Mechanisms for persistence of Gracilariopsis andersonii in the Elkhorn Slough: links to sediments. Megan Wehrenberg Moss Landing Marine Labs

Size: px
Start display at page:

Download "Mechanisms for persistence of Gracilariopsis andersonii in the Elkhorn Slough: links to sediments. Megan Wehrenberg Moss Landing Marine Labs"

Transcription

1 Mechanisms for persistence of Gracilariopsis andersonii in the Elkhorn Slough: links to sediments Megan Wehrenberg Moss Landing Marine Labs

2 Gracilariopsis andersonii in Central CA Intertidal Open Coast Attached to rocky shelves Direct impact of swells Bays and Estuaries Within soft sediment No direct swell energy

3 Study Sites Pigeon Point California Santa Cruz ~69 km apart Elkhorn Slough N Monterey

4 Gracilariopsis andersonii Cylindrical, erect, perennial red alga Grows up to 2 m long Attached by small discoid holdfast to rock or shell or unattached Can tolerate periodic inundation by sand

5 Gracilariopsis andersonii Can propagation through vegetative fragmentation Biomass loss stimulates branching and can therefore stimulate growth Gracilaroids are 3 rd most cultivated group of seaweeds worldwide; world s major source of agar

6 Study Site Mouth of Elkhorn Slough Estuary in Moss Landing Protected, soft-sediment beach Google Earth Van Dyke- CDFG

7 Survey Sampled Jan Jan 2009 Measured above- and belowground biomass Measured reproductive biomass

8 Monthly Biomass- Elkhorn Slough Average Biomass g/m² Above-ground Below-ground J F M A M J J A S O N D J -Highest above-ground biomass in Fall -Primarily below-ground during winters

9 Below-ground Biomass in Elkhorn Slough Up to 40 cm below surface Highly fragmented Pigmented Healthy Suggests that new growth can be a result of exposure of underground material

10 Sexual Reproduction- Elkhorn Slough Average Biomass g/m² Vegetative Sexually reproductive 0 J F M A M J J A S O N D J -Only few reproductive fragments in August Sexual fertilization uncommon

11 Sedimentation in Elkhorn Slough Records of algal burial of this magnitude had not been reported Monthly algal biomass is greater or equal to the highest quantities reported in literature Sedimentation appears to play important role in the persistence of thriving bed

12 Mouth of Elkhorn Slough CA DFG Tidal velocities can reach 1.25m/s (Broenkow and Breaker 2005)

13 Bathymetry of Main Channel and Beach Flat Hwy 1 Bridge Southern Sub-tidal Mud Bank (Israel and Watt 2005) Bridge Contours = 1m

14 Investigating Depositional History Mean Grain Size Large Small Standard Deviation of Grain Size (Sorting) WELL POOR

15 Particle movement Velocity (cm/sec) Particle Size (mm) modified Hjulström diagram

16 Estuarine Grain Size Domains Bivariate plots used to evaluate the energy of the environment and the degree of processing Estuarine domains: Tanner (1991) modified by Lario et al. (2000) Closed Basins Storm (high energy) Environments 10 More sorting Soritng 1 Closed Basin Closed Basin 1 10 Mean grain size

17 Aids to Sedimentation Biological material can aid in sediment stabilization as well as deposition Seagrasses have been shown to baffle currents Enhance smaller particle deposition Bryan Largay

18 Questions 1. Was algal burial associated with seasonal sedimentary transport? 2. Did algae play a role in deposition (e.g. acting as sediment trap)?

19 Methods- Grain Size Analysis 24 cores collected randomly: July 08, October 08, January 09 Cores: 1.5 x 1.5 and collecting ~1ft (30cm) of sediment

20 Methods- Grain Size Analysis Cores extruded by gravity or with pressurized air Grain sizes analyzed using Coulter LS Laser Granulometer

21 Question 1. Was algal burial associated with seasonal sedimentary transport?

22 Methods- Monthly Surface Sediments I analyzed and compared grain sizes from the surface sediment (top 1cm of core) of all 24 cores collected in July 08, October 08, and January 09 Model I ANOVA (and Tukey post hoc) to test effect of month on sediment size 0-1cm for

23 Question 2. Did algae play a role in deposition (e.g. acting as sediment trap)?

24 Methods- Sediment Within Algae I analyzed and compared grain sizes from sediment within algae to sediment in locations without algae in January 09 cores only

25 Methods- Sediment Within Algae With Algae Without Algae 0cm 0cm 0cm 0cm 0cm 0cm 0cm 5cm 5cm 5cm 5cm 5cm 5cm 5cm 15cm 15cm 15cm 15cm 15cm 15cm 15cm 25cm 25cm 25cm 25cm 25cm 25cm 25cm 35cm 35cm 35cm 35cm 35cm 35cm 35cm

26 Methods- Sediment Within Algae With Algae A Without Algae 0cm 0cm 0cm 0cm 0cm 0cm 0cm 5cm 5cm 5cm 5cm 5cm 5cm 5cm 15cm 15cm 15cm 15cm 20cm 15cm 15cm 15cm 25cm 25cm 25cm 25cm 25cm 25cm 25cm 35cm 35cm 35cm 35cm 35cm 35cm 35cm

27 Methods- Sediment Within Algae With Algae A Without Algae N2 0cm 0cm 0cm 0cm 0cm 0cm 0cm 5cm 5cm 5cm 5cm 5cm 5cm 5cm 15cm 15cm 15cm 15cm 15cm 15cm 15cm 20cm 25cm 25cm 25cm 25cm 25cm 25cm 25cm 35cm 35cm 35cm 35cm 35cm 35cm 35cm N1 N3

28 Methods- Sediment Within Algae Compared grain sizes within core classifications A N1 N2 N3 with algae without algae Used Model I ANOVA (and Tukey post hoc) to test for effect of algae on sediment size composition

29 Results 1. Was algal burial associated with seasonal sedimentary transport?

30 Sediment Coring Months- Elkhorn Slough Average Biomass g/m² Above-ground Below-ground J F M A M J J A S O N D J

31 Results- Monthly surface sediments 5 Standard deviation (µm) July 08 October 08 January Mean diameter (µm)

32 Results- Monthly surface sediments 5 Better sorted Standard deviation (µm) July 08 October 08 January Mean diameter (µm) -Shift toward larger better sorted particles in Jan 09

33 Results- Monthly surface sediments 5 P= Average S.D (µm) SE July 08 n= 24 October 08 n= 24 January09 n= Average Mean (µm) SE

34 Nearby loss of beach sand Ivano Aiello, unpublished data

35 Minerals Smear slide of surface particles within site Identical mineral structure to sand found on surrounding beaches INT15 Ivano Aiello 500µm

36 Results 2. Did algae play a role in deposition (e.g. acting as sediment trap)?

37 Results- Core classifications in January 09 sediment 4 P > Average S.D. (µm) SE A N1 N2 N3 (n=19) (n=15) (n=9) (n=4) Average mean diameter (µm) SE

38 Conclusion Algal burial coincided with: shift in surface sediment toward larger, better sorted particles Simultaneous increase in wave height and erosion of beach sand from closest beaches Suggests sediment coming from beaches outside of slough

39 Conclusion Algae contained sediment with smaller more poorly sorted particles Suggests a baffling of currents by the biological material, aiding in sedimentation The biology controls the geology and the geology controls the biology

40 Significance The unique sedimentation cycle in the lower slough is sustaining one of the most dense populations of Gracilariopsis andersonii in central CA In an tidal estuary which is readily eroding, a source of biological material which provides a mechanical aid to sediment stabilization can be a major asset

41 Acknowledgements FUNDING: PADI Foundation (Grant #69) Surfrider Foundation Graduate Scholarship Meyers Oceanographic Trust Packard Foundation Signe Lundstrom Memorial Fund PSA- Hoshaw Award THESIS COMMITTEE: Dr. Michael Graham (MLML) Dr. Ivano Aiello (MLML) Dr. Alejandro Buschmann (ULAGOS, Chile)

42 Thank you!

Effects of erosion on subtidal communities in Elkhorn Slough. Catalina E. Reyes Moss Landing Marine Laboratories January 20, 2010

Effects of erosion on subtidal communities in Elkhorn Slough. Catalina E. Reyes Moss Landing Marine Laboratories January 20, 2010 Effects of erosion on subtidal communities in Elkhorn Slough Catalina E. Reyes Moss Landing Marine Laboratories January 2, 21 Estuarine Habitats Estuaries Low relief sedimentary Little to no rocky substrate

More information

Limits and Potentials of High Resolution Terrestrial Laser Scanning in Monitoring Estuarine Geomorphologic Variability.

Limits and Potentials of High Resolution Terrestrial Laser Scanning in Monitoring Estuarine Geomorphologic Variability. Limits and Potentials of High Resolution Terrestrial Laser Scanning in Monitoring Estuarine Geomorphologic Variability Charlie Endris January 20, 2010 Elkhorn Slough: Erosion and Habitat Loss Evolution

More information

Item #9: Amphipod Tox Proposal Modification Page 1 of 9

Item #9: Amphipod Tox Proposal Modification Page 1 of 9 Item #9: Amphipod Tox Proposal Modification Page 1 of 9 The effects of particle size and shape and animal health on toxicity test results using the amphipod Eohaustorius estuarius. Estimated Cost: $30,000

More information

Environmental Implications A Case Study

Environmental Implications A Case Study Grain Size Variations and Its Environmental Implications A Case Study DR PURANDARA BEKAL SCIENTIST, NATIONAL INSTITUTE OF HYDROLOGY HARD ROCK REGIONAL CENTER HANUMAN NAGAR BELGAUM, KARNATAKA Particle Transport

More information

Section 2.1 Ocean Basins. - Has helped determine where ocean basins are located. - Tectonic plates move changing the position of the continents.

Section 2.1 Ocean Basins. - Has helped determine where ocean basins are located. - Tectonic plates move changing the position of the continents. Science 8 Unit 1: Water Systems on Earth Chapter 2: Oceans Control the Water Cycle Section 2.1 Ocean Basins Oceans are important because: 1. Primary water source for the water cycle 2. Control weather

More information

TIDAL EROSION AT ELKHORN SLOUGH

TIDAL EROSION AT ELKHORN SLOUGH TIDAL EROSION AT ELKHORN SLOUGH Virtually all of California s tidal wetlands have been dramatically altered. Hydrological manipulations changes in water flow are widespread. Either flow has been decreased

More information

Sedimentary Rocks. Origin, Properties and Identification. Physical Geology GEOL 100. Ray Rector - Instructor

Sedimentary Rocks. Origin, Properties and Identification. Physical Geology GEOL 100. Ray Rector - Instructor Sedimentary Rocks Origin, Properties and Identification Physical Geology GEOL 100 Ray Rector - Instructor Sedimentary Rock Origin and Identification Lab Pre-Lab Internet Link Resources 1) http://www.rockhounds.com/rockshop/rockkey/index.html

More information

Sedimentary Rocks. Origin, Properties and Identification. Geology Laboratory GEOL 101 Lab Ray Rector - Instructor

Sedimentary Rocks. Origin, Properties and Identification. Geology Laboratory GEOL 101 Lab Ray Rector - Instructor Sedimentary Rocks Origin, Properties and Identification Geology Laboratory GEOL 101 Lab Ray Rector - Instructor Sedimentary Rock Origin and Identification Lab Pre-Lab Internet Link Resources 1) http://www.rockhounds.com/rockshop/rockkey/index.html

More information

UNIT SEVEN: Earth s Water. Chapter 21 Water and Solutions. Chapter 22 Water Systems. Chapter 23 How Water Shapes the Land

UNIT SEVEN: Earth s Water. Chapter 21 Water and Solutions. Chapter 22 Water Systems. Chapter 23 How Water Shapes the Land UNIT SEVEN: Earth s Water Chapter 21 Water and Solutions Chapter 22 Water Systems Chapter 23 How Water Shapes the Land Chapter Twenty-Three: How Water Shapes the Land 23.1 Weathering and Erosion 23.2

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

Grade 8 Science. Unit 1: Water Systems on Earth Chapter 2

Grade 8 Science. Unit 1: Water Systems on Earth Chapter 2 Grade 8 Science Unit 1: Water Systems on Earth Chapter 2 Oceans are important... 1. Primary water source for the water cycle 2. Control weather 3. Support diverse life 4. Provides humans with food, minerals,

More information

Modeling dispersal kernals with limited. information. Douglas T. Fischer, Louis W. Botsford, David M. Kaplan, J. William White, John Largier

Modeling dispersal kernals with limited. information. Douglas T. Fischer, Louis W. Botsford, David M. Kaplan, J. William White, John Largier Modeling dispersal kernals with limited http://www.nmfs.noaa.gov/habitat/ habitatprotection/profile/pacificcouncil.htm information Douglas T. Fischer, Louis W. Botsford, David M. Kaplan, J. William White,

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

Wetland Sediment Dynamics at Crissy Field Marsh Annual Report

Wetland Sediment Dynamics at Crissy Field Marsh Annual Report Wetland Sediment Dynamics at Crissy Field Marsh 27 Annual Report John Callaway Department of Environmental Science University of San Francisco 217 Fulton St. San Francisco, CA 94117 (415) 422-572 callaway@usfca.edu

More information

Sedimentary Rocks. Origin, Properties and Identification. Physical Geology GEOL 101 Lab Ray Rector - Instructor

Sedimentary Rocks. Origin, Properties and Identification. Physical Geology GEOL 101 Lab Ray Rector - Instructor Sedimentary Rocks Origin, Properties and Identification Physical Geology GEOL 101 Lab Ray Rector - Instructor Sedimentary Rock Origin and Identification Lab Pre-Lab Internet Link Resources 1) http://www.rockhounds.com/rockshop/rockkey/index.html

More information

Coastal Processes and Shoreline Erosion on the Oregon Coast, Cascade Head to Cape Kiwanda

Coastal Processes and Shoreline Erosion on the Oregon Coast, Cascade Head to Cape Kiwanda State of Oregon Department of Geology and Mineral Industries Vicki S. McConnell, State Geologist Open File Report OFR O-04-11 Coastal Processes and Shoreline Erosion on the Oregon Coast, Cascade Head to

More information

STUDY AREA AND METHODOLOGY

STUDY AREA AND METHODOLOGY . CHAPTER 2 STUDY AREA AND METHODOLOGY 26 CHAPTER 2 STUDY AREA AND METHODOLOGY Kundalika is a major river in konkan region of Maharashtra. River originates in Western Ghats at an altitude of 820 m ASL

More information

Unit 1: Water Systems on Earth Chapter 2

Unit 1: Water Systems on Earth Chapter 2 Unit 1: Water Systems on Earth Chapter 2 Create a mind map with the driving question, Why are Oceans Important? Remember: Why are oceans so important? Why are oceans so important? Primary water source

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

Understanding Earth Fifth Edition

Understanding Earth Fifth Edition Understanding Earth Fifth Edition Grotzinger Jordan Press Siever Chapter 5: SEDIMENTATION: Rocks Formed by Surface Processes Lecturer: H Mohammadzadeh Assistant professors, Department of Geology, FUM Copyright

More information

High Resolution Numerical Models of Tidal Marshes in the Delaware Bay

High Resolution Numerical Models of Tidal Marshes in the Delaware Bay High Resolution Numerical Models of Tidal Marshes in the Delaware Bay Ramona Stammermann Dept. of Civil, Architectural & Environmental Engineering, Drexel University, Philadelphia, PA Michael Piasecki

More information

The National Marine Biological Analytical Quality Control Scheme Particle Size Results PS34

The National Marine Biological Analytical Quality Control Scheme   Particle Size Results PS34 The National Marine Biological Analytical Quality Control Scheme www.nmbaqcs.org Particle Size Results PS34 David Hall Unicomarine Ltd. October 2009 E-mail: davidhall@unicomarine.com Contents Tables Table

More information

Sedimentary Rocks - are one of the three main rock types

Sedimentary Rocks - are one of the three main rock types Today s Objective: What Makes Sedimentary Rocks Special? Sedimentary Rocks - are one of the three main rock types A sedimentary rock can form one of three ways: 1. by the deposition of the weathered remains

More information

CLASSIC BOOKS OF OCEANOGRAPHY AND MARINE BIOLOGY: AN ANNOTATED BIBLIOGRAPHY. I. MARINE BOTANY

CLASSIC BOOKS OF OCEANOGRAPHY AND MARINE BIOLOGY: AN ANNOTATED BIBLIOGRAPHY. I. MARINE BOTANY CLASSIC BOOKS OF OCEANOGRAPHY AND MARINE BIOLOGY: AN ANNOTATED BIBLIOGRAPHY. I. MARINE BOTANY Introduction Janet Webster Hatfield Marine Science Center Oregon State University Newport, OR 97365 janet.webster@oregonstate.edu

More information

SHORELINE AND BEACH PROCESSES: PART 2. Implications for Coastal Engineering

SHORELINE AND BEACH PROCESSES: PART 2. Implications for Coastal Engineering SHORELINE AND BEACH PROCESSES: PART 2 Implications for Coastal Engineering Objectives of the lecture: Part 2 Show examples of coastal engineering Discuss the practical difficulties of ocean engineering

More information

RED LIST OF EUROPEAN HABITATS. Marine Results Presentation 24 th May, 2016

RED LIST OF EUROPEAN HABITATS. Marine Results Presentation 24 th May, 2016 RED LIST OF EUROPEAN HABITATS Marine Results Presentation 24 th May, 2016 Geographical scope of the project Habitat Typology One typology for marine and terrestrial At the same time... revision of EUNIS

More information

Surface Processes Focus on Mass Wasting (Chapter 10)

Surface Processes Focus on Mass Wasting (Chapter 10) Surface Processes Focus on Mass Wasting (Chapter 10) 1. What is the distinction between weathering, mass wasting, and erosion? 2. What is the controlling force in mass wasting? What force provides resistance?

More information

Weathering, Erosion, Deposition, and Landscape Development

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

More information

CHANGES IN BEACH SURFACE SEDIMENT COMPOSITION

CHANGES IN BEACH SURFACE SEDIMENT COMPOSITION CHANGES IN BEACH SURFACE SEDIMENT COMPOSITION Compiled by Tamsin Watt. Edited by Rendel Williams and Cherith Moses 1 Aims...2 2 Introduction...2 3 Sites...2 4 Survey methodology...2 5 Analysis procedure...3

More information

Chapter 2. Denudation: Rivers and Ice

Chapter 2. Denudation: Rivers and Ice Chapter 2. Denudation: Rivers and Ice DENUDATION: process that lowers level of land - caused by rivers, glaciers, waves & wind - involves processes of WEATHERING & EROSION Weathering Def: breakdown of

More information

CORRELATION ANALYSIS BETWEEN PALAEMONETES SHRIMP AND VARIOUS ALGAL SPECIES IN ROCKY TIDE POOLS IN NEW ENGLAND

CORRELATION ANALYSIS BETWEEN PALAEMONETES SHRIMP AND VARIOUS ALGAL SPECIES IN ROCKY TIDE POOLS IN NEW ENGLAND CORRELATION ANALYSIS BETWEEN PALAEMONETES SHRIMP AND VARIOUS ALGAL SPECIES IN ROCKY TIDE POOLS IN NEW ENGLAND Douglas F., Department of Biology,, Worcester, MA 01610 USA (D@clarku.edu) Abstract Palamonetes

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

Module 9 Sedimentary Rocks

Module 9 Sedimentary Rocks Module 9 Sedimentary Rocks SEDIMENTARY ROCKS Rocks formed from material derived from preexisting rocks by surfacial processes followed by diagenesis There are two main classes of sedimentary rocks Clastic

More information

THE CHANGING SURFACE OF THE EARTH

THE 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 information

A BEACH IS A BEACH. Or Is It? Hawaii. St. Croix, US Virgin Islands

A BEACH IS A BEACH. Or Is It? Hawaii. St. Croix, US Virgin Islands A BEACH IS A BEACH Or Is It? Pt. Reyes, California Western Florida Hawaii AGI What is a beach? Eastern Maine A beach is a strip of shoreline washed by waves and tides. Crane Key, Florida Bay St. Croix,

More information

Laboratory#6 Sediment Particle Size Distribution and Turbidity Flows

Laboratory#6 Sediment Particle Size Distribution and Turbidity Flows Laboratory#6 Sediment Particle Size Distribution and Turbidity Flows Although this laboratory will pertain to oceanic sediments similar processes can also be observed on land and other aquatic systems

More information

13. Sedimentary Rocks I (p )

13. Sedimentary Rocks I (p ) 13. Sedimentary Rocks I (p. 194-208) Sediment Deposition Weathering results in rock being broken down into smaller fragments, called regolith. This regolith is then broken down to form soil. The regolith

More information

What is weathering and how does it change Earth s surface? Answer the question using

What is weathering and how does it change Earth s surface? Answer the question using 7 th Grade Lesson What is weathering and how does it change Earth s surface? Answer the question using the sentence frame. You have 4 minutes. Weathering is. This changes the Earth s surface because. 1

More information

The Rocky Road Game. Sedimentary Rock. Igneous Rock. Start. Metamorphic Rock. Finish. Zone of Transportation. Weathering Way.

The Rocky Road Game. Sedimentary Rock. Igneous Rock. Start. Metamorphic Rock. Finish. Zone of Transportation. Weathering Way. Sedimentary Rock Deposition Depot Zone of Transportation Transported: Advance 3 Weathering Way The Rocky Road Game Uplift: Advance 5 Lithification Lane Crystallization Crossway Submerge Detour take the

More information

Supplemental Slides. Shore: Junction of Land & Water. Junction of Land & Water. Sea Level Variations. Shore vs. Coast. Sea Level Variations

Supplemental Slides. Shore: Junction of Land & Water. Junction of Land & Water. Sea Level Variations. Shore vs. Coast. Sea Level Variations Shore: Junction of Land & Water Supplemental Slides Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents Junction of Land & Water Features: Breaking waves,

More information

Shore: Junction of Land & Water. Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents

Shore: Junction of Land & Water. Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents Shore: Junction of Land & Water Supplemental Slides Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents Junction of Land & Water Features: Breaking waves,

More information

Pre-Lab Reading Questions ES202

Pre-Lab Reading Questions ES202 ES202 The are designed to encourage students to read lab material prior to attending class during any given week. Reading the weekly lab prior to attending class will result in better grade performance

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

1. Oceans. Example 2. oxygen.

1. Oceans. Example 2. oxygen. 1. Oceans a) Basic facts: There are five oceans on earth, making up about 72% of the planet s surface and holding 97% of the hydrosphere. Oceans supply the planet with most of its oxygen, play a vital

More information

Chapter 17. Ocean and Coastal Processes

Chapter 17. Ocean and Coastal Processes Chapter 17 Ocean and Coastal Processes Ocean Basins and Plates Ocean Basins Ocean Basins are profoundly different from the continents. Ocean crust is thin and dense and young. New ocean crust is generated

More information

Geology of the Hawaiian Islands

Geology of the Hawaiian Islands Geology of the Hawaiian Islands Class 12 19 February 2004 A B C D F 97 94 92 91 88 87 86 85 85 84 82 77 73 73 mean 66 64 60 69 60 57 51 29 Exam Scores Mean = 71 Median = 82/77 Any Questions? Sedimentary

More information

GEOLOGY MEDIA SUITE Chapter 5

GEOLOGY MEDIA SUITE Chapter 5 UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 5 Sedimentation Rocks Formed by Surface Processes 2010 W.H. Freeman and Company Mineralogy of sandstones Key Figure 5.12

More information

II Why study coastal landforms?

II Why study coastal landforms? COASTAL LANDFORMS (32) I Main topics A Why study coastal landforms? B Sediment budget and system response C Coastal landforms 3/26/15 GG454 1 II Why study coastal landforms? A Dynamic systems B Reflect

More information

Ocean and Coastal Processes. Ocean Basins. Chapter 20. Ocean Basins and Plates. Ocean Terms. Sea Arch Bay-mouth Bar Spit Tombolo Coast.

Ocean and Coastal Processes. Ocean Basins. Chapter 20. Ocean Basins and Plates. Ocean Terms. Sea Arch Bay-mouth Bar Spit Tombolo Coast. Chapter 20 Ocean Basins and Plates Ocean and Coastal Processes Tide Wave Height Length Period Base Refraction Tsunami Beach Sea stack Ocean Terms Sea Arch Bay-mouth Bar Spit Tombolo Coast Emergent Submergent

More information

Sedimentary Rocks. Rocks made of bits & pieces of other rocks.

Sedimentary Rocks. Rocks made of bits & pieces of other rocks. Sedimentary Rocks Rocks made of bits & pieces of other rocks. Sedimentary Rocks Igneous rocks are the most common rocks on Earth, but because most of them exist below the surface you might not have seen

More information

Weathering, Erosion and Deposition

Weathering, 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 information

Earth Science Lesson Plan Quarter 2, Week 10, Day 1

Earth Science Lesson Plan Quarter 2, Week 10, Day 1 Earth Science Lesson Plan Quarter 2, Week 10, Day 1 Outcomes for Today Standard Focus: PREPARE 1. Background knowledge necessary for today s reading. Beaches are created by the actions of waves, tides,

More information

Weathering of Rocks. Weathering - Breakdown of rocks into pieces (sediment) 2 main types of weathering to rocks

Weathering of Rocks. Weathering - Breakdown of rocks into pieces (sediment) 2 main types of weathering to rocks Weathering of Rocks Weathering - Breakdown of rocks into pieces (sediment) 2 main types of weathering to rocks Mechanical weathering requires physical forces to break rocks into smaller pieces. Chemical

More information

Engineering Geology ECIV 2204

Engineering Geology ECIV 2204 Engineering Geology ECIV 2204 Instructor : Dr. Jehad Hamad 2017-2016 Chapter (6) : Sedimentary Rocks Chapter 6: Sedimentary Rocks Chapter 6: Sedimentary Rocks Origin and nature of sedimentary rocks: Sedimentary

More information

Classify Rock (rock1)

Classify Rock (rock1) Name: Date: 1. Cleavage of a mineral is related to a mineral's A. chemical composition. B. streak color. C. luster. D. crystalline structure. 2. Which is not part of the definition of a mineral? A. naturally

More information

4. The map below shows a meandering stream. Points A, B, C, and D represent locations along the stream bottom.

4. 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 information

L.O: SLOWING STREAMS DEPOSIT (SORT) SEDIMENT HORIZONTALLY BY SIZE.

L.O: SLOWING STREAMS DEPOSIT (SORT) SEDIMENT HORIZONTALLY BY SIZE. L.O: SLOWING STREAMS DEPOSIT (SORT) SEDIMENT HORIZONTALLY BY SIZE. 1. Base your answer to the following question on the profile shown below, which shows the pattern of horizontal sorting produced at a

More information

The 1700/01/26 Cascadia subduction zone Earthquake and Tsunami

The 1700/01/26 Cascadia subduction zone Earthquake and Tsunami Jason R. Patton GEO 142 1/13/15 Abstract: Cascadia subduction zone earthquakes (CSZ) can generate strong ground shaking and deadly tsunamis. Geologists used sediment cores and stream bank exposures to

More information

What creates a coral reef? Why are corals able to form huge reefs?

What creates a coral reef? Why are corals able to form huge reefs? Marine ecosystems 5: Coral Reefs Unique features The foundation of the ecosystem is produced by living things Reef-building corals Similarities with tropical rain forests Richness and complexity 3-dimensional

More information

Aim and objectives Components of vulnerability National Coastal Vulnerability Assessment 2

Aim and objectives Components of vulnerability National Coastal Vulnerability Assessment 2 ASSESSING THE UTILITY OF GEOMORPHIC SENSITIVITY MAPPING ON THE ILLAWARRA COAST Pamela Abuodha, Christina Baker, Chris Sharples, Darren Skene and Colin Woodroffe Geoquest Research Centre, University of

More information

Sedimentary Environments Chapter 8

Sedimentary Environments Chapter 8 Sedimentary Environments Chapter 8 Does not contain complete lecture notes. To be used to help organize lecture notes and home/test studies. What is a sedimentary rock? Sedimentary rocks are products of

More information

1 Shoreline Landforms 2. 2 Emergent v. Submergent 2. 3 Wavecutting 3. 4 Planview 4. 5 Marine Terraces 5. 6 California 7. 7 Tombolos, Sea Stacks 8

1 Shoreline Landforms 2. 2 Emergent v. Submergent 2. 3 Wavecutting 3. 4 Planview 4. 5 Marine Terraces 5. 6 California 7. 7 Tombolos, Sea Stacks 8 Shorelines November 9, 2008 Contents 1 Shoreline Landforms 2 2 Emergent v. Submergent 2 3 Wavecutting 3 4 Planview 4 5 Marine Terraces 5 6 California 7 7 Tombolos, Sea Stacks 8 8 Active Processes 9 9 Emergence

More information

ESC102. Sedimentary Rocks. Our keys to the past. Monday, February 11, 13

ESC102. Sedimentary Rocks. Our keys to the past. Monday, February 11, 13 ESC102 Sedimentary Rocks Our keys to the past Sedimentary Rocks Sedimentary rocks are rocks that form through the accumulation of sediment and the process of lithification. Lithification occurs after deposition

More information

Forecast of Nearshore Wave Parameters Using MIKE-21 Spectral Wave Model

Forecast of Nearshore Wave Parameters Using MIKE-21 Spectral Wave Model Forecast of Nearshore Wave Parameters Using MIKE-21 Spectral Wave Model Felix Jose 1 and Gregory W. Stone 2 1 Coastal Studies Institute, Louisiana State University, Baton Rouge, LA 70803 2 Coastal Studies

More information

Sedimentary rocks. Sedimentary Rocks are produced from weathered debris of older rocks. Sedimentary rocks are produced by the following steps:

Sedimentary rocks. Sedimentary Rocks are produced from weathered debris of older rocks. Sedimentary rocks are produced by the following steps: Sedimentary rocks Most figures contained here are fro m Understand ing Earth Fourth Edition by F rank P ress, Raymond Sieve r, John Grotzinge r, and Thomas H. Jor dan Sedimentary Rocks are produced from

More information

Sedimentary Rocks Chapter 6

Sedimentary Rocks Chapter 6 Sedimentary Rocks Chapter 6 I. What is a sedimentary rock? A. Sedimentary rock 1) Rock made of detrital sediments (such as sand) or inorganic/organic chemical precipitates (such as calcite) 2) Detrital

More information

Sea Level Rise and the Scarborough Marsh Scarborough Land Trust Annual Meeting April 24, 2018

Sea Level Rise and the Scarborough Marsh Scarborough Land Trust Annual Meeting April 24, 2018 Sea Level Rise and the Scarborough Marsh Scarborough Land Trust Annual Meeting April 24, 2018 Peter A. Slovinsky, Marine Geologist Maine Geological Survey Funded by: 50% 40% Figure modified from Griggs,

More information

OFFSHORE SAND PROSPECTING IN HAWAII

OFFSHORE SAND PROSPECTING IN HAWAII OFFSHORE SAND PROSPECTING IN HAWAII James H. Barry Sea Engineering, Inc. Waimanalo, HI Honolulu, Hawaii Makai Research Pier, Waimanalo, Hawaii Santa Cruz and Santa Barbara, California www.seaengineering.com

More information

The Nature of Sedimentary Rocks

The Nature of Sedimentary Rocks The Nature of Sedimentary Rocks Sedimentary rocks are composed of: Fragments of other rocks Chemical precipitates Organic matter or biochemically produced materials The Nature of Sedimentary Rocks Sedimentary

More information

Sand. Sand is any eroded material (igneous, metamorphic or sedimentary) that has a grain size from 1/16 th to 2 millimeters in size.

Sand. Sand is any eroded material (igneous, metamorphic or sedimentary) that has a grain size from 1/16 th to 2 millimeters in size. Sedimentology 001 What is sedimentology? Sedimentology...encompasses the study of modern sediments such as sand [1], mud (silt) [2] andclay [3] and understanding the processes that deposit them.[4] It

More information

Teacher s Pack Key Stage 3 GEOGRAPHY

Teacher s Pack Key Stage 3 GEOGRAPHY Teacher s Pack Key Stage 3 GEOGRAPHY Geography Key Stage 3 Fieldwork Worksheet Rivers: 1. Is the water fresh or salty? (test its resistance or specific gravity) 2. Do you know where the water is coming

More information

Surface Water Short Study Guide

Surface Water Short Study Guide Name: Class: Date: Surface Water Short Study Guide Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The three ways in which a stream carries

More information

The Systems Approach. Alun Williams, ABPmer

The Systems Approach. Alun Williams, ABPmer The Systems Approach Alun Williams, ABPmer Overview What is A Systems Approach? Behavioural / Qualitative Modelling? System Definition / Mapping (Behavioural Statements Objective) What is a Systems Approach?

More information

Core Examples from Modern Estuarine Tidal Bars, Tillamook Bay, Oregon

Core Examples from Modern Estuarine Tidal Bars, Tillamook Bay, Oregon Core Examples from Modern Estuarine Tidal Bars, Tillamook Bay, Oregon Rares Bistran* University of Alberta, Edmonton, Alberta, Canada rares.bistran@ualberta.ca David Herbers, Murray Gingras, John-Paul

More information

Pratice Surface Processes Test

Pratice 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

Relatively little hard substrate occurs naturally in the

Relatively little hard substrate occurs naturally in the CHAPTER FIVE Rock Habitats Relatively little hard substrate occurs naturally in the estuary, owing mainly to the vast quantities of fine sediment that have been deposited by the rivers. Rock habitat is

More information

THE SETTLING OF MUD FLOCS IN THE DOLLARD ESTUARY, THE NETHERLANDS

THE SETTLING OF MUD FLOCS IN THE DOLLARD ESTUARY, THE NETHERLANDS THE SETTLING OF MUD FLOCS IN THE DOLLARD ESTUARY, THE NETHERLANDS SUMMARY Chapter 1 Introduction and literature review Morphological changes of estuarine channels and tidal flats depend on erosion, sediment

More information

Elkhorn Slough Marsh Stratigraphy

Elkhorn Slough Marsh Stratigraphy Elkhorn Slough Marsh Stratigraphy Prehistoric marsh extent & recent sediment accretion Elizabeth Burke Watson, Ph.D. U.S. Environmental Protection Agency Narragansett, RI Paleoecology: Reconstruction of

More information

To get you thinking Explain how these different layers of rock formed? Why are these layers different colors? Sedimentary Rocks

To get you thinking Explain how these different layers of rock formed? Why are these layers different colors? Sedimentary Rocks To get you thinking Explain how these different layers of rock formed? Why are these layers different colors? Sedimentary Rocks Bryce Canyon, Utah Badlands, South Dakota Weathering Whenever rock is exposed

More information

Sediments and. Sedimentary Rocks

Sediments and. Sedimentary Rocks Sediments and Sedimentary Rocks Bottom Line Sedimentary rocks form from particles accumulated in sedimentary layers Sedimentary layers can be formed by clastic or detrital particles (e.g., sand grains,

More information

CHAPTER 1 INTRODUCTION

CHAPTER 1 INTRODUCTION 1 CHAPTER 1 INTRODUCTION 1.1 GENERAL Washover sandsheets are often found in low-lying coastal embayment s (Sedgwick and Davis 2003). Washover deposition of marine sand is usually attributed to storm activity

More information

EROSION, DEPOSITION AND SEDIMENTARY ROCKS. Reading: Earth Science Tarbuck and Lutgens Chapter 5: pages Chapter 3: pages 52-54, 61-69

EROSION, DEPOSITION AND SEDIMENTARY ROCKS. Reading: Earth Science Tarbuck and Lutgens Chapter 5: pages Chapter 3: pages 52-54, 61-69 EROSION, DEPOSITION AND SEDIMENTARY ROCKS Reading: Earth Science Tarbuck and Lutgens Chapter 5: pages 124-133 Chapter 3: pages 52-54, 61-69 Base Level Resistant bed Resistant bed creates a local base level

More information

Australian Coastal Councils Conference

Australian Coastal Councils Conference Australian Coastal Councils Conference 11 March 2015 Estimating Future Coastal Inundation and Erosion Hazards Dr Andrew McCowan Dr Christine Lauchlan-Arrowsmith Warwick Bishop Background Victorian Future

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

4 Marine Biology Notes. Multi-cellular Primary Producers: Seaweeds and Plants

4 Marine Biology Notes. Multi-cellular Primary Producers: Seaweeds and Plants 4 Marine Biology Notes Multi-cellular Primary Producers: Seaweeds and Plants Marine Algae Marine algae are important primary producers (photosynthetic) These algae are called by a generic term seaweeds

More information

Depositional Environment

Depositional Environment Depositional Environment Sedimentary depositional environment describes the combination of physical, chemical and biological processes associated with the deposition of a particular type of sediment. Types

More information

9693 MARINE SCIENCE. Mark schemes should be read in conjunction with the question paper and the Principal Examiner Report for Teachers.

9693 MARINE SCIENCE. Mark schemes should be read in conjunction with the question paper and the Principal Examiner Report for Teachers. CAMBRIDGE INTERNATIONAL EXAMINATIONS GCE Advanced Subsidiary Level and GCE Advanced Level www.xtremepapers.com MARK SCHEME for the May/June 01 series 969 MARINE SCIENCE 969/01 Paper 1 (AS Structured Questions),

More information

Physical landscapes River landscapes in the UK

Physical landscapes River landscapes in the UK Physical landscapes River landscapes in the UK The shape of river valleys change s as rivers flow downstream - PROCESSES Erosion Abrasion or corrasion Attrition Hydraulic Action Solution or corrosion Deposition

More information

COASTAL DYNAMICS VIRTUAL FIELD TRIP, NORTHEAST FLORIDA. Joann Mossa Department of Geography University of Florida

COASTAL DYNAMICS VIRTUAL FIELD TRIP, NORTHEAST FLORIDA. Joann Mossa Department of Geography University of Florida COASTAL DYNAMICS VIRTUAL FIELD TRIP, NORTHEAST FLORIDA Joann Mossa Department of Geography University of Florida WHERE ARE WE GOING? In NE Florida (Flagler and St. Johns County, south of St. Augustine),

More information

Science Matters. Grade Six Earth Science. Weathering and Erosion

Science Matters. Grade Six Earth Science. Weathering and Erosion Science Matters Grade Six Earth Science Weathering and Erosion Written By Kim Castagna Jennifer Foster Meagan Callahan Tracy Schifferns Developed in Conjunction with K-12 Alliance/WestEd Table of Contents

More information

The Coast: Beaches and Shoreline Processes

The Coast: Beaches and Shoreline Processes 1 2 3 4 5 6 7 8 9 The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions.

More information

Sedimentary Rocks. Rocks made of bits & pieces of other rocks.

Sedimentary Rocks. Rocks made of bits & pieces of other rocks. Sedimentary Rocks Rocks made of bits & pieces of other rocks. Sedimentary Rocks Igneous rocks are the most common rocks on Earth, but because most of them exist below the surface you might not have seen

More information

Sedimentary Rocks. All sedimentary rocks begin to form when existing rocks are broken down into sediments Sediments are mainly weathered debris

Sedimentary Rocks. All sedimentary rocks begin to form when existing rocks are broken down into sediments Sediments are mainly weathered debris Rocks! Objectives Describe the major processes involved in the formation of sedimentary rock Distinguish between clastic sedimentary rocks and chemical sedimentary rocks Identify the features that are

More information

Sediment. Weathering: mechanical and chemical decomposition and disintegration of rock and minerals at the surface

Sediment. Weathering: mechanical and chemical decomposition and disintegration of rock and minerals at the surface Sediment Some basic terminology Weathering: mechanical and chemical decomposition and disintegration of rock and minerals at the surface Erosion: removal of weathered rock and minerals from one place to

More information

Read 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 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 information

The Coast: Beaches and Shoreline Processes Trujillo & Thurman, Chapter 10

The Coast: Beaches and Shoreline Processes Trujillo & Thurman, Chapter 10 The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions. Identify seasonal

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 Coastal Processes in the Lubec Embayment

Active Coastal Processes in the Lubec Embayment The Lubec Embayment Maine Geologic Facts and Localities August, 1998 Active Coastal Processes in the Lubec Embayment 44 49 50.51 N, 66 59 34.16 W Text by Joseph T. Kelley, Department of Agriculture, Conservation

More information

Winfried Siefert ; Volker Barthel**' and

Winfried Siefert ; Volker Barthel**' and CHAPTER 176 THE GERMAN "MORAN" PROJECT by Winfried Siefert ; Volker Barthel**' and Abstract The project "MORAN" (Morphological Analyses of the North- Sea-Coast) is an extensive program in order to try

More information

Earth Materials Unit: Sedimen ntary Rocks and Processes Maybe One Day Text: Chapters Five and Six Lab: Laboratorry Six Name

Earth Materials Unit: Sedimen ntary Rocks and Processes Maybe One Day Text: Chapters Five and Six Lab: Laboratorry Six Name Earth Materi ials Unit: Sedimentary Rocks and Proces sses Maybe One Day Text: Chapters Fivee and Six Lab: Laboratory Six Name Page 1 Sedimentary Rocks and Processes Purpose: To classify sedimentary rocks

More information