitarianism
More informationOccurs in Nature SOLID Inorganic (not from a plant or animal) Crystalline (forms crystals) Atoms / Molecules bond in a regular pattern
#12: Mineral Occurs in Nature SOLID Inorganic (not from a plant or animal) Crystalline (forms crystals) Atoms / Molecules bond in a regular pattern Regular Composition EX- Halite (salt) is always NaCl
More informationGEOLOGICAL AGE OF ROCKS. Absolute geological age
GEOLOGICAL AGE OF ROCKS Absolute geological age The pioneer of nuclear physics discovered at the turn of centuries that atoms of certain elements, the radioactive ones, spontaneously disintegrate to form
More informationPage 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
More informationL.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
More informationChapter 2. Early Geologists Tackle History's Mysteries
Chapter 2 Early Geologists Tackle History's Mysteries Nicolaus Steno and his Laws Danish (lived in Italy); 1638-1687 Pioneering studies of Italian strata Developed basic principles (laws) regarding age
More informationA Geology Trail Around
A Geology Trail Around There is an interesting story to be told as you walk around the building. There are many rocks for you to see. They are of different geological ages. The Geological Time Scale text
More informationChanges over Time: Destructive Processes
1 Name Date Changes over Time: Destructive Processes Earth s surface is always changing. Blowing wind and flowing water causes some changes. Moving rock deep inside Earth causes other changes. These processes
More information4th Grade. Earth Systems.
1 4th Grade Earth Systems 2015 11 10 www.njctl.org 2 Earth Systems Click on the topic to go to that section Earth's Systems Mechanical Weathering Chemical Weathering Erosion Biogeology 3 Earth's Systems
More informationLesson 4 Rocks Rock! Lesson Overview: Students will become familiar with rocks, minerals, and be introduced to the rock cycle.
Lesson 4 Rocks Rock! Lesson Overview: Students will become familiar with rocks, minerals, and be introduced to the rock cycle. Objectives: Students will be able to: 1. Explain the difference between rocks
More informationPage 1. Name:
Name: 1) Which property would best distinguish sediment deposited by a river from sediment deposited by a glacier? thickness of sediment layers age of fossils found in the sediment mineral composition
More informationEarth has more than 600 active volcanoes. An active volcano is one that has erupted within recorded history.
Volcanoes A volcano is an opening in Earth s surface that erupts gases, ash, and lava. These materials pile up in layers around the opening, forming volcanic mountains. Earth has more than 600 active volcanoes.
More informationTAKE HOME EXAM 8R - Geology
Name Period Date TAKE HOME EXAM 8R - Geology PART 1 - Multiple Choice 1. A volcanic cone made up of alternating layers of lava and rock particles is a cone. a. cinder b. lava c. shield d. composite 2.
More information4th Grade. Slide 1 / 101. Slide 2 / 101. Slide 3 / 101. Earth Systems. Earth Systems Earth's Systems. Mechanical Weathering
Slide 1 / 101 Slide 2 / 101 4th Grade Earth Systems 2015-11-10 www.njctl.org Earth Systems Slide 3 / 101 Click on the topic to go to that section Earth's Systems Mechanical Weathering Chemical Weathering
More informationName Test Date Hour. forms that lived only during certain periods. abundant and widespread geographically. changes to the surface of Earth.
Name Test Date Hour Earth Processes#3 - Notebook Earth s History LEARNING TARGETS I can explain the lack of evidence about the Precambrian Time. I can describe possible causes for the mass extinction in
More information2 Aggregates in Indiana
2 Aggregates in Indiana Origin of Aggregates Gravel and Natural Sands Crushed Stone Slag Distribution of Aggregates Glacial Deposits Bedrock Deposits Aggregate Types Natural Aggregates Artificial Aggregates
More informationCross-Cutting Relationships Cross-Cutting and Sequencing Lab Earth Science Essentials-Advanced by Russ Colson
Cross-Cutting Relationships Cross-Cutting and Sequencing Lab Earth Science Essentials-Advanced by Russ Colson Introduction: It isn't possible to bring all of outdoors into the classroom, and stratigraphic
More informationPacific Northwest Rock Lab, Part II. Igneous Rocks. Name Per.
Name Per. Pacific Northwest Rock Lab, Part II After you ve classified all your rocks, place their numbers next to the names and read the information about the rock. Check the classifications here (igneous,
More informationSection 1: Earth s Interior and Plate Tectonics Section 2: Earthquakes and Volcanoes Section 3: Minerals and Rocks Section 4: Weathering and Erosion
Section 1: Earth s Interior and Plate Tectonics Section 2: Earthquakes and Volcanoes Section 3: Minerals and Rocks Section 4: Weathering and Erosion Key Terms Crust Mantle Core Lithosphere Plate Tectonics
More informationTEACHER BACKGROUND KNOWEDGE. Minerals, Rocks and the Rock Cycle
TEACHER BACKGROUND KNOWEDGE Minerals, Rocks and the Rock Cycle Core Concepts Rocks in the Earth s crust vary in their form and structure based on process that made them. The constant changing of the form
More informationPortion 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
More information4. The map below shows a meandering stream. Points A, B, C, and D represent locations along the stream bottom.
1. Sediment is deposited as a river enters a lake because the A) velocity of the river decreases B) force of gravity decreases C) volume of water increases D) slope of the river increases 2. Which diagram
More informationGeneral Geology Lab #7: Geologic Time & Relative Dating
General Geology 89.101 Name: General Geology Lab #7: Geologic Time & Relative Dating Purpose: To use relative dating techniques to interpret geological cross sections. Procedure: Today we will be interpreting
More informationRocks and The Rock Cycle
Rocks and The Rock Cycle 3 Main Rock Types Igneous Sedimentary Metamorphic 3 Main Rock Types Igneous Sedimentary Metamorphic Igneous EXTRUSIVE Forms when lava cools quickly on the Earths surface Forms
More informationChapter 4: Rocks and Their Transformations
Thai Christian School Grade 6 English Program SCIENCE Home Study Name : Number :... Subject : Science Grade : 6/ Teacher : Miss Maggie Quinn Date : November 2011 Parent Signature:... Instructions: Read
More informationBradbury Mountain, Pownal, Maine
Maine Geologic Facts and Localities August, 2008 Bradbury Mountain, Pownal, Maine 43 o 53 56.56 N, 70 o 10 45.11 W Text by Henry N. Berry IV, Department of Agriculture, Conservation & Forestry 1 Introduction
More informationUnit 3 Review - Surface Processes
Unit 3 Review - Surface Processes 1. Why is the surface of Mercury covered with meteor impact craters, while Earth s surface has relatively few craters? A) Mercury is larger than Earth, so it gets hit
More informationIgneous. Sedimentary Transformation by heat and pressure
Melting, cooling and hardening Turns you into an Igneous Rock! Limestone A Sedimentary Rock Erosion, deposition and cementation Turns you into a Sedimentary Rock! Transformation by heat and pressure Turns
More informationShe hammered it into pieces and then ground them into a powder using a pestle and mortar.
1. Linda had a piece of red sandstone. She hammered it into pieces and then ground them into a powder using a pestle and mortar. She put the powder into a measuring cylinder with water and shook the mixture.
More informationAngel International School - Manipay 1 st Term Examination November, 2015
Grade 08 Angel International School - Manipay 1 st Term Examination November, 2015 Chemistry Duration: 2 Hours Index No:- Underline the correct answer. 1. Which of the following is a fossil fuel? a) Natural
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 7 Glaciers, Desert, and Wind 7.1 Glaciers Types of Glaciers A glacier is a thick ice mass that forms above the snowline over hundreds or thousands of
More informationWeathering, Erosion and Deposition
Weathering, Erosion and Deposition Shaping the Earth s Surface Weathering the process of breaking down rocks into smaller fragments Erosion the transport of rock fragments from one location to another
More informationRocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock
Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock can start out as one type and change into another.
More informationB) color B) Sediment must be compacted and cemented before it can change to sedimentary rock. D) igneous, metamorphic, and sedimentary rocks
1. Which characteristic of nonsedimentary rocks would provide the least evidence about the environment in which the rocks were formed? A) structure B) color C) crystal size D) mineral composition 2. Which
More informationEarth 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.
More informationSurface Events & Landforms. Mrs. Green
Surface Events & Landforms Mrs. Green Bell Work 1) Which event MOST likely causes the slowest change to the surface of Earth? a) Earthquake b) Landslide c) Volcano d) Wind 2) When cold weather freezes
More informationDay 3 Weathering and Erosion.notebook. October 02, Section 7.2. Erosion and Deposition. Objectives
Objectives Describe the relationship of gravity to all agents of erosion. Contrast the features left from different types of erosion. Analyze the impact of living and nonliving things on the processes
More informationChapter 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
More informationObjectives: Define Relative Age, Absolute Age
S6E5. Students will investigate the scientific view of how the earth s surface is formed. c. Classify rocks by their process of formation. g. Describe how fossils show evidence of the changing surface
More informationRelative Dating. The Rock Cycle. Key Concept Scientists can interpret the sequence of events in Earth s history by studying rock layers.
2 What You Will Learn The rock cycle includes the formation and recycling of rock. Relative dating establishes the order in which rocks formed or events took place. The principle of superposition states
More information4 th Grade Science Vocabulary ~ Student List
Magnetism Attract Force Magnetism Repel Compass Pole Magnetic field Battery Circuit Closed Circuit Open circuit Electricity Conductor Insulator Static Electricity Series Circuit Parallel circuit Electromagnet
More informationReview - Unit 2 - Rocks and Minerals
Review - Unit 2 - Rocks and Minerals Base your answers to questions 1 and 2 on the diagram below, which shows the results of three different physical tests, A, B, and C, that were performed on a mineral.
More informationWonder as you Wander up the Carding Mill Valley
Wonder as you Wander up the Carding Mill Valley Spot clues to the 600 million year old history of the Long Mynd. Consider how the Earth has evolved since the rock you are walking over first formed. Welcome
More informationThe 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
More informationDemonstrate knowledge of Earth Science. US (v5), 2 credits
GEOLOGY UNIT STANDARD Demonstrate knowledge of Earth Science US 18982 (v5), 2 credits UNIT STANDARD Title: Demonstrate knowledge of Earth science Level: 1 Credits: 2 Purpose: People credited with this
More informationTHE CHANGING SURFACE OF THE EARTH
THE CHANGING SURFACE OF THE EARTH Key words Drain geological agent weathering erosion Sediment deposition transport The landscape is a consequence of the action of two types of geological processes; internal
More informationAngel International School - Manipay
c Grade 8 Angel International School - Manipay 1 st Term Examination November, 2016 Chemistry PART I Multiple Choice Questions. Duration: 02 Hours Index No:- (1) A common sedimentary rock which is formed
More informationAll About Rocks. What Exactly Are Rocks? 298 words. Born from Magma: Igneous Rock 223 words. Layer After Layer: Sedimentary Rock 192 words
ARTICLE-A-DAY All About Rocks 6 Articles Check articles you have read: What Exactly Are Rocks? 298 words Born from Magma: Igneous Rock 223 words Layer After Layer: Sedimentary Rock 192 words Changing Form:
More informationSTATION #1 Compaction and Cementation
STATION #1 Compaction and Cementation STATION #2 High Temperature and Pressure STATION #3 Sediments Examples: Glacial deposits: gravel, sand, clay River and lake deposits: gravel, sand, mud Sand dunes
More informationPHYSICAL 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
More informationChapter 8 Earth Systems and Resources
Chapter 8 Earth Systems and Resources Earth s resources were determined when the planet formed. The Earth s Crust Layers Core: innermost zone of the planet, largely nickel and iron. Mantle: above the core,
More informationChapter 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
More informationStudying Rocks and Soil
Studying Rocks and Soil How do rocks form? Rocks Rock is found in nature. Rock is solid. It is nonliving matter. All rocks are made of one or more minerals. A mineral is a natural material that forms from
More informationMichigan s Geology and Groundwater
Michigan s Geology and Groundwater Ralph J. Haefner Deputy Director U.S. Geological Survey Michigan-Ohio Water Science Center Lansing, Michigan Outline About the USGS Geology 101 Michigan s geology Bedrock
More informationBell Ringer. Are soil and dirt the same material? In your explanation be sure to talk about plants.
Bell Ringer Are soil and dirt the same material? In your explanation be sure to talk about plants. 5.3 Mass Movements Triggers of Mass Movements The transfer of rock and soil downslope due to gravity is
More informationtransform boundary Photograph by Robert E. Wallace, USGS.
transform boundary The San Andreas Fault is undoubtedly the most famous transform boundary in the world. To the west of the fault is the Pacific plate, which is moving northwest. To the east is the North
More informationPratice Surface Processes Test
1. The cross section below shows the movement of wind-driven sand particles that strike a partly exposed basalt cobble located at the surface of a windy desert. Which cross section best represents the
More information