Supplementary Materials

SEA-FLOOR SPREADING. In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:-

SEA-FLOOR SPREADING In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:- Detailed bathymetric (depth) studies showed that there was an extensive submarine

Lecture 13. Hydrothermal Circulation

Lecture 13. Hydrothermal Circulation The discovery of hot springs on the ocean floor during the 1970s was one of the most exciting events in the history of oceanography. Although hydrothermal activity

Geochemistry & mineralogy of late-metamorphic shear zones:

Geochemistry & mineralogy of late-metamorphic shear zones: Disseminated gold in the Otago Schist, New Zealand Dave Craw Geology Department University of Otago Dunedin, NZ in collaboration with: D.J. MacKenzie,

Using SBSE for the study of organic compounds in submarine hydrothermal vents: from the research vessel to the lab

Using SBSE for the study of organic compounds in submarine hydrothermal vents: from the research vessel to the lab Cécile Konn, Sophie Chataing LGM, Ifremer, Brest 2 nd SBSE technical meeting, Paris, 11&12

Salinity distribution in the Oceans

Salinity distribution in the Oceans Average practical salinity of open ocean waters 34.72 http://eps.mcgill.ca/~courses/c542/ 1/58 Salinity distribution in the Oceans Factors that control seawater salinity:

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

Magmatic Eruptions and Iron Volatility in Deep-Sea Hydrothermal Fluids

GSA DATA REPOSITORY 2014101 Magmatic Eruptions and Iron Volatility in Deep-Sea Hydrothermal Fluids Authors: Nicholas J. Pester, Kang Ding and William E. Seyfried, Jr. This file contains the following Supplementary

The Lead 206/207 Dating Method

The Lead 206/207 Dating Method 1 U Pb Zircon Ages, Chemical Geology, Volume 211 (2004) Pages 87 109 2 Lead Isotope Planetary Profiling, Chemical Geology, Volume 233 (2006) Pages 1 45 3 U Pb Step-Leaching

Kasahara, H, Masuda, Ariyoshi. & K. Fujioka, southwestern mapping T. Gamo, Mariana Lost T. Ishii, M. volcanoes of the Island Arc: New swath- and geochemical studies of the extension of the Mariana active

Prospects and Status of Exploration for Polymetallic Sulphides. Georgy Cherkashov VNIIOkeangeologia St.Petersburg, RUSSIA

Prospects and Status of Exploration for Polymetallic Sulphides Georgy Cherkashov VNIIOkeangeologia St.Petersburg, RUSSIA Introduction Outline Hydrothermal processes and seafloor massive sulfides (SMS):

Destabilization of Carbon Dioxide Hydrates in the Ocean. Resherle Verna Department of Earth Science, University of Southern California

Verna 1 Destabilization of Carbon Dioxide Hydrates in the Ocean Resherle Verna Department of Earth Science, University of Southern California I. ABSTRACT This paper features the investigation of the change

Research Article Organic, Gas, and Element Geochemistry of Hydrothermal Fluids of the Newly Discovered Extensive Hydrothermal Area in

Hindawi Geofluids Volume 2018, Article ID 7692839, 25 pages https://doi.org/10.1155/2018/7692839 Research Article Organic, Gas, and Element Geochemistry of Hydrothermal Fluids of the Newly Discovered Extensive

Lecture 4 What Controls the Composition of Seawater

Lecture 4 What Controls the Composition of Seawater Seawater is salty! Why? What controls the composition of seawater? Do Chemical Equilibrium reactions control the composition of the Ocean? What is meant

4.1 Atomic structure and the periodic table. GCSE Chemistry

4.1 Atomic structure and the periodic table GCSE Chemistry All substances are made of atoms this is cannot be chemically broken down it is the smallest part of an element. Elements are made of only one

Deep-Sea and Sub-Seafloor Resources: A Polymetallic Sulphide and Co-Mn Crust Perspective. Stephen Roberts

Deep-Sea and Sub-Seafloor Resources: A Polymetallic Sulphide and Co-Mn Crust Perspective by Stephen Roberts The LRET Research Collegium Southampton, 16 July 7 September 2012 1 Deep-Sea and Sub-Seafloor

Sr Isotopes and REEs Geochemistry of Anhydrites from L Vent Black Smoker Chimney, East Pacific Rise 9ºN 10ºN

Journal of Earth Science, Vol. 26, No. 6, p. 920 928, December 2015 ISSN 1674-487X Printed in China DOI: 10.1007/s12583-015-0545-8 Sr Isotopes and REEs Geochemistry of Anhydrites from L Vent Black Smoker

IMPORTANT FACTS HYDROTHERMAL VENTS OCCUR WHERE HIGH TEMPERATURE WATER IS COMING INTO THE OCEANS. First discovered in 1977 by Bob Ballard.

HYDROTHERMAL VENTS IMPORTANT FACTS HYDROTHERMAL VENTS OCCUR WHERE HIGH TEMPERATURE WATER IS COMING INTO THE OCEANS. First discovered in 1977 by Bob Ballard. HOW THEY WORK * COLD OVERLYING SEAWATER PENETRATES

Liquid CO 2 venting on the seafloor: Yonaguni Knoll IV hydrothermal system, Okinawa Trough

GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L16607, doi:10.1029/2006gl026115, 2006 Liquid CO 2 venting on the seafloor: Yonaguni Knoll IV hydrothermal system, Okinawa Trough Uta Konno, 1 Urumu Tsunogai, 1 Fumiko

Fluid Chemistry Scenarios Anticipated for IDDP-2 to be Drilled in Reykjanes, Iceland

Proceedings World Geothermal Congress 21 Melbourne, Australia, 19-2 April 21 Fluid Chemistry Scenarios Anticipated for IDDP-2 to be Drilled in Reykjanes, Iceland Thráinn Fridriksson 1, Andri Stefánsson

Hydrothermal vents from the Azores

Hydrothermal vents from the Azores Ana Colaço Center of IMAR from University of Azores Departement of Oceanography and Fisheries 1 Hydrothermal vents are zones of fluid expulsion from the sea floor, normally

Hydrothermal Vent Challenge

2004 Ring of Fire Expedition Hydrothermal Vent Challenge FOCUS Chemistry of hydrothermal vents GRADE LEVEL 9-12 (Chemistry) FOCUS QUESTION What are common features of hydrothermal vent fluids, and how

Serpentinization, Abiogenic Methane, and Extremophilic Archaea within the Seafloor

Serpentinization, Abiogenic Methane, and Extremophilic Archaea within the Seafloor Michael J. Mottl Department of Oceanography NAI Winter School, Jan. 2005 Earth s mantle is 68% of its mass and 83% of

GSA Data Repository

GSA Data Repository 218145 Parolari et al., 218, A balancing act of crust creation and destruction along the western Mexican convergent margin: Geology, https://doi.org/1.113/g39972.1. 218145_Tables DR1-DR4.xls

Exploration for VMS Mineralization in Submarine Arcs

Regional Exploration Paper 121 Exploration for VMS Mineralization in Submarine Arcs 1. GNS Science, P.O. Box 30-368, Lower Hutt, New Zealand de Ronde, C.E.J. [1], Leybourne, M.I. [1] ABSTRACT The Kermadec

Hydrothermal Vents. "oases. of life." Evolution Physiology Biodiversity. Barbara Zimmermann, Kirstin Claußen, Ulrich Markmann

Hydrothermal Vents "oases of life." Evolution Physiology Biodiversity Barbara Zimmermann, Kirstin Claußen, Ulrich Markmann Hydrothermal vents are geysers on the seafloor. They continuously spew super-hot,

Biodiversity of Hydrothermal Vents at Brothers Volcano

Biodiversity of Hydrothermal Vents at Brothers Volcano Background One measure of biodiversity of an ecosystem is the species diversity, which is a combination of both species richness and species evenness.

Manganese concentration of hydrothermal plume at Pele s Pit, Loihi Seamount, Hawaii. Brian Min February 18 th, 2011

Manganese concentration of hydrothermal plume at Pele s Pit, Loihi Seamount, Hawaii Brian Min February 18 th, 2011 School of Oceanography, Box 357940, University of Washington, Seattle, Washington, 98195-7940

Lecture 6 - Determinants of Seawater Composition. Sets up electric dipole because O is more electronegative A o. Figure 3.

12.742 - Marine Chemistry Fall 2004 Lecture 6 - Determinants of Seawater Composition Prof. Scott Doney What is seawater? Water Dissolved inorganic salts (major ions) Trace species, organics, colloids,

Systems? Climate Systems. Earth Systems. Earth Interior Systems. Atmospheric/Biospheric Systems: Human Impact Hydrologic Cycle.

Chapter 15 Climate Systems Systems? What is a system? Geologic phenomena are complex. All processes are related to, and interact with, other processes. So it is useful to think of geologic processes as

Key role of continental margin sediments in the oceanic mass balance of Zn and Zn isotopes

Data Repository 2016062 Key role of continental margin sediments in the oceanic mass balance of Zn and Zn isotopes Little et al. Table DR1. Summary of data and data sources reported in Figure 1 Mean 1SD

Salinity. See Appendix 1 of textbook x10 3 = See Appendix 1 of textbook

Length Area Volume m m m foot = 0.305m yard = 0.91m square feet ~0.09m2 US pint ~ 0.47 L fl. oz. ~0.02 L Speed m/s mph Acceleration m/s mph/s Weight kg, gram pound ~0.45kg Temperature o o See Appendix

Search and Discovery Article #50999 (2014)** Posted August 18, Abstract

Oil Degradation in the Gullfaks Field (Norway): How Hydrogeochemical Modeling can Help to Decipher Organic- Inorganic Interactions Controlling CO 2 Fate and Behavior* Wolfgang van Berk 1, Yunjiao Fu 2,

Chapter 1. I- Fill the following table. Element symbol and the mass no. n p n n n e. number. II - Choose the correct answer for the following: Ca-40

Chapter 1 I- Fill the following table. Element symbol and the mass no. Ca-40 Ca 2+ -40 O-17 O 2- -16 C-12 C-13 Atomic number n p n n n e II - Choose the correct answer for the following: 1. Consider the

Experimental investigation of single carbon compounds under hydrothermal conditions

Geochimica et Cosmochimica Acta 70 (2006) 446 460 www.elsevier.com/locate/gca Experimental investigation of single carbon compounds under hydrothermal conditions Jeffrey S. Seewald a, *, Mikhail Yu. Zolotov

Active and fossil geothermal systems in Iceland

Active and fossil geothermal systems in Iceland Exploration for epithermal deposits Hjalti Franzson Iceland GeoSurvey Main points Geological framework Geological structures Geothermal systems Exploration

Supplementary Figure 1 Map of the study area Sample locations and main physiographic features of the study area. Contour interval is 200m (a) and 40m

Supplementary Figure 1 Map of the study area Sample locations and main physiographic features of the study area. Contour interval is 200m (a) and 40m (b). Dashed lines represent the two successive ridge

Metals in geothermal fluids and metal precipitations in surface pipelines in Iceland can these been utilized?

Metals in geothermal fluids and metal precipitations in surface pipelines in Iceland can these been utilized? Dr. Vigdís Hardardóttir, Iceland GeoSurvey - ÍSOR Msc. NordMin course Iceland Nov. 2016 Black

Jon Telling Dept. of Geology, University of Toronto.

Compound Specific Hydrogen and Carbon Isotopes as a Tool to Distinguish Abiogenic from Biogenic Hydrocarbons Implications for the Terrestrial Deep Biosphere and Astrobiology Jon Telling Dept. of Geology,

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION Supplementary Information for Survival of mussels in extremely acidic waters on a submarine volcano Verena Tunnicliffe *, Kimberley T.A. Davies, David A. Butterfield, Robert W.

6th Grade Science Sample Assessment Items S6E3c.

Composition 6th Grade Science Sample Assessment Items Ocean water differs from freshwater in that it has. A. a lower temperature B. a higher temperature C. a higher concentration of silicon dioxide D.

John Breier. CURRICULUM VITAE 28 August 2007 ADDRESS AND TELEPHONE

CURRICULUM VITAE 28 August 2007 John Breier ADDRESS AND TELEPHONE Woods Hole Oceanographic Institution Applied Ocean Physics & Engineering 266 Woods Hole Road Blake Building, Room 200 Woods Hole, MA, 02543

Earthquakes. Earthquakes are caused by a sudden release of energy

Earthquakes Earthquakes are caused by a sudden release of energy The amount of energy released determines the magnitude of the earthquake Seismic waves carry the energy away from its origin Fig. 18.1 Origin

Gas geochemical characteristics of hydrothermal plumes at the HAKUREI and JADE vent sites, the Izena Cauldron, Okinawa Trough

Geochemical Journal, Vol. 44, pp. 507 to 518, 2010 Gas geochemical characteristics of hydrothermal plumes at the HAKUREI and JADE vent sites, the Izena Cauldron, Okinawa Trough SHINSUKE KAWAGUCCI, 1 *

Geol. 656 Isotope Geochemistry

HYDROTHERMAL ACTIVITY, METAMORPHISM, AND ORE DEPOSITS II SULFUR ISOTOPE FRACTIONATION IN LOW-TEMPERATURE SYSTEMS 2 - At temperatures below about 400 C, sulfate (SO 4 ) species becomes the dominant form

The Sea Floor. Chapter 2

The Sea Floor Chapter 2 Geography of the Ocean Basins World ocean is the predominant feature on the Earth in total area Northern Hemisphere = 61% of the total area is ocean. Southern Hemisphere = about

Chemistry 31A Autumn 2004 Professors Chidsey & Zare Exam 4 Name: 9:00am 10:00am 2:15pm 3:15pm 7:00pm 8:00pm S02 OC103 Charles

Chemistry 31A Autumn 2004 Professors Chidsey & Zare Exam 4 Name: SUNetID: @stanford.edu Honor Code Observed: (Signature) 9:00am 10:00am 2:15pm 3:15pm 7:00pm 8:00pm S02 OC103 Charles S04 OC103 Charles S06

May 07- June 02 John McDonough: Ocean Exploration An Investigation of the Deep Coral Lophellia pertusa in the Northern Gulf of Mexico

ALVIN REPORTS 2006 May 07- June 02 John McDonough: Ocean Exploration An Investigation of the Deep Coral Lophellia pertusa in the Northern Gulf of Mexico Quantifying Elemental Fluxes and Fluid Origins at

OCN 201. Chemistry & Physics of the Ocean. (but no need to panic) foot = 0.305m yard = 0.91m. Length. Area m 2 square feet ~0.09m2

Chemistry & Physics of the Ocean OCN 201 (but no need to panic) Length m foot = 0.305m yard = 0.91m Area m 2 square feet ~0.09m2 Volume m 3 US pint ~ 0.47 L, L (liters) fl. oz. ~0.02 L Speed m/s mph Acceleration

predictive mineral discovery*cooperative Research Centre A legacy for mineral exploration science Mineral Systems Q3 Fluid reservoirs

Mineral Systems Q3 Fluid reservoirs 1 Key Parameter Mineral System Exploration is reflected in scale-dependent translation A. Gradient in hydraulic potential B. Permeability C. Solubility sensitivity to

Reporting Category 1: Matter and Energy

Name: Science Teacher: Reporting Category 1: Matter and Energy Atoms Fill in the missing information to summarize what you know about atomic structure. Name of Subatomic Particle Location within the Atom

Paso Robles Groundwater Basin: Effects of Geothermal Waters on Water Quality and Availability

Paso Robles Groundwater Basin: Effects of Geothermal Waters on Water Quality and Availability Jim Rytuba and Daniel Goldstein U.S. Geological Survey, Menlo Park, CA Paso Robles Intake from Lake Nacimiento

Salinity. foot = 0.305m yard = 0.91m. Length. Area m 2 square feet ~0.09m2. Volume m 3 US pint ~ 0.47 L fl. oz. ~0.02 L.

Length m foot = 0.305m yard = 0.91m Area m 2 square feet ~0.09m2 Volume m 3 US pint ~ 0.47 L, L (liters) fl. oz. ~0.02 L Speed m/s mph Acceleration m/s 2 mph/s Weight kg, gram pound ~0.45kg Temperature

Data Repository item Beard et al. 1. Data Repository Supplementary Information

Data Repository item 2003088 Beard et al. 1 Data Repository Supplementary Information Analytical methods: Iron isotope compositions were measured using a Micromass IsoProbe on 400 to 300ppb Fe solutions

Isotopic tracers in Oceanography

Isotopic tracers in Oceanography Isotopic tracers in oceanography Pathways of different trace metals from their sources to their sinks M. Frank: Reviews of Geophysics, vol. 40 DOI: 10.1029/2000RG000094

Submarine Hydrothermal Mineralisations and Fluids off the Lesser Antilles Island Arc Initial Results from the CARIBFLUX Cruise SO 154

18 InterRidge ews International Research: Island arc/bab Submarine Hydrothermal Mineralisations and Fluids off the Lesser Antilles Island Arc Initial Results from the CARIBFLUX Cruise SO 154 P. Halbach

Week 3 Intro to Hydrothermal Activity and Event Plumes (aka Megaplumes) from Submarine Eruptions

Week 3 Intro to Hydrothermal Activity and Event Plumes (aka Megaplumes) from Submarine Eruptions Hydrothermal Processes overview General comments vent types: Focused flow, diffuse flow chronic plumes over

Fall 2016 Due: 10:30 a.m., Tuesday, September 13

Geol 330_634 Problem Set #1_Key Fall 2016 Due: 10:30 a.m., Tuesday, September 13 1. Why is the surface circulation in the central North Pacific dominated by a central gyre with clockwise circulation? (5)

Chapter 2: Plate Tectonics: A Unifying Theory

Chapter 2: Plate Tectonics: A Unifying Theory Chapter Outline 2.1 Introduction 2.2 Early Ideas About Continental Drift 2.3 What Is the Evidence for Continental Drift? 2.4 Features of the Seafloor 2.5 Earth

WERE FE(II) OXIDIZING PHOTOAUTOTROPHS INVOLVED IN THE DEPOSITION OF PRECAMBRIAN BANDED IRON

19 1. Introduction WERE FE(II) OXIDIZING PHOTOAUTOTROPHS INVOLVED IN THE DEPOSITION OF PRECAMBRIAN BANDED IRON FORMATIONS? Banded Iron Formations (BIFs) are ancient sedimentary rocks characterized by laminations

Atomic structure. The subatomic particles. - a small, but relatively massive particle that carres an overall unit POSITIVE CHARGE

35 Atomic structure - Until the early 20th century, chemists considered atoms to be indivisible particles. - The discovery of SUBATOMIC PARTICLES changed the way we view atoms! PROTON NEUTRON ELECTRON

Atomic terms. Example: Helium has an atomic number of 2. Every helium atom has two protons in its nucleus.

Atomic terms - ATOMIC NUMBER: The number of protons in the atomic nucleus. Each ELEMENT has the SAME NUMBER OF PROTONS in every nucleus. In neutral atoms, the number of ELECTRONS is also equal to the atomic

CERD STATE OF KNOWLEDGE OF THE GEOTHERMAL PROVINCES OF REPUBLIC OF DJIBOUTI. ARGEO-C1 Conference Addis-Ababa, Ethiopia, November 2006

STATE OF KNOWLEDGE OF THE GEOTHERMAL PROVINCES OF REPUBLIC OF DJIBOUTI ARGEO-C1 Conference Addis-Ababa, Ethiopia, 24-29 November 2006 JALLUDIN Mohamed Djibouti, GEOTHERMAL EXPLORATIONS IN DJIBOUTI FIRST

Electronic Appendix A: Supplementary material to accompany the manuscript, Fe 3+ / Fe in Mariana Arc basalts and primary fo 2.

Electronic Appendix A: Supplementary material to accompany the manuscript, Fe 3+ / Fe in Mariana Arc basalts and primary fo 2. Screening for olivine interference in Fe-µ-XANES spectra When collecting Fe-µ-XANES

Long-term interaction between mid-ocean ridges and mantle plumes

SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2437 Long-term interaction between mid-ocean ridges and mantle plumes Whittaker, J. M., Afonso, J. C., Masterton, S., Müller, R. D., Wessel, P., Williams S. E.

Geotherms. Reading: Fowler Ch 7. Equilibrium geotherms One layer model

Geotherms Reading: Fowler Ch 7 Equilibrium geotherms One layer model (a) Standard model: k = 2.5 W m -1 C -1 A = 1.25 x 10-6 W m -3 Q moho = 21 x 10-3 W m -2 shallow T-gradient: 30 C km -1 deep T-gradient:

Mantle geochemistry: How geochemists see the deep Earth

Geochemistry: Overview: the geochemist's Earth (reservoirs, budgets and processes) Mantle geochemistry: How geochemists see the deep Earth Don DePaolo/Stan Hart CIDER - KITP Summer School Lecture #1, July

Periodic Table. - Mendeleev was able to predict the properties of previously unknown elements using his "periodic law" Modern periodic table

74 Periodic Table - Mendeleev (1869): --- When atoms are arranged in order of their atomic weight, some of their chemical and physical properties repeat at regular intervals (periods) --- Some of the physical

Chemical Reactions BASICS

Chemical Reactions BASICS There are 5 simple reactions in this chemistry class (but more are coming later in the year). They are synthesis, decomposition, single replacement, double replacement, and combustion.

General Oceanography Geology 105 Expedition 14 Dive & Discover Explorations of the Seafloor See Due Date in Greensheet or in Module Area of Canvas

General Oceanography Name Geology 105 Expedition 14 Dive & Discover Explorations of the Seafloor See Due Date in Greensheet or in Module Area of Canvas Expedition Objective: In this expedition, we will

Lecture 5. Introduction to Stable Isotopes

Lecture 5 Introduction to Stable Isotopes Stable Isotope Geochemistry Primarily concerned with the isotope ratios of H, C, N, O, and S Si and B often included and new instrumentation has opened up others

INSTRUCTIONS: CHEM Exam I. September 13, 1994 Lab Section

CHEM 1314.05 Exam I John I. Gelder September 13, 1994 Name TA's Name Lab Section Please sign your name below to give permission to post, by the last 4 digits of your student I.D. number, your course scores

Hydrothermal activity in the Northwest Lau Backarc Basin: Evidence from water column measurements

Article Volume 13, Number 1 31 May 2012 Q0AF04, doi:10.1029/2011gc003891 ISSN: 1525-2027 Hydrothermal activity in the Northwest Lau Backarc Basin: Evidence from water column measurements J. E. Lupton NOAA

1. Introduction 2. Ocean circulation a) Temperature, salinity, density b) Thermohaline circulation c) Wind-driven surface currents d) Circulation and

1. Introduction 2. Ocean circulation a) Temperature, salinity, density b) Thermohaline circulation c) Wind-driven surface currents d) Circulation and climate change e) Oceanic water residence times 3.

Week 7 Submarine Pyroclastic Activity (there was no lecture for week 6)

Week 7 Submarine Pyroclastic Activity (there was no lecture for week 6) Note: some of these slides were provided by Dave Clague, MBARI Two topics: fluidal clasts and bubble wall fragments internal water

Hydrothermal Chemistry/ Reverse Weathering. Marine Chemistry Seminar

Hydrothermal Chemistry/ Reverse Weathering Marine Chemistry Seminar 1974 Drever, The Sea Chapter 10:The Magnesium Problem 1979 Edmonds et al., Ridge Crest Hydrothermal Activity and the Balances of Major

ORGANIC SPECIES IN GEOTHERMAL WATERS IN LIGHT OF FLUID INCLUSION GAS ANALYSES

PROCEEDINGS, Twenty-Eighth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 27-29, 2003 SGP-TR-173 ORGANIC SPECIES IN GEOTHERMAL WATERS IN LIGHT OF FLUID

Image courtesy Lau ISS Scientists. Donna Blackman, current chair of the R2K Steering Committee Scripps Institution of Oceanography

Image courtesy Lau ISS Scientists Donna Blackman, current chair of the R2K Steering Committee Scripps Institution of Oceanography 1 meter Endeavour hydrothermal vent chimneys, Juan de Fuca Ridge An integrated,

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/

Geologic Resources. Geologic Resources and Society. Geologic Resources and Society

Geologic Resources Our entire society rests upon - and is dependent upon - our water, our land, our forests, and our minerals. How we use these resources influences our health, security, economy, and well-being.

Reporting Category 1: Matter and Energy

Name: Science Teacher: Reporting Category 1: Matter and Energy Atoms 8.5A Fill in the missing information to summarize what you know about atomic structure. Name of Subatomic Particle Location within the

GEOCHEMISTRY OF RWENZORI HOT SPRINGS. Vincent Kato Department of Geological Survey and Mines, Entebbe, Uganda

GEOCHEMISTRY OF RWENZORI HOT SPRINGS Vincent Kato Department of Geological Survey and Mines, Entebbe, Uganda RWENZORI Length of 115Km Width of central dome 48 64 km Highest peak >5105m SnowyMountain Lakes

Periodic Table. Modern periodic table

41 Periodic Table - Mendeleev (1869): --- When atoms are arranged in order of their atomic weight, some of their chemical and physical properties repeat at regular intervals (periods) --- Some of the physical

A Si-Cl geothermobarometer for the reaction zone of high-temperature, basaltic-hosted mid-ocean ridge hydrothermal systems

A Si-Cl geothermobarometer for the reaction zone of high-temperature, basaltic-hosted mid-ocean ridge hydrothermal systems Fabrice Fontaine, William Wilcock, Dionysis Foustoukos, David Butterfield To cite

02/05/09 Last 4 Digits of USC ID: Dr. Jessica Parr

Chemistry 05 B First Letter of PLEASE PRINT YOUR NAME IN BLOCK LETTERS Exam last Name Name: 02/05/09 Last 4 Digits of USC ID: Dr. Jessica Parr Lab TA s Name: Question Points Score Grader 2 2 9 3 9 4 2

Unit 5 Chemical Reactions Notes. Introduction: Chemical substances have physical and chemical properties

Unit 5 Chemical Reactions Notes Introduction: Chemical substances have physical and chemical properties Physical Properties 2 Types of Physical Properties Extensive Physical Properties Intensive Physical

CERD GEOTHERMAL EXPLORATIONS AND RESULTS IN THE REPUBLIC OF DJIBOUTI. Short Course Naivasha, Kenya, November 2006

GEOTHERMAL EXPLORATIONS AND RESULTS IN THE REPUBLIC OF DJIBOUTI Short Course Naivasha, Kenya, 11-22 November 2006 JALLUDIN Mohamed Djibouti, CERD PRESENTATION PLAN General geological and hydrothermal activity

Geologic Evolution of Latin America. Plate Tectonics: General Concepts & Applications to Latin America

Geologic Evolution of Latin America Plate Tectonics: General Concepts & Applications to Latin America Structure of Earth: 3 major divisions of Core, Mantle, and Crust Upper mantle differs in the way that

Horizontal rows are called periods. There are seven periods on the periodic chart.

Chemistry Lecture #29: Sections of the Periodic Chart The periodic chart is divided into many sections. You need to memorize the location and names of the sections. Horizontal rows are called periods.

OCN 201 Fall nd mid term Section 1

Name: Class: _ Date: _ OCN 201 Fall 2013 2nd mid term Section 1 True/False Indicate whether the statement is true or false. 1. The hydrothermal vent sites at Loihi have lots of animals around them. 2.

Three (3) (Qatar only) The expected learning outcome is that the student will be able to:

Course Information for 2014-2015 COURSE NUMBER: COURSE TITLE: CH1120 Chemistry COURSE DESCRIPTION: This in an introductory course designed to give students knowledge and understanding of the fundamental

NUCLEAR MODEL. Electron cloud. Electron cloud. Nucleus. Nucleus

37 NUCLEAR MODEL - Atoms are mostly empty space - NUCLEUS, at the center of the atom, contains protons and neutrons. This accounts for almost all the mass of an atom - Electrons are located in a diffuse

Atomic weight: This is a decimal number, but for radioactive elements it is replaced with a number in parenthesis.

47 Blocks on the periodic table 11 Sodium 22.99 Atomic number: This is always a whole number. The periodic table is arranged by atomic number! Element symbol: A one or two letter abbreviation for the name

- Dalton's theory sets LIMITS on what can be done with chemistry. For example:

34 - Dalton's theory sets LIMITS on what can be done with chemistry. For example: Chemistry can't convert lead (an element) into gold (another element). Sorry, alchemists! You can't have a compound form

14. TEMPERATURE AND SALINITY OF FLUID INCLUSIONS IN ANHYDRITE AS INDICATORS OF SEAWATER ENTRAINMENT AND HEATING IN THE TAG ACTIVE MOUND 1

Herzig, P.M., Humphris, S.E., Miller, D.J., and Zierenberg, R.A. (Eds.), 998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 8. TEMPERATURE AD SALIITY OF FLUID ICLUSIOS I AHYDRITE AS

Last 4 Digits of USC ID:

Chemistry 05 B Practice Exam Dr. Jessica Parr First Letter of last Name PLEASE PRINT YOUR NAME IN BLOCK LETTERS Name: Last 4 Digits of USC ID: Lab TA s Name: Question Points Score Grader 8 2 4 3 9 4 0

TRACE ELEMENT ANALYSIS OF DIAMOND BY LAM ICPMS: STANDARDISATION, RESULTS AND DIRECTIONS

TRACE ELEMENT ANALYSIS OF DIAMOND BY LAM ICPMS: STANDARDISATION, RESULTS AND DIRECTIONS W.L. Griffin 1, 3, Sonal Rege 1, Rondi M. Davies 1, 2, Simon Jackson 1, Suzanne Y. O Reilly 1 1.ARC National Key

Periodic Table. Modern periodic table

41 Periodic Table - Mendeleev (1869): --- When atoms are arranged in order of their atomic weight, some of their chemical and physical properties repeat at regular intervals (periods) --- Some of the physical

Introduction to Earth s s Spheres The Benchmark

Introduction to Earth s s Spheres The Benchmark Volcanism Volcanic eruptions Effusive: lavas (e.g., Kilauea) Volcanism Volcanic eruptions Explosive: pyroclastic rocks (e.g., Krakatau) Factors Governing

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

Evidence of a recent input of magmatic gases into the quiescent volcanic edifice of Panarea, Aeolian Islands, Italy

GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L07619, doi:10.1029/2003gl019359, 2004 Evidence of a recent input of magmatic gases into the quiescent volcanic edifice of Panarea, Aeolian Islands, Italy S. Caliro,