The Importance of Habitat Mapping

Size: px
Start display at page:

Download "The Importance of Habitat Mapping"

Transcription

1 The Importance of Habitat Mapping H. Gary Greene With Assistance from: Charlie Endris and Bryan Dieter For: MESH Conference Dublin Castle, Dublin, Ireland - 14 March 2007

2 Objectives To illustrate why habitat mapping is important To show how deep-water habitat mapping has been used along the western margin of the U.S. to facilitate management of marine resources To present different types of case histories that show how habitat mapping can be used in resources management To show how GIS can be useful in habitat evaluation To illustrate how habitats can be efficiently archived and retrieved in a GIS

3

4 Before Multibeam

5 After!

6

7

8 Hurbert Vos, 1898 Study of Hawaiian Fish

9 A Geologist

10

11 A Biologist

12

13 SCALE SCALE SCALE Scale In Time & Space

14

15

16

17

18 MBARI Santa Barbara multibeam data Slope-shaded bathymetry

19 Santa Barbara Habitat Map Anoxic basin Ss_u Smh_h Shm_l/p Shs_i She_c Fs_u Fsc_u/c Fsc/f_u Fsg/o_h/u Fsc/t_u Fsg_u Fsg/m_s/u Fsl_h/u Fsl/s_i/u Fsm_s/u Fst_u Fsy_u Fmt_u/c Fhc_c Fhe_c Fhm_c/l Fhs/t_i Rs_u Rsg_u Rsl_h/u Rsm_l/s Rhm_l/p Bs_u Unconsolidated Sediment (Shelf) Tar Flow Carbonate Mound (Shelf) Fault Scarp Bedrock Exposure (Shelf) Unconsolidated Sediment (Flank) Soft Canyon Wall (Flank) Canyon Floor (Flank) Braded Channel (Flank) Terrace Deposit in Canyon (Flank) Gully (Flank) Potholes (Flank) Landslide (Flank) Landslide Scarp (Flank) Scour Depression (Flank) Terrace Deposit (Flank) Fan (Flank) Terrace Slope (Flank) Hard Canyon Wall (Flank) Bedrock Exposure (Flank) Carbonate Mound (Flank) Terrace Scarp (Flank) Unconsolidated Sediment (Ridge) Gully (Ridge) Landslide (Ridge) Pockmark (Ridge) Carbonate Mound (Ridge) Unconsolidated Sediment (Basin)

20

21 Interpretations of benthic habitats from USGS data

22

23 After Mosher and Johnson, 2000

24 Before Multibeam

25 Large submarine dune field in western Boundary Pass A A`

26 After Mosher and Johnson, 2000

27 Strait of Juan de Fuca sand waves After Mosher and Johnson, 2000

28 Sandwave Field Shaw Island FHL San Juan Island N Lopez Island

29

30 1) Sampling

31 Density (531,893 m 2 sandwave area, 0.12 m 2 grab area) Dark: 48 fish/m 2 (var. of mean=27) Light: 120 fish/m 2 (var. of mean=50) Dark vs. Light t-test: p= Average: 84 fish/m 2 Range: fish/m 2

32 Abundance in Sandwave Field If avg. density = 84 fish/m 2 : 44,556,805 fish If light density = 120 fish/m 2 : 63,742,733 fish

33 Dynamic bedforms values in meters 2003 Boundary Pass region, Canada

34

35 Geologic Setting Numerous episodes of uplift & subsidence associated with tectonics and glacial cycles (Burmester, Blake, & Engebretson, 2000))

36 Seafloor Complexity RUGOSITY = Surface area / Planar area Quantitative, Standardized method (reproducible)

37

38 Turn Island Seafloor Complexity Low ( ) Intermediate ( ) Mod. High to High ( ) Extremely High ( ) Turn Is.

39 Methodology Pile Point Pile Point Habitat Extensions Fractured bedrock Fractured bedrock wall Channel sediments Low Intermediate Mod. High to High Extremely High

40 Abbreviations: - PSF = Peril Strait Fault - MEVF = Mt. Edgecombe Volcanic Field - CSF = Chattam Strait Fault Submarine Volcanic Center - QC-FW = Queen Charlotte- Fairweather Fault

41

42

43

44

45

46

47 Abbreviations: - PSF = Peril Strait Fault - MEVF = Mt. Edgecombe Volcanic Field - CSF = Chattam Strait Fault Submarine Volcanic Center - QC-FW = Queen Charlotte- Fairweather Fault

48

49

50

51

52 Abbreviations: - PSF = Peril Strait Fault - MEVF = Mt. Edgecombe Volcanic Field - CSF = Chattam Strait Fault Submarine Volcanic Center - QC-FW = Queen Charlotte- Fairweather Fault

53 Volcanic Cone

54 Fairweather Habitat Map 1:45,0000

55

56

57

58

59 Bimodal substrate Mud Scoured depression Scarp Sand waves w/ ripples Sand waves Sed. covered bedrock Exposed bedrock Pinnacle

60 Bimodal substrate Mud Scoured depression Scarp Sand waves w/ ripples Sand waves Sed. covered bedrock Exposed bedrock Pinnacle

61 Bimodal substrate Mud Scoured depression Scarp Sand waves w/ ripples Sand waves Sed. covered bedrock Exposed bedrock Pinnacle

62 Bimodal substrate Mud Scoured depression Scarp Sand waves w/ ripples Sand waves Sed. covered bedrock Exposed bedrock Pinnacle

63

64

65

66

67

68

69

70 Conclusions Marine benthic habitat maps are important sources of information critical to the evaluation of marine resources Interpreted potential habitat maps provides a base upon which biological and other data can be added Resolution and accuracy of data collection and scale of interpretation should be considered at all times GIS facilitates efficient achieving and retrieval of habitat characteristics if habitat types are attributed properly

71 From Managing Disasters to Managing Risk

Ocean Basins, Bathymetry and Sea Levels

Ocean Basins, Bathymetry and Sea Levels Ocean Basins, Bathymetry and Sea Levels Chapter 4 Please read chapter 5: sediments for next class and start chapter 6 on seawater for Thursday Basic concepts in Chapter 4 Bathymetry the measurement of

More information

1. Name at least one place that the mid-atlantic Ridge is exposed above sea level.

1. Name at least one place that the mid-atlantic Ridge is exposed above sea level. Interpreting Tectonic and Bathymetric Maps. The purpose of this lab is to provide experience interpreting the bathymetry of the seafloor in terms of tectonic and geologic settings and processes. Use the

More information

The Ocean Floor Earth Science, 13e Chapter 13

The Ocean Floor Earth Science, 13e Chapter 13 The Ocean Floor Earth Science, 13e Chapter 13 Stanley C. Hatfield Southwestern Illinois College The vast world ocean Earth is often referred to as the blue planet Seventy-one percent of Earth s surface

More information

Ocean Floor. Continental Margins. Divided into 3 major regions. Continental Margins. Ocean Basins. Mid-Ocean Ridges. Include:

Ocean Floor. Continental Margins. Divided into 3 major regions. Continental Margins. Ocean Basins. Mid-Ocean Ridges. Include: Ocean Floor Divided into 3 major regions Continental Margins Ocean Basins Mid-Ocean Ridges Continental Margins Include: Continental Shelves Continental Slopes Continental Rise 1 Continental Shelves Part

More information

Map shows 3 main features of ocean floor

Map shows 3 main features of ocean floor Map shows 3 main features of ocean floor 2017 Pearson Education, Inc. Chapter 3 Marine Provinces 2017 Pearson Education, Inc. 1 Chapter 3 Overview The study of bathymetry determines ocean depths and ocean

More information

Bathymetry Measures the vertical distance from the ocean surface to mountains, valleys, plains, and other sea floor features

Bathymetry Measures the vertical distance from the ocean surface to mountains, valleys, plains, and other sea floor features 1 2 3 4 5 6 7 8 9 10 11 CHAPTER 3 Marine Provinces Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools.

More information

Lecture Outlines PowerPoint. Chapter 13 Earth Science 11e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 13 Earth Science 11e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 13 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

More information

Full file at

Full file at Essentials of Oceanography, 10e (Trujillo/Keller) Chapter 2 Plate Tectonics and the Ocean Floor Match the term with the appropriate phrase. You may use each answer once, more than once or not at all. A)

More information

The Ocean Floor Chapter 14. Essentials of Geology, 8e. Stan Hatfield and Ken Pinzke Southwestern Illinois College

The Ocean Floor Chapter 14. Essentials of Geology, 8e. Stan Hatfield and Ken Pinzke Southwestern Illinois College The Ocean Floor Chapter 14 Essentials of Geology, 8e Stan Hatfield and Ken Pinzke Southwestern Illinois College The vast world ocean Earth is often referred to as the water planet 71% of Earth s surface

More information

Oceanography, An Invitation to Marine Science 9e Tom Garrison. Ocean Basins Cengage Learning. All Rights Reserved.

Oceanography, An Invitation to Marine Science 9e Tom Garrison. Ocean Basins Cengage Learning. All Rights Reserved. Oceanography, An Invitation to Marine Science 9e Tom Garrison 4 Ocean Basins Key Concepts Tectonic forces shape the seabed The ocean floor is divided into continental margins and deep ocean basins The

More information

Geography of the world s oceans and major current systems. Lecture 2

Geography of the world s oceans and major current systems. Lecture 2 Geography of the world s oceans and major current systems Lecture 2 WHY is the GEOMORPHOLOGY OF THE OCEAN FLOOR important? (in the context of Oceanography) WHY is the GEOMORPHOLOGY OF THE OCEAN FLOOR important?

More information

Chapter Overview. Bathymetry. Measuring Bathymetry. Measuring Bathymetry

Chapter Overview. Bathymetry. Measuring Bathymetry. Measuring Bathymetry CHAPTER 3 Marine Provinces Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools. Most ocean floor features

More information

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question.

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. Geology 300, Physical Geology Spring 2019 Quiz Chapter 18, Seafloor Name MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. 1) Abyssal fans are made

More information

MARINE GEOLOGY & GEOGRAPHY

MARINE GEOLOGY & GEOGRAPHY MARINE GEOLOGY & GEOGRAPHY Bathymetry BATHYMETRY BATHYMETRY THE UNDERWATER EQUIVALENT TO TOPOGRAPHY THE STUDY OF WATER DEPTH A BATHYMETRIC MAP SHOWS FLOOR RELIEF OR TERRAIN AS CONTOUR LINES Bathymetry

More information

EARTH SCIENCE 11 PLATE TECTONICS - CHAPTERS13 &14 DIAGRAMS & TERMINOLOGY REVIEW. Plate Boundaries. Hot Spots. Type of Plate Boundary CONVERGENT

EARTH SCIENCE 11 PLATE TECTONICS - CHAPTERS13 &14 DIAGRAMS & TERMINOLOGY REVIEW. Plate Boundaries. Hot Spots. Type of Plate Boundary CONVERGENT EARTH SCIENCE 11 PLATE TECTONICS - CHAPTERS13 &14 DIAGRAMS & TERMINOLOGY REVIEW KEY Plate oundaries Point A C D Type of Plate oundary CONVERGENT DIVERGENT SPREADING CENTER SLIDING TRANSCURRENT / FAULT

More information

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Oceans: The Last Frontier Foundations, 6e - Chapter 9 Stan Hatfield Southwestern Illinois College The vast world ocean Earth is often referred

More information

OCN 201 Physiography of the Seafloor

OCN 201 Physiography of the Seafloor OCN 201 Physiography of the Seafloor Hypsometric Curve for Earth s solid surface Note histogram Hypsometric curve of Earth shows two modes. Hypsometric curve of Venus shows only one! Why? Ocean Depth vs.

More information

Examining the Terrestrial Planets (Chapter 20)

Examining the Terrestrial Planets (Chapter 20) GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Examining the Terrestrial Planets (Chapter 20) For this assignment you will require: a calculator, colored pencils, a metric ruler, and your geology

More information

60% water. Big Bang: 14,000 millions years ago The Earth originated about 4,500 millions years ago its orbit allows water to exist in a liquid state!

60% water. Big Bang: 14,000 millions years ago The Earth originated about 4,500 millions years ago its orbit allows water to exist in a liquid state! Ch2. The Sea Floor #1 Why geology of the oceans? Marine habitats are directly shaped by geological processes The form of the coastlines The depth of the water Type of bottom (muddy, sandy, rocky) #2 Geological

More information

Lecture Marine Provinces

Lecture Marine Provinces Lecture Marine Provinces Measuring bathymetry Ocean depths and topography of ocean floor Sounding Rope/wire with heavy weight Known as lead lining Echo sounding Reflection of sound signals 1925 German

More information

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor

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,

More information

Chapter 2 Plate Tectonics and the Ocean Floor

Chapter 2 Plate Tectonics and the Ocean Floor Chapter 2 Plate Tectonics and the Ocean Floor Matching. Match the term or person with the appropriate phrase. You may use each answer once, more than once or not at all. 1. hydrothermal vents A. convergent

More information

3.1 GEOLOGY AND SOILS Introduction Definition of Resource

3.1 GEOLOGY AND SOILS Introduction Definition of Resource 3.1 GEOLOGY AND SOILS 3.1.1 Introduction 3.1.1.1 Definition of Resource The geologic resources of an area consist of all soil and bedrock materials. This includes sediments and rock outcroppings in the

More information

Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor

Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor Multibeam echo sounders - Research vessel Scripps Institution of Oceanography R/V Roger Revelle depth Source: Scripps Institution of Oceanography http://woodshole.er.usgs.gov/project-pages/caribbean/movie1.html

More information

Unit 6: The Sea Floor

Unit 6: The Sea Floor Unit 6: The Sea Floor Turn to Page 62 in Introduction to the World s Oceans Study the bathymetric chart What features do you see? How do the Atlantic and Pacific Oceans differ? What do you think accounts

More information

4) Treyson Gillespie and Dr. Leslie Sautter Bathymetric Analysis of Glaciokarstic Limestone Substrate on the Western Irish Coast

4) Treyson Gillespie and Dr. Leslie Sautter Bathymetric Analysis of Glaciokarstic Limestone Substrate on the Western Irish Coast 2017 US Hydro Conference Academic Poster Abstracts by College of Charleston BEAMS Program students 1) Evalynn Barbare and Dr. Leslie Sautter Using Multibeam Sonar to Identify Potential Deep Sea Coral Habitat

More information

Marine Science and Oceanography

Marine Science and Oceanography Marine Science and Oceanography Marine geology- study of the ocean floor Physical oceanography- study of waves, currents, and tides Marine biology study of nature and distribution of marine organisms Chemical

More information

B.C. s Offshore Oil and Gas: a Guide to the Geology and Resources.

B.C. s Offshore Oil and Gas: a Guide to the Geology and Resources. B.C. s Offshore Oil and Gas: a Guide to the Geology and Resources. Introduction Beneath the offshore regions of British Columbia are four moderately large, geologically young sedimentary basins (Figure

More information

Understanding The Seafloor. Dr. Frank R. Hall. Resources for pictures, etc. used in this presentation

Understanding The Seafloor. Dr. Frank R. Hall. Resources for pictures, etc. used in this presentation Slide 1 Understanding The Seafloor Dr. Frank R. Hall Geological Oceanographer University of New Orleans New Orleans, LA 2003 This is a presentation prepared in the Summer 2003 for the Gulf Coast COSSEE

More information

Coastal and Marine Ecological Classification Standard (CMECS)

Coastal and Marine Ecological Classification Standard (CMECS) Coastal and Marine Ecological Classification Standard (CMECS) Mark Finkbeiner NOAA Coastal Services Center Presented at the International Workshop on Seabed Mapping Methods and Technology 18 October 2012

More information

Seafloor Morphology. Techniques of Investigation. Bathymetry and Sediment Studies

Seafloor Morphology. Techniques of Investigation. Bathymetry and Sediment Studies Seafloor Morphology I f we select a grid for the surface of the earth (i.e. 5 km 2 ) and assign it an average elevation in relation to sea level, we can construct a graph of elevation versus area of the

More information

Earth s Seafloors. Ocean Basins and Continental Margins. Introductory Oceanography Ray Rector - Instructor

Earth s Seafloors. Ocean Basins and Continental Margins. Introductory Oceanography Ray Rector - Instructor Earth s Seafloors Ocean Basins and Continental Margins Introductory Oceanography Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types

More information

SEABED MORPHOLOGY OFF SOUTHERN LONG ISLAND: STUDIES OF ARTIFICIAL REEFS AND IMPLICATIONS FOR WIND FARMS. Juliet Kinney & Roger D.

SEABED MORPHOLOGY OFF SOUTHERN LONG ISLAND: STUDIES OF ARTIFICIAL REEFS AND IMPLICATIONS FOR WIND FARMS. Juliet Kinney & Roger D. SEABED MORPHOLOGY OFF SOUTHERN LONG ISLAND: STUDIES OF ARTIFICIAL REEFS AND IMPLICATIONS FOR WIND FARMS Juliet Kinney & Roger D. Flood Marine Sciences Research Center, Stony Brook University Stony Brook,

More information

Oceanography is the scientific study of oceans Oceans make up over 70% of the Earth s surface

Oceanography is the scientific study of oceans Oceans make up over 70% of the Earth s surface Oceanography Oceanography is the scientific study of oceans Oceans make up over 70% of the Earth s surface An ocean must be large and have features which set it apart from other oceans (currents, water

More information

Introduction to Acoustic Remote Sensing and Seafloor Mapping (AE4-E13) May 19, 2010

Introduction to Acoustic Remote Sensing and Seafloor Mapping (AE4-E13) May 19, 2010 Introduction to Acoustic Remote Sensing and Seafloor Mapping (AE4-E13) May 19, 2010 1 Delft Vermelding Institute onderdeel of Earth organisatie Observation and Space Systems Why Acoustic Remote Sensing?

More information

Chapter 9 Lecture Outline. Oceans: The Last Frontier

Chapter 9 Lecture Outline. Oceans: The Last Frontier Chapter 9 Lecture Outline Oceans: The Last Frontier The Vast World Ocean Earth is referred to as the blue planet 71% of Earth s surface is oceans and marginal seas Continents and islands comprise the remaining

More information

Chapter 2 Plate Tectonics and the Ocean Floor

Chapter 2 Plate Tectonics and the Ocean Floor Chapter 2 Plate Tectonics and the Ocean Floor Chapter Overview Much evidence supports plate tectonics theory. The plate tectonics model describes features and processes on Earth. Plate tectonic science

More information

Unit 4 - Water. Earth s Interior. Earth s Interior. Continental Drift. Continental Drift. Continental Drift. Crust. Mantle. Core.

Unit 4 - Water. Earth s Interior. Earth s Interior. Continental Drift. Continental Drift. Continental Drift. Crust. Mantle. Core. Unit 4 - Water How did the oceans form? What special adaptations do saltwater organisms have? Where does our water come from? How do humans affect the Earth s water? Crust Rigid outer shell of Earth Oceanic

More information

Plate Tectonics: A Unifying Theory

Plate Tectonics: A Unifying Theory Plate Tectonics: A Unifying Theory What is Plate Tectonics? - 7 large tectonic plates and many smaller ones that break up the lithosphere - Plates are brittle and float on asthenosphere and glide past

More information

OCN 201 Physiography of the Seafloor

OCN 201 Physiography of the Seafloor OCN 201 Physiography of the Seafloor 1 Ocean Depth versus Continental Height Why do we have dry land? Solid surface of Earth is dominated by two levels: Land with a mean elevation of +840 m (29% of Earth

More information

Fluid-Rock Interactions and the Sub-Seafloor Biosphere

Fluid-Rock Interactions and the Sub-Seafloor Biosphere Fluid-Rock Interactions and the Sub-Seafloor Biosphere BACKGROUND DATA Examples of Key Scientific Questions (OOI Science Plan) Scientific Priorities (San Juan Meeting) Example ORION Experiments (San Juan

More information

An overview of the use of acoustic data for geology and habitat mapping in MAREANO

An overview of the use of acoustic data for geology and habitat mapping in MAREANO An overview of the use of acoustic data for geology and habitat mapping in MAREANO Margaret Dolan, Valerie Bellec, Sigrid Elvenes, Reidulv Bøe, Terje Thorsnes, Shyam Chand, Leif Rise, Monica Winsborrow

More information

Activity Turbidites in a Jar

Activity Turbidites in a Jar Sand Dikes & Marine Turbidites Activity Turbidites in a Jar Paleoseismology is the study of the timing, location, and magnitude of prehistoric earthquakes preserved in the geologic record. Knowledge of

More information

The Marine Environment

The Marine Environment The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write or. 1.

More information

Isostasy and Tectonics Lab Understanding the Nature of Mobile Floating Lithospheric Plates

Isostasy and Tectonics Lab Understanding the Nature of Mobile Floating Lithospheric Plates Isostasy and Tectonics Lab Understanding the Nature of Mobile Floating Lithospheric Plates Crust Mantle Dynamics Introductory Geology Lab Ray Rector - Instructor Isostasy and Tectonics Laboratory Topics

More information

Image: G. Parker. Presenters: Henry Chan, Kayla Ireland, Mara Morgenstern, Jessica Palmer, Megan Scott

Image: G. Parker. Presenters: Henry Chan, Kayla Ireland, Mara Morgenstern, Jessica Palmer, Megan Scott Image: G. Parker Presenters: Henry Chan, Kayla Ireland, Mara Morgenstern, Jessica Palmer, Megan Scott Is the Ross Formation a suitable analog for sand-rich turbidite plays in passive margin basins? Play:

More information

14.2 Ocean Floor Features Mapping the Ocean Floor

14.2 Ocean Floor Features Mapping the Ocean Floor 14.2 Ocean Floor Features Mapping the Ocean Floor The ocean floor regions are the continental margins, the ocean basin floor, and the mid-ocean ridge. 14.2 Ocean Floor Features Continental Margins A continental

More information

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE!

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE! ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE! WHAT PROMINENT FEATURE CAN YOU IDENTIFY IN THIS PICTURE? What do you think the different colors represent? Who might find such a picture

More information

24. Ocean Basins p

24. Ocean Basins p 24. Ocean Basins p. 350-372 Background The majority of the planet is covered by ocean- about %. So the majority of the Earth s crust is. This crust is hidden from view beneath the water so it is not as

More information

Alfred Wegener gave us Continental Drift. Fifty years later...

Alfred Wegener gave us Continental Drift. Fifty years later... CHAPTER 2 Plate Tectonics and the Ocean Floor Plate Tectonics: summary in haiku form Alfred Wegener gave us Continental Drift. Fifty years later... Words Chapter Overview Much evidence supports plate tectonics

More information

Earth / Environmental Science. Ch. 14 THE OCEAN FLOOR

Earth / Environmental Science. Ch. 14 THE OCEAN FLOOR Earth / Environmental Science Ch. 14 THE OCEAN FLOOR The Blue Planet Nearly 70% of the Earth s surface is covered by the global ocean It was not until the 1800s that the ocean became an important focus

More information

Marine Sediments. Introductory Oceanography. Ray Rector: Instructor

Marine Sediments. Introductory Oceanography. Ray Rector: Instructor Marine Sediments Introductory Oceanography Ray Rector: Instructor Ocean Basins are Vast Sinks for Huge Amounts of Sediment from Numerous Different Sources Four Major Types of Seafloor Sediments 1. Lithogenous

More information

Oceanography Field Trip One Key

Oceanography Field Trip One Key Oceanography Field Trip One Key If you are using this key as a make-up guide, you should get a COLOR version of this field trip guide by going to http://www.mpcfaculty.net/alfred_hochstaedter/oceanography.htm

More information

Plate Tectonics. entirely rock both and rock

Plate Tectonics. entirely rock both and rock Plate Tectonics I. Tectonics A. Tectonic Forces are forces generated from within Earth causing rock to become. B. 1. The study of the origin and arrangement of Earth surface including mountain belts, continents,

More information

Crustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones

Crustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones Name: Date: Period: Tectonics The Physical Setting: Earth Science CLASS NOTES Tectonics - s - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones The plates are

More information

Activity #3 - Bathymetric Mapping

Activity #3 - Bathymetric Mapping Activity #3 - Bathymetric Mapping Concepts # 1, 2 #1 The floor of the ocean is composed of hills, plains, ridges, trenches, and seamounts. #2 Oceanographers have developed methods for mapping the ocean

More information

Plate Tectonics Tutoiral. Questions. Teacher: Mrs. Zimmerman. Plate Tectonics and Mountains Practice Test

Plate Tectonics Tutoiral. Questions. Teacher: Mrs. Zimmerman. Plate Tectonics and Mountains Practice Test Teacher: Mrs. Zimmerman Print Close Plate Tectonics and Mountains Practice Test Plate Tectonics Tutoiral URL: http://www.hartrao.ac.za/geodesy/tectonics.html Questions 1. Fossils of organisms that lived

More information

Science EOG Review: Landforms

Science EOG Review: Landforms Mathematician Science EOG Review: Landforms Vocabulary Definition Term canyon deep, large, V- shaped valley formed by a river over millions of years of erosion; sometimes called gorges (example: Linville

More information

FOOT OF THE CONTINENTAL SLOPE IN ARTICLE 76

FOOT OF THE CONTINENTAL SLOPE IN ARTICLE 76 FOOT OF THE CONTINENTAL SLOPE IN ARTICLE 76 Vaughan Stagpoole, Institute of Geological & Nuclear Sciences, Lower Hutt, New Zealand, v.stagpoole@gns.cri.nz Ray Wood, Institute of Geological & Nuclear Sciences,

More information

Marine ecosystem mapping at the Prince Edward Islands

Marine ecosystem mapping at the Prince Edward Islands Marine ecosystem mapping at the Prince Edward Islands Biodiversity Planning Forum NBA special session June 2018 R Adams, C von der Meden, A Dayaram, K Sink, A Lombard, A Bosman, M Dopolo, F Fourie, L Harris,

More information

Finding an Earthquake Epicenter Pearson Education, Inc.

Finding an Earthquake Epicenter Pearson Education, Inc. Finding an Earthquake Epicenter Measuring the Size of Earthquakes Two measurements that describe the size of an earthquake are: 1. Intensity a measure of the degree of earthquake shaking at a given locale

More information

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?

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)

More information

Science Targets Along a Proposed Gale Traverse. Ryan Anderson, Dawn Sumner & Jim Bell 5 th Mars Science Laboratory Landing Site Workshop May 17, 2011

Science Targets Along a Proposed Gale Traverse. Ryan Anderson, Dawn Sumner & Jim Bell 5 th Mars Science Laboratory Landing Site Workshop May 17, 2011 Science Targets Along a Proposed Gale Traverse Ryan Anderson, Dawn Sumner & Jim Bell 5 th Mars Science Laboratory Landing Site Workshop May 17, 2011 Traverse Overview This is a notional traverse. Based

More information

2) re-positioning of the SSS data, 3) individuation of geomorphological features and morphometrical parameters correlated to instability phenomena.

2) re-positioning of the SSS data, 3) individuation of geomorphological features and morphometrical parameters correlated to instability phenomena. HIGH-RESOLUTION SIDE SCAN SONAR AND MULTIBEAM DATA PROCESSING AND MERGING TO STUDY SUBMARINE INSTABILITY PHENOMENA ON VOLCANIC ISLANDS (PONTINE, CAMPANIAN AND AEOLIAN ARCHIPELAGOS) A. BOSMAN Extended abstract:

More information

Linking surficial geomorphology with vertical structure in high and low energy marine

Linking surficial geomorphology with vertical structure in high and low energy marine Linking surficial geomorphology with vertical structure in high and low energy marine environments Erica Sampaga 1 Advisors: Miles Logsdon, Emily Roland 1 University of Washington, School of Oceanography

More information

Divergent Boundaries: Origin and Evolution of the Ocean Floor

Divergent Boundaries: Origin and Evolution of the Ocean Floor 1 2 3 4 5 6 7 8 9 10 11 12 Divergent Boundaries: Origin and Evolution of the Ocean Floor Earth, 12 th Edition, Chapter 13 Chapter 13 Divergent Boundaries From 1872 to 1876, the HMS Challenger expedition

More information

Non-living Resources of the OCS. Harald Brekke NPD

Non-living Resources of the OCS. Harald Brekke NPD Non-living Resources of the OCS Harald Brekke NPD The Continental Shelf and the Area http://www.grida.no/publications/shelf-last-zone/ Outer Continental Shelf Example http://www.grida.no/publications/shelf-last-zone/

More information

Search and Discovery Article #40536 (2010) Posted June 21, 2010

Search and Discovery Article #40536 (2010) Posted June 21, 2010 Modern Examples of Mass Transport Complexes, Debrite and Turbidite Associations: Geometry, Stratigraphic Relationships and Implications for Hydrocarbon Trap Development* Fabiano Gamberi 1, Marzia Rovere

More information

Geol 117 Lecture 18 Beaches & Coastlines. I. Types of Coastlines A. Definition:

Geol 117 Lecture 18 Beaches & Coastlines. I. Types of Coastlines A. Definition: I. Types of Coastlines A. Definition: 1. Shore = narrow zone where ocean meets land (e.g. beach) 2. Coast is a broad area where both ocean and land processes act a. Includes onshore marshes, dunes, sea

More information

Origin and Evolution of the Ocean Floor

Origin and Evolution of the Ocean Floor Origin and Evolution of the Ocean Floor Outline Mapping the Ocean Floor Continental Margins Origin of Oceanic Lithosphere Structure of Ocean Crust Mapping the ocean floor Depth originally measured by lowering

More information

1. Define habitat and describe how geologic processes influence habitats. Habitats 2. How much of the earth s surface is covered by sea water?

1. Define habitat and describe how geologic processes influence habitats. Habitats 2. How much of the earth s surface is covered by sea water? 1. Define habitat and describe how geologic processes influence habitats. Habitats are the natural environments in which organisms live. They are directly shaped by geological processes, which influence

More information

The Marine Environment

The Marine Environment The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write true or

More information

Questions and Topics

Questions and Topics Plate Tectonics and Continental Drift Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence that Continents move? 3. What are the forces that

More information

Geochemistry, Geophysics, Geosystems. Supporting Information for

Geochemistry, Geophysics, Geosystems. Supporting Information for Geochemistry, Geophysics, Geosystems Supporting Information for Segment-scale variations in seafloor volcanic and tectonic processes from multibeam sonar imaging, Mid-Atlantic Ridge Rainbow region (35º45-36º35

More information

Basin & Range / Mojave Desert

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,

More information

In 1990, 50% of the U.S. population lived within 75 km of a coast. By 2010, 75% of the U.S. population will live within 75 km of a coast.

In 1990, 50% of the U.S. population lived within 75 km of a coast. By 2010, 75% of the U.S. population will live within 75 km of a coast. In 1990, 50% of the U.S. population lived within 75 km of a coast. By 2010, 75% of the U.S. population will live within 75 km of a coast. High Tech Methods for Surveying the Deep Sea Floor Fig. 20.18 1

More information

Magnitude 7.7 QUEEN CHARLOTTE ISLANDS REGION

Magnitude 7.7 QUEEN CHARLOTTE ISLANDS REGION A major 7.7 magnitude earthquake struck at 8:04 PM local time in western British Columbia, Canada. The epicenter is located on Moresby Island, the southern large island in the Queen Charlotte Islands region.

More information

Black Point & Bihler Point

Black Point & Bihler Point Black Point & Bihler Point Conglomerate Photo: looking north toward end of Black Point (south of post 1) All of the rocks in this photo are conglomerate. Both Black Point and Bihler Point are formed from

More information

Cross walking to the New Coastal and Marine Ecological Classification Standard (CMECS)

Cross walking to the New Coastal and Marine Ecological Classification Standard (CMECS) Cross walking to the New Coastal and Marine Ecological Classification Standard (CMECS) Mark Finkbeiner and Chris Robinson NOAA Coastal Services Center EBM Tools Webinar 16 May 2013 Outline What is CMECS

More information

Small area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA?

Small area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA? The Ocean Basins How Deep is the Ocean? 1 2 Three Major Oceans Three Major Oceans Pacific Atlantic the shallowest ocean (3.3km average depth) Indian second shallowest ocean (3.8km average depth) Pacific

More information

Essentials of Oceanography Eleventh Edition

Essentials of Oceanography Eleventh Edition Chapter Chapter 1 2 Clickers Lecture Essentials of Oceanography Eleventh Edition Plate Tectonics and the Ocean Floor Alan P. Trujillo Harold V. Thurman Chapter Overview Much evidence supports plate tectonics

More information

6. In the diagram below, letters A and B represent locations near the edge of a continent.

6. In the diagram below, letters A and B represent locations near the edge of a continent. 1. Base your answer to the following question on the cross section below and on your knowledge of Earth science. The cross section represents the distance and age of ocean-floor bedrock found on both sides

More information

Changes in Geomorphology and Backscatter Patterns in Mount Misery Shoal, Long Island Sound as Revealed through Multiple Multibeam Surveys

Changes in Geomorphology and Backscatter Patterns in Mount Misery Shoal, Long Island Sound as Revealed through Multiple Multibeam Surveys Changes in Geomorphology and Backscatter Patterns in Mount Misery Shoal, Long Island Sound as Revealed through Multiple Multibeam Surveys Laurie A. Zaleski Laurie.Zaleski@msrc.sunysb.edu, Roger D. Flood

More information

Objectives: Define Relative Age, Absolute Age

Objectives: 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 information

Paleo Lab #4 - Sedimentary Environments

Paleo Lab #4 - Sedimentary Environments Paleo Lab #4 - Sedimentary Environments page - 1. CHARACTERISTICS OF SEDIMENT Grain size and grain shape: The sizes and shapes of sedimentary particles (grains) are modified considerably during their transportation

More information

Submarine canyons and channels of the Tyrrhenian Sea: from geological observations to oceanographic, biological and hazards studies

Submarine canyons and channels of the Tyrrhenian Sea: from geological observations to oceanographic, biological and hazards studies SUBMARNE CANYON DYNAMCS - Sorrento, taly, 15-18 April 2015 Submarine canyons and channels of the Tyrrhenian Sea: from geological observations to oceanographic, biological and hazards studies Fabiano Gamberi

More information

Geology 12 FINAL EXAM PREP. Possible Written Response Exam Questions

Geology 12 FINAL EXAM PREP. Possible Written Response Exam Questions Geology 12 FINAL EXAM PREP Possible Written Response Exam Questions Use this study guide to prepare for the written response portion of the final exam. Name FINAL EXAM - POSSIBLE WRITTEN RESPONSE QUESTIONS

More information

Lecture Outline Wednesday - Friday February 14-16, 2018

Lecture Outline Wednesday - Friday February 14-16, 2018 Lecture Outline Wednesday - Friday February 14-16, 2018 Quiz 2 scheduled for Friday Feb 23 (Interlude B, Chapters 6,7) Questions? Chapter 6 Pages of the Past: Sedimentary Rocks Key Points for today Be

More information

Sediment and sedimentary rocks Sediment

Sediment and sedimentary rocks Sediment Sediment and sedimentary rocks Sediment From sediments to sedimentary rocks (transportation, deposition, preservation and lithification) Types of sedimentary rocks (clastic, chemical and organic) Sedimentary

More information

Active Tectonics. Earthquakes, Uplift, and Landscape. Edward A. Keller University of California, Santa Barbara

Active Tectonics. Earthquakes, Uplift, and Landscape. Edward A. Keller University of California, Santa Barbara Prentice Hall Earth Science Series SUB Gottingen 214 80416X, im ^, 2002 A 7883 lllllllilwii Active Tectonics Earthquakes, Uplift, and Landscape Second Edition V Edward A. Keller University of California,

More information

MARINE GEOLOGY & GEOGRAPHY

MARINE GEOLOGY & GEOGRAPHY MARINE GEOLOGY MARINE GEOLOGY & GEOGRAPHY Marine Geology 4 LAYERS OF THE EARTH CRUST THICKNESS: VARIES BETWEEN OCEAN & CONTINENTS 5-40 KM STATE: SOLID ELEMENTS: SILICON, ALUMINUM, CALCIUM, SODIUM, POTASSIUM

More information

A. rift valley B. deep trench C. volcanic cone D. uplifted mountain. A. a volcanic island arc B. a large watershed area

A. rift valley B. deep trench C. volcanic cone D. uplifted mountain. A. a volcanic island arc B. a large watershed area DC Practice Test Dynamic Crust PRCTICE TEST Zimm's Earth Science 2013 1. Which feature would most likely be forming at converging continental tectonic plate boundaries?. rift valley. deep trench C.

More information

Marine Geosciences / Oceanography Fields and disciplines

Marine Geosciences / Oceanography Fields and disciplines Marine Geosciences / Oceanography Fields and disciplines Marine Geosciences; Oceanography Chemical Oceanography Marine chemistry; marine geochemistry Biological Oceanography Marine biology; marine biogeochemistry

More information

Origin and Evolution of the Ocean Floor

Origin and Evolution of the Ocean Floor Chapter 13 Lecture Earth: An Introduction to Physical Geology Twelfth Edition Origin and Evolution of the Ocean Floor Tarbuck and Lutgens Chapter 13 Divergent Boundaries An Emerging Picture of the Ocean

More information

CHAPTER 2 Plate Tectonics and the Ocean Floor Pearson Education, Inc.

CHAPTER 2 Plate Tectonics and the Ocean Floor Pearson Education, Inc. CHAPTER 2 Plate Tectonics and the Ocean Floor Plate Tectonics Alfred Wegener first proposed in 1912 Called it Continental Drift Evidence for Continental Drift 1. Noted puzzle-like fit of modern continents

More information

Seas. A sea is a part of an ocean that is nearly surrounded by water. The Mediterranean, Arctic and Black Sea are really part of the Atlantic Ocean.

Seas. A sea is a part of an ocean that is nearly surrounded by water. The Mediterranean, Arctic and Black Sea are really part of the Atlantic Ocean. Exploring the Ocean Since ancient times people have studied the ocean such as waters and ocean floor It provides food and services, and serves as a route for trade and travel The World s Oceans 71% of

More information

Submersible investigation of unconfirmed western Miami Terrace habitat

Submersible investigation of unconfirmed western Miami Terrace habitat Submersible investigation of unconfirmed western Miami Terrace habitat Prepared By: Brian K. Walker, Ph.D. Nova Southeastern University Oceanographic Center 6/08/2015 On June 5, 2015 Nova Southeastern

More information

Z046 Seismic Characteristics of Gas Migration Structures on the North Atlantic Margin Imaged by High-resolution 3D Seismic

Z046 Seismic Characteristics of Gas Migration Structures on the North Atlantic Margin Imaged by High-resolution 3D Seismic Z046 Seismic Characteristics of Gas Migration Structures on the North Atlantic Margin Imaged by High-resolution 3D Seismic O.K. Eriksen* (P-Cable 3D Seismic), C. Berndt (IFM-GEOMAR), S. Buenz (University

More information

Divergent Boundaries: Origin and Evolution of the Ocean Floor Earth - Chapter 13 Stan Hatfield Southwestern Illinois College

Divergent Boundaries: Origin and Evolution of the Ocean Floor Earth - Chapter 13 Stan Hatfield Southwestern Illinois College Divergent Boundaries: Origin and Evolution of the Ocean Floor Earth - Chapter 13 Stan Hatfield Southwestern Illinois College Mapping the Ocean Floor Depth was originally measured by lowering weighted lines

More information

1. Erosion by Running Water Most powerful cause of erosion

1. Erosion by Running Water Most powerful cause of erosion I. Destructive Forces Notes: Destructive force: a process in which land is destroyed or changed such as weathering and erosion. All landforms are a result of a combination of constructive and destructive

More information