G.S.I. Seabed Survey Seminar Possible Carbonate Mound Distribution November 2001 Thomas Furey.

Slides:



Advertisements
Similar presentations
T Netherlands Institute of Applied Geoscience TNO - National Geological Survey How can injected CO 2 be monitored? OSPAR Workshop, Trondheim, November.
Advertisements

Data integration: publications. Data integration: datasets Sediment core description sheets Sediment core description sheets Sediment core description.
Ireland’s Marine Mapping Programme & Atlantic Priorities Koen Verbruggen Geological Survey of Ireland Atlantic Mapping Workshop Dublin Castle, Dec 2 nd,
NVC0901 Maritime Alliance Symposium San Diego, August 2011 By: Michael Broadbent Fugro Pelagos Inc. Seafloor Mapping Technologies.
Structural character of the terrace zone and implications for crater formation: Chicxulub impact crater David L. Gorney Sean Gulick Gail Christeson GSA.
OCEANIC TOPOGRAPHY By Greg Schwab May 7, Competency 39 The teacher understands structure and function of the hydrosphere The teacher understands.
Mesophotic Coral Ecosystems of Puerto Rico and the US Virgin Islands Roy Armstrong, Ph.D. Bio-optical Oceanography Laboratory University of Puerto Rico.
Characterization of Mesophotic Coral Reefs Using the Seabed AUV Roy A. Armstrong 1 and Hanumant Singh 2 1 Bio-optical Oceanography Laboratory, Deapartment.
UNIT ONE: Science Skills  Chapter 1Measurement  Chapter 2The Scientific Process  Chapter 3Mapping Earth.
Mapping Earth's Surface Review and Assessment Answers
Sonar Chapter 9. History Sound Navigation And Ranging (SONAR) developed during WW II –Sound pulses emitted reflected off metal objects with characteristic.
An evaluation of regional active along-slope and down-slope processes of the NW European continental margin Michael Cunningham, Sophie Hodgson, Lindsay.
Abstract Detection of active faults and seismic hazards in the Seattle area is problematic, owing to thick surficial deposits and abundant vegetative cover.
Multibeam Sonar Mapping and Scallop Stock Assessment: GIS Data Integration in Support of Sustainable Fisheries Management Gerry Sutton O.Tully, J. Hickey:
3 What does the bottom of the ocean look like? OR What is the topography or bathymetry of the ocean floor?
Chapter 5 Interpreting Topographical Maps.
Coordinate System Unit 1: Mapping the Earth
Bathymetry of the Sea Floor
Mapping the Seafloor. Depth Soundings The earliest soundings were made with a hand line of rope weighted at one end. The earliest soundings were made.
EXPLORING THE OCEAN FLOOR pbs
Earth Science System Energy Constructive Force Destructive Force
Multibeam Bathymetric and Backscatter Products for Benthic Habitat Mapping There’s No Silver Bullet Joyce Miller Pacific Islands Fisheries Science Center.
Subject: Geography Topic: Where are we?--- Basic Map Reading Skills
Maps and Map Reading.
Wet DEMs – Lessons Learned Working with Bathymetric Data in the Hawaiian Islands Emily Lundblad NOAA Pacific Islands Fisheries Science Center Coral Reef.
Understanding maps Geographical Data Skills (Part 1)
Geologic Sea-Floor Mapping: Marine Data Model Case Study Brian Andrews-USGS, Woods Hole, MA Seth Ackerman-CZM, Woods Hole, MA.
Maps  A map is a model or representation of the Earth’s surface.  The map contains latitude and longitude.  The United States is always North of the.
Understanding maps Geographical Data Skills (Part 1)
Ice sheets viewed from the ocean: the contribution of marine science to understanding modern and past ice sheets by Colm Ó Cofaigh Philosophical Transactions.
Chapter 3 Section 1- Finding Locations on Earth
Geography of Canada Geographer’s Toolkit.
Structure of Ocean Basins Chapter 4. Focus now on structure  Problem of the ocean being remote  First “soundings” were made with a weight attached to.
Lidar Bathymetry – Technology and applications Oct 24rd, Netanya, Israel Anders Ekelund Managing Director Airborne Hydrography AB.
Labs Start Next Week Don’t forget your lab book!!!  Read through labs ahead of time  Exploring the Deep: GEO/OC 103 Lab Manual by Hall-Wallace et al.
What are Latitudes and Longitudes?
Mapping Earth Chapter 1 Earth Science. Ch1 L.1 Maps How can a map help determine location? Why are there different map projections for representing Earth’s.
3 Bathymetry of the Ocean Floor Bathymetry= measuring ocean depths and charting the shape or topography of the ocean floor “Sounding” lines (started in.
Mapping the SF Bay Overview SF Bay: Know the waterways and bridges.
Chapter 4 The Sea Floor and Its Sediments. 4.1 Measuring the Depths Methods for measuring depths: Hand line and wire marked with fathoms, with a lead.
The Global Ocean The Vast World Ocean.
Hydrographic Services Review Panel October 2010 David Fox Oregon Department of Fish & Wildlife Marine Resources Program Use of seafloor mapping data in.
Oceans Basins. Ocean Bathymetry ► The study of underwater depth and ocean floor. ► In the same way that topographic maps represent the three-dimensional.
SIDE SCAN OVERVIEW. Sidescan Survey Overview A sidescan sonar can be used for a wide variety of survey operations. Search and recovery Geological Identification.
UNCLASSIFIED The CarbonNet Project MMV constraints for shallow-water nearshore storage sites POSTER A Index Map: Location of Gippsland Basin in Victoria,
ALEXANDRU – VLAD LAZAR 1, GHEORGHE – VIOREL UNGUREANU 1,2, ALEXANDRU – DAN IONESCU 1, ANDREI – DANIEL BALAHURA 1*, ROBERT LAZAR 1, ALEXANDRU MAGHER 1 1.
© 2002 Brooks/Cole, a division of Thomson Learning, Inc. BATHYMETRY New technology, such as this bathyscaphe, allows scientists to study deep-ocean basins.
Bellringer Explain in complete sentences what are pros and cons of coal energy use.
1 Web Search What are coral reefs? How are they formed? 2 Image Search Find a map that shows the areas of the world where coral reefs can be found.
© 2014 Pearson Education, Inc. Marine Provinces Chapter 1 Clickers Essentials of Oceanography Eleventh Edition Alan P. Trujillo Harold V. Thurman © 2014.
Geography of Canada Mr. Hartley, Malvern Collegiate Geographer’s Toolkit.
Earth Science Chapter 2. $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $100 Earth’s.
Instructor: Dr. C. Charles Dong,
Mapping Overview.
Measuring bathymetry Ocean depths and topography of ocean floor
Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools.
Developments in Seabed Mapping
Bathymetry of the Sea Floor
Topographic Difference Models
Geography CORNELL NOTES.
Mapping the Seafloor.
Mapping Earth Science.
Mapping the Seafloor.
How do maps help us model the Earth?
MORPHOLOGICAL AND SEDIMENTARY CHARACTERIZATION THROUGH ANALYSIS OF MULTIBEAM DATA AT DECEPTION ISLAND, ANTARCTIC Filipe Japiassu Leitão, Arthur Ayres.
The Ocean Basins.
Marine Habitat Mapping, Applications for Fisheries Management
by Alan M. Roberts, Andrew D. Alvey, and Nick J. Kusznir
PORCUPINE STUDIES GROUP
Oceans Basins.
Presentation transcript:

G.S.I. Seabed Survey Seminar Possible Carbonate Mound Distribution November 2001 Thomas Furey

Presentation Overview n Introduction. n Overview of carbonate mound distribution to date offshore Ireland. n Mounds and their settings, data examples, data resolution. n Summary and conclusions.

What Are Mounds? n Topographic highs - circular & ridge morphology Of what importance are they? n Environmental – Associated coral ecosystems n Hazards – trawling damage, shallow gas Line 140, Area 3A 30 m 500 m

Interested Groups GEOMOUND – htttp://geomound.ucd.ieGEOMOUND – htttp://geomound.ucd.ie ECOMOUNDECOMOUND ACES - Atlantic Coral Ecosystem StudyACES - Atlantic Coral Ecosystem Study CORSAIRESCORSAIRES ENAM-2ENAM-2 Recent Irish Studies 1996 AIRS survey - Gloria1996 AIRS survey - Gloria Logachev Seismic & SidescanLogachev Seismic & Sidescan Belgica SeismicBelgica Seismic

Mound Identification Trawling, sidescan sonar, seismic.Trawling, sidescan sonar, seismic. Sub bottom profiler.Sub bottom profiler. Multibeam – bathymetry & backscatter.Multibeam – bathymetry & backscatter. Problems incurred: How are they identified? Multibeam Chart Resolution: 1 Pixel = 100 m 2Multibeam Chart Resolution: 1 Pixel = 100 m 2 Contour Interval = 50 m Sub Bottom Profiles: 2D, Digital InterpretationSub Bottom Profiles: 2D, Digital Interpretation

Mound Characteristics Water Depth Ranges: mWater Depth Ranges: m Size:Size: –Height Range: m approximately –Diameter: 250 metres km –Elongate Reefs (?) : Several Km’s

GEOMOUND Carbonate Mounds 24ºW 20 ºW 16 ºW 12 ºW 8 ºW 4 ºW 56 ºN 54ºN 52 ºN 50 ºN 48 ºN 56 ºN 54ºN 52 ºN 50 ºN 48 ºN NWRT SERT MPB SPB

Mound Groups South Porcupine Bite – SPBSouth Porcupine Bite – SPB Main Porcupine Basin – MPBMain Porcupine Basin – MPB South East Rockall Trough – SERTSouth East Rockall Trough – SERT North West Rockall Trough – NWRTNorth West Rockall Trough – NWRT West Rockall Bank – WRBWest Rockall Bank – WRB Edoras Bank - EBEdoras Bank - EB Fangorn Bank - FBFangorn Bank - FB

24ºW 20 ºW 16 ºW 12 ºW 8 ºW 4 ºW 56 ºN 54ºN 52 ºN 50 ºN 48 ºN 56 ºN 54ºN 52 ºN 50 ºN 48 ºN Possible Mound Distribution 2001 EB FB WRB

Bathymetric Mound Distribution Bathymetric Mound Distribution 23º W 18º W 13º W 8º W 57º N 52º N 57º N 52º N 500 m 1000 m 1500 m 2000 m

23º W 18º W 13º W 8º W 57º N 52º N 57º N 52º N PAD Structural Map & Mounds NEXT SLIDE

West Rockall Bank Mounds PINCH MICKS IMAGE – add transects Mounds Ridge 020 km N

West Rockall Bank Mound Example Mound Location 30 metres 500 metres Acoustic Blanking Sub Bottom Profile – Line 144 WSW ENE

Shaded Relief with Bathymetric Contours. WRB Mounds N Line 156 Line 155 Line 154 Line 153 Tracklines Ridge Isolated Mound Contour Parallel Mounds

Raw Backscatter Data - WRB 5 km 50 km WSW ENE

Raw Backscatter Data - WRB n Individual Mounds n Grouped Mounds n Elongate: North-South Contour Parallel Line 154 Line km 10 km

Line 144, Area 3A 500 metres 40 metres Small Mound x 20 metres WRB WRB Mounds 130 metres 1 km Line 155, Area 3A Large Mound metres x 1.5 km

20 metres Line 145, Area 3A 500 metres Acoustic Blanking Acousting Blanking Beneath Possible Gasified Mounds Conical Mound with Moat Feature 500 metres Acoustic Blanking Line 150, Area 3A 40 metres Moat WRB Mounds

Fangorn Bank Bathymetry Map Sheet 28 N Mound features 025 km

Next Slide N 025 km Fangorn Bank Shaded Relief Map Sheet 28

Fangorn Bank Sub bottom record - Line 1353 seabed 40 metres SENW 500 metres

MPB & SPB Mounds 3D Surface North Area 3E 40 km ShadedRelief MBP SPB

Conclusions n Additional Mound locations identified. n Relief useful Mound identification tool. n Raw Backscatter is good quality. n Small features require reprocessing. n West Rockall Bank study proposed. n Ground truthing required. n Large uninterpreted dataset available.

Zone 3 3A W.P. 3E 3F 3H

Area 3E colour contoured map of area covered N Ship track lines Depth Range 200 m to 4500 m 0150 km

Area 3E sun illuminated map of area covered Next slide Gollum Channel Complex 0150 km

Area 3E, Line Possible gas associated with Carbonate Mound. seabed Gas bearing sediment SW NE 500 metres