How To Map A Lake In The North Of The Holland (Fiji)
|
|
|
- Baldric Fleming
- 5 years ago
- Views:
Transcription
1 1. Hydrogelogical mapping Jiri Sima
2 Aim of HG map Groundwater and rocks qualitative permeability and quantitative potential of rock units aquifers / aquitards / aquiclides Water points (spatial distribution and type) Supporting information (surface water network and divide, gw flow direction, river discharge, etc.)
3 Stakeholders The map, database and Explanations are addressed to: hydrogeologists, geochemists, balneologists, and balneo-technicians, whose study and exploit mineral water. all geologists, geographers and university students dealing with mineral waters, as well as to technological public interested in this natural heritage. informed publik
4 History 1940 various scale and purpose 1959 Commission for Hg. Maps (IAH) 1961 Helsinki (IAHS) exhibition 200 (IAH) survey of map techniques 1963 UNESCO /Anon draft legend 1970 UNESCO /Anon new legend 1974 UNESCO /Anon legend for geohydrochemical maps (Anon 1975) 1995 IAH /Struckmaier hydrogeological map
5 Concept From geology-oriented map to visualization of groundwater related features map Basic types of hydrogeological maps: 1. Hydrogeological regional mapping project (nation basic maps map sheets/ basins) 2. Thematic synthesis of existing data and reports to answer specific question water management - protection, pollution 3. Parametric maps baseflow, aquifer thickness, T, S
6 EARTH SCIENCE Geoscience Water science HYDROGEOLOGICAL MAP Geological map Hydrological map Topographical maps
7 Edition of hydrogeological map geological survey National edition of basic hydrogeological maps 1 : Compulsory guidelines - methodology Trained manpower Vehicle (tool) GIS
8 General elements Basic hydrogeological map Guidelines for compilation and publishing - compulsory procedure (National) water point database standardized legend explanatory notes - meteorological - hydrological - hydrogeological
9 Compulsory guidelines General principles for compilation and publishing (1 : ) General legend to hydrogeological map Contents of explanatory note (Provided by editor to sheet author/project manager/chief compiler)
10 General principles of Guidelines Validity of guidelines / basic provisions Primary documentation of the basic hydrogeological map Content of the hydrogeological map (layout and legend) Explanatory notes to the basic hydrogeological map
11 Integral parts of hydrogeological map Hydrogeological map Map sheet Explanatory notes Primary documentation to map and explanatory notes
12 Hydrogeological map Compulsory data Original map Legend Aquifer scheme (Cross-section Authors scheme) Sheets scheme Basin scheme Explanatory note Primary data Voluntary data Water quality data (hydrochemical map) Geophysical exploration Physiography Rainfall, temperature Regional aquifers Soil cover Quaternary cover
13 Layout of map sheet Sheet s. Basin s. Aquifer scheme Main map sheet Legend Authors (Cross-section if available)
14 General legend to map extent of aquifers and their types, and lithology with tectonic features basic structural and topographical settings all-important hydrogeological features (natural, man made) water quality, thermal water, and mineral water provinces
15 Aquifer system color The basic hydrogeological map is compiled as color maps Qualitative type of permeability (porous, fissured, karst, formation with low or without permeability - gw resources) Quantification of (amount) permeability Yield of water points (specific yield of well) transmissivity
16 Type of permeability Aquifer Color Rock example Porous Blue Alluvial Fissured Green Sandstone/basalt Fissured/karstic Green (dark) Limestone Basement Brown-red Granite/gneiss Aquiclude Brown Marlstone Aquitard Brown (dark) Claystone Mixed Blue/green strips Volcanic/sedimentary
17 Quantification of permeability Aquifer class T (m 2 /d) q (l/sm) Yield (l/s) Extra high More 25 High Moderate Low Extra low Neglegible /seepage Less 0.005
18 Quantification volcanic Rift Number of data Max Min Median Average
19 Permeability k (m/s) gravel - sand xloess silt -clay -x lava - basalt x limestone x snadstone x
20 Background information Simplified topography dark gray (60% black): towns, names, international and administrative boundaries Drainage blue: stream or rivers Grids or lines of longitude and latitude black Additional information: inset maps, explanatory notes (separate better)
21 Groundwater and rocks 1 Intergranular permeability - blue Extensive (>100 Km 2) and highly productive T = m 2 /d, q = l/sm, Q = l/s productive aquifers (dark blue) Local or discontinues highly productive aquifers, or extensive but only moderately productive aquifers (T = m 2 /d, q = l/s.m, with spring and well yield Q = l/s) (light blue)
22 Groundwater and rocks 2 Fissured (karst) aquifers - green Extensive (>100 Km 2) and highly productive T = m 2 /d, q = l/sm, Q = l/s productive aquifers (dark green) Local or discontinues highly productive aquifers, or extensive but only moderately productive aquifers (T = m 2 /d, q = l/s.m, with spring and well yield Q = l/s) (light green)
23 Groundwater and rocks 3 Basement rcks forming aquifers with local and limited groundwater resources brownred (T = m 2 /d, q = l/s.m, with spring and well yield Q = l/s).
24 Groundwater and rocks 4 Rocks with fissured porosity and with essentially no groundwater resources - brown Strata (sediments) with limited groundwater resources - light brown for T = 1m 2 /d, q = 0.01 l/sm, Q = l/s Strata with essentially no groundwater resources - dark brown for T = 0.1m 2 /d, q = l/sm, Q = 0.05
25 Groundwater and rocks 5 Covered / confined aquifers Where there is an extensive aquifer immediately underlying a thin impermeable cover, the appropriate aquifer color should be used crossed by brown stripes ( 1 mm wide and 3 mm separation) - Adigrad sandstone Humara area
26 Lithology Ornament in gray The orientation of the ornament indicates the type of bedding Horizontal = unfolded, horizontal of gently inclined strata (less that 20 O ) Vertical = folded strata
27 Representation of detailed data 1 Violet: groundwater and springs Orange: physical and chemical characteristics of groundwater quality and temperature Blue: surface water and karst hydrography Red: man-made features and alterations to the natural groundwater regime
28 Representation of detailed data 2 Dark green: horizon contours (isopachytes) and limits of certain features Black: geological information (fault, volcanic cone)
29 Hydrogeological map (AA) Shallow wells
30 Content of explanatory note 1. Basic characteristic of the area 2. Selected physical and geographical settings 3. Geological settings 4. Hydrogeological settings (aquifer system definition) 5. Hydrochemistry (of natural waters) 6. Natural resources of the area Annexes (WP inventory, chemical analyses, well logs)
31 Annexes Water point inventory (bore holes, dug wells, springs, water holes, rivers) Chemistry (results of chemical analysis - used for compilation of hydrochemical map and assessment of water quality) Well logs (essence of drilling reports information for next drilling) - same color and oranaments used in map for geology
32 Well log
33 Ignimbrite - mixed aquifers
34 Artesian mixed aquifer
35 Conclusions Systematical use of digital data, including GIS - Accelerate the process - More flexibility in data analysis - Easy to update - Presentation an any time (always actual) - More universal - can serve to more (various) users - Posibility of internet presentation
36 Recommendations Prepare methodology adopt international everybody be able to understand Legend to hydrogeological map documenting all map features / colors Contents to explanatory notes Develop, update, publish water database Use appropriate tools for your work
The International Hydrogeological Map of Europe ( IHME ) at the scale of 1:1.5 Million
The International Hydrogeological Map of Europe ( IHME ) at the scale of 1:1.5 Million - A coherent hydrogeological map for greater Europe and a model for the Rest of the World Historical Background State
WILLOCHRA BASIN GROUNDWATER STATUS REPORT 2009-10
WILLOCHRA BASIN GROUNDWATER STATUS REPORT 2009-10 SUMMARY 2009-10 The Willochra Basin is situated in the southern Flinders Ranges in the Mid-North of South Australia, approximately 50 km east of Port Augusta
APPLICATION OF GEOSPATIAL TECHNOLOGIES FOR SUSTAINABLE ENVIRONMENTAL MANAGEMENT
APPLICATION OF GEOSPATIAL TECHNOLOGIES FOR SUSTAINABLE NATURAL RESOURCES AND ENVIRONMENTAL MANAGEMENT IN MALAYSIA By James Dawos Mamit, Ph.D. Deputy Minister Ministry of Natural Resources and Environment,
A GIS BASED GROUNDWATER MANAGEMENT TOOL FOR LONG TERM MINERAL PLANNING
A GIS BASED GROUNDWATER MANAGEMENT TOOL FOR LONG TERM MINERAL PLANNING Mauro Prado, Hydrogeologist - SRK Consulting, Perth, Australia Richard Connelly, Principal Hydrogeologist - SRK UK Ltd, Cardiff, United
1.72, Groundwater Hydrology Prof. Charles Harvey Lecture Packet #2: Aquifers, Porosity, and Darcy s Law. Lake (Exposed Water Table)
1.72, Groundwater Hydrology Prof. Charles Harvey Lecture Packet #2: Aquifers, Porosity, and Darcy s Law Precipitation Infiltration Lake (Exposed Water Table) River Water table Saturated zone - Aquifer
Review of Groundwater Vulnerability Assessment Methods Unsaturated Zone. Dept. of Earth Sciences University of the Western Cape
Review of Groundwater Vulnerability Assessment Methods Unsaturated Zone Dept. of Earth Sciences University of the Western Cape Background Sililo et al. (2001) Groundwater contamination depends on: Intrinsic
Hydrogeological characteristics of Deccan trap formations of India
Hard Rock Hydrosysteins (Proceedings of Rabat Symposium S2, May 1997). IAHS Publ. no. 241, 1997 75 Hydrogeological characteristics of Deccan trap formations of India B. B. S. SINGHAL Department of Earth
NUMERICAL ANALYSIS OF SEEPAGE THROUGH EMBANKMENT DAMS (CASE STUDY: KOCHARY DAM, GOLPAYEGAN)
NUMERICAL ANALYSIS OF SEEPAGE THROUGH EMBANKMENT DAMS (CASE STUDY: KOCHARY DAM, GOLPAYEGAN) *Reza Naghmehkhan Dahande 1 and Ahmad Taheri 2 1 Department of Civil Engineering-Water Management, Islamic Azad
Principles of groundwater flow
Principles of groundwater flow Hydraulic head is the elevation to which water will naturally rise in a well (a.k.a. static level). Any well that is not being pumped will do for this, but a well that is
REPORT OF WORK GUIDELINES
REPORT OF WORK GUIDELINES The following guidelines apply to a report of work submitted under section 56(1) of the Mining Act (http://laws.gnb.ca/en/showdoc/cs/m-14.1). 1 (1) A report of work shall be submitted
Groundwater Training Course SOPAC, April 2005. Electromagnetic (EM) Induction method for Groundwater Investigations
Groundwater Training Course SOPAC, April 2005 Electromagnetic (EM) Induction method for Groundwater Investigations Electromagnetic (EM) Induction Method Basic principle: An AC electric current is applied
How To Create A 3D Model Of The Phanerozoic Succession In Southern Manitoba
3D GEOLOGICAL MAPPING IN MANITOBA MOVING FORWARD Greg Keller ([email protected]), Gaywood Matile, Manitoba Geological Survey (RET), Canada Harvey Thorleifson, Minnesota Geological Survey, United States
Dip is the vertical angle perpendicular to strike between the imaginary horizontal plane and the inclined planar geological feature.
Geological Visualization Tools and Structural Geology Geologists use several visualization tools to understand rock outcrop relationships, regional patterns and subsurface geology in 3D and 4D. Geological
EXPLAINING GROUNDWATER AND WATER WELLS
EXPLAINING GROUNDWATER AND WATER WELLS This document aims to provide a non-technical description of groundwater: how it occurs, how it moves underground, and the basic principles behind constructing and
Ground Water in the Piedmont and Blue Ridge Provinces of North Carolina
Ground Water in the Piedmont and Blue Ridge Provinces of North Carolina Prepared by: R.L. Huffman Extension Agricultural Engineering Specialist Published by: North Carolina Cooperative Extension Service
Deep Geothermal energy and groundwater in
Deep Geothermal energy and groundwater in the UK Jon Busby Deep Geothermal energy and groundwater in the UK Outline 1. UK geothermal 2. Deep saline aquifers 3. Engineered geothermal systems 4. Fractured
Explanatory notes to the Geological Base Map of the Czech Republic at 1: 25 000 scale
Pavel Hanžl et al. Explanatory notes to the Geological Base Map of the Czech Republic at 1: 25 000 scale czech geological survey Explanatory notes to the Geological Base Map of the Czech Republic at 1:25
Vulnerability Assessment
Vulnerability Assessment VULNERABILITY As used in this report, vulnerability refers to the sensitivity of groundwater to contamination, and is determined by intrinsic characteristics of the aquifer. It
FROM REGIONAL MAPS TO THE EUROPEAN SCALE: THE INSPIRE-CHALLENGE FOR THE EXAMPLE OF HYDROGEOLOGY
FROM REGIONAL MAPS TO THE EUROPEAN SCALE: THE INSPIRE-CHALLENGE FOR THE EXAMPLE OF HYDROGEOLOGY Bernhard Wagner Bavarian Environment Agency Geological Survey Introduction The INSPIRE-challenge for geological
LABORATORY TWO GEOLOGIC STRUCTURES
EARTH AND ENVIRONMENT THROUGH TIME LABORATORY- EES 1005 LABORATORY TWO GEOLOGIC STRUCTURES Introduction Structural geology is the study of the ways in which rocks or sediments are arranged and deformed
APPLICATION OF THE GEO-EMR METHOD IN HYDROGEOPHYSICS
NOVITOVI ALEKSANDAR 1, ŠESTAK ALEKSANDAR 1 APPLICATION OF THE GEO-EMR METHOD IN HYDROGEOPHYSICS During the recent decade, several new geophysical techniques have been introduced for mapping subsurface
RESERVOIR GEOSCIENCE AND ENGINEERING
RESERVOIR GEOSCIENCE AND ENGINEERING APPLIED GRADUATE STUDIES at IFP School from September to December RGE01 Fundamentals of Geoscience I Introduction to Petroleum Geosciences, Sedimentology RGE02 Fundamentals
Numerical Modelling of Water Flow (Seepage) in the Karun 4 Dam and Abutments (Steady State)
Numerical Modelling of Water Flow (Seepage) in the Karun 4 Dam and Abutments (Steady State) Mohammad Hosseiny Sohi 03 November 2015 Contents: Objectives Karun River & Karun 4 Dam in Iran Geology of dam
Lars-Göran Gustafsson, DHI Water and Environment, Box 3287, S-350 53 Växjö, Sweden
Alternative Drainage Schemes for Reduction of Inflow/Infiltration - Prediction and Follow-Up of Effects with the Aid of an Integrated Sewer/Aquifer Model Introduction Lars-Göran Gustafsson, DHI Water and
GeoEnergy a national shallow geothermal research project
European Geothermal Congress 2013 Pisa, Italy, 3 7 June 2013 GeoEnergy a national shallow geothermal research project Claus Ditlefsen 1, Thomas Vangkilde-Pedersen 1, Inga Sørensen 2, Henrik Bjørn 2, Anker
MO2GEO: An OpenSource software approach for geological modelling
MO2GEO: An OpenSource software approach for geological modelling Wolfgang GOSSEL 1 1 Dept. Hydrogeology and Environmental Geology, Institute for Geosciences, Martin Luther University Halle, Germany, [email protected]
Earth Science & Environmental Science SOL
Earth Science & Environmental Science SOL THE SOL FOR GRADE 6 The Virginia Science SOL for Grades K 6 are organized according to a set of strands, with the SOL in each strand developed progressively through
CHAPTER - X WATER HARVERSTING AND RECHARGING IN HARD ROCK AREAS
CHAPTER - X WATER HARVERSTING AND RECHARGING IN HARD ROCK AREAS CHAPTER X WATER HARVERSTING AND RECHARGING IN HARD ROCK AREAS 10.0 CONCEPTUAL FRAME WORK From a technical stand point, though hard rock areas
The Geothermal Information System for Germany
The Geothermal Information System for Germany www.geotis.de Britta Ganz T. Agemar, J. A. Alten, J. Kuder, K. Kühne, S. Schumacher & R. Schulz CGER Meeting 21 May 2012, Oslo Project Funding Partners Support
PROTECTION OF THE GROUNDWATER RESOURCES OF METROPOLIS CEBU (PHILIPPINES) IN CONSIDERATION OF SALTWATER INTRUSION INTO THE COASTAL AQUIFER
17 th Salt Water Intrusion Meeting, Delft, The Netherlands, 6-10 May 2002 489 PROTECTION OF THE GROUNDWATER RESOURCES OF METROPOLIS CEBU (PHILIPPINES) IN CONSIDERATION OF SALTWATER INTRUSION INTO THE COASTAL
College of Science and Health ENVIRONMENTAL SCIENCE & GEOGRAPHY Course Outline
College of Science and Health ENVIRONMENTAL SCIENCE & GEOGRAPHY Course Outline 1. TITLE OF COURSE AND COURSE NUMBER: General Geology ENV 115, 4 credits 2. DESCRIPTION OF THE COURSE: Includes the study
Oil and Gas Terms. Anticline: An arch of stratified rock layers that may form a trap for hydrocarbons.
Oil and Gas Terms American Petroleum Institute (API): The API is the trade organization for the oil and gas industry, which establishes standards governing industry operations, safety and the manufacturing
Hydrogeology Experiment on Surface-Groundwater Interactions: How Do Our Actions Affect Water Quantity and Quality?
Name: Period: Hydrogeology Experiment on Surface-Groundwater Interactions: How Do Our Actions Affect Water Quantity and Quality? Purpose/Objective: Students will learn how groundcover influences surface
Step 2: Learn where the nearest divergent boundaries are located.
What happens when plates diverge? Plates spread apart, or diverge, from each other at divergent boundaries. At these boundaries new ocean crust is added to the Earth s surface and ocean basins are created.
Ground Water Surveys and Investigation
Ground Water Surveys and Investigation By Gautam Mahajan ASHISH PUBLISHING HOUSE 8/81, PUNJABI BAGH, NEW DELHI-110 026 - Contents Preface List of Abbrivations (v) (vii) 1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.7.1
Ground-Water-Level Monitoring and the Importance of Long-Term Water-Level Data U.S. Geological Survey Circular 1217
Ground-Water-Level Monitoring and the Importance of Long-Term Water-Level Data U.S. Geological Survey Circular 1217 by Charles J. Taylor William M. Alley Denver, Colorado 2001 U.S. DEPARTMENT OF THE INTERIOR
P02 Calibration of Density Driven Flow Model for the Freshwater Lens beneath the North Sea Island Borkum by Geophysical Data
P02 Calibration of Density Driven Flow Model for the Freshwater Lens beneath the North Sea Island Borkum by Geophysical Data H. Sulzbacher (LIAG), H. Wiederhold* (LIAG), M. Grinat (LIAG), J. Igel (LIAG),
Geological Maps 1: Horizontal and Inclined Strata
Geological Maps 1: Horizontal and Inclined Strata A well-rounded geologist must be familiar with the processes that shape the Earth as well as the rocks and minerals that comprise it. These processes cover
4.10 Geological models
4.10 Geological models 4.10 Geological models A geological model is a spatial representation of the distribution of sediments and rocks in the subsurface. The model is traditionally presented by 2D cross-sections,
ILLINOIS DEPARTMENT OF CENTRAL MANAGEMENT SERVICES CLASS SPECIFICATION ENVIRONMENTAL PROTECTION GEOLOGIST SERIES
ILLINOIS DEPARTMENT OF CENTRAL MANAGEMENT SERVICES CLASS SPECIFICATION ENVIRONMENTAL PROTECTION GEOLOGIST SERIES CLASS TITLE POSITION CODE ENVIRONMENTAL PROTECTION GEOLOGIST I 13801 ENVIRONMENTAL PROTECTION
Permafrost in Marine Deposits at Ilulissat Airport in Greenland, Revisited
NICOP IX International Conference on Permafrost University of Alaska Fairbanks 2008 Session 28: Cold Regions Infrastructures and Transportation Permafrost in Marine Deposits at Ilulissat Airport in Greenland,
MCLAREN VALE PWA GROUNDWATER LEVEL AND SALINITY STATUS REPORT 2009 10
MCLAREN VALE PWA GROUNDWATER LEVEL AND SALINITY STATUS REPORT 2009 10 SUMMARY 2009 10 The McLaren Vale PWA is located approximately 35 km south of Adelaide. It is a regional-scale resource for which groundwater
(1) Discuss the determination of the need for public visitation. Visitor center density within 100 miles.
Chapter 4 Specifications Designs 3. Visitors Centers 3. Visitors Centers. The Introduction (Chapter 1) for these design data collection guidelines contains additional information concerning: preparing
Plotting Earthquake Epicenters an activity for seismic discovery
Plotting Earthquake Epicenters an activity for seismic discovery Tammy K Bravo Anne M Ortiz Plotting Activity adapted from: Larry Braile and Sheryl Braile Department of Earth and Atmospheric Sciences Purdue
PHYSICAL GEOLOGY LAB ONLINE SYLLABUS GLY 1010L Physical Geology Lab Fall 2010
This course is not taught completely online. Please note that you must complete five labs using materials at the Dale Mabry Campus library in Tampa to participate in this course. PHYSICAL GEOLOGY LAB ONLINE
Assessment of groundwater inflow into a metro tunnel (Ankara)
Géoline 25 Lyon, France 23 rd - 25 th, May/Mai 25 Assessment of groundwater inflow into a metro tunnel (Ankara) DOYURAN VEDAT Department of Geological Engineering, Middle East Technical University, 6531Ankara,
Using Google Earth to Explore Plate Tectonics
Using Google Earth to Explore Plate Tectonics Laurel Goodell, Department of Geosciences, Princeton University, Princeton, NJ 08544 [email protected] Inspired by, and borrows from, the GIS-based Exploring
POTENTIAL FOR SUBSIDENCE FISSTJRING IN THE PHOENIX ARIZONA USA AREA
POTENTIAL FOR SUBSIDENCE FISSTJRING IN THE PHOENIX ARIZONA USA AREA Michael K. Larson Kansas Department of Health and Environment Bureau of Oil Field and Environmental Geology 10U Cody Hays, Kansas 67601
Minnesota Department of Natural Resources \mn_dnr \mn_dnr\spatial \mn_dnr\tabular \mn_dnr\metadata
INDEX OF GIS SPATIAL DATA, TABULAR DATA, AND METADATA ASSOCIATED WITH REPORT 380, AGGREGATE RESOURCE POTENTIAL PARTS OF NORTHERN ST. LOUIS AND LAKE COUNTIES, MN. Project of the Minnesota Department of
VULNERABILITY ASSESSMENT OF GROUNDWATER RESOURCES IN THE LAMPANG BASIN OF NORTHERN THAILAND. Bangkok, Thailand, 10300. Chiang Mai, Thailand, 50200.
VULNERABILITY ASSESSMENT OF GROUNDWATER RESOURCES IN THE LAMPANG BASIN OF NORTHERN THAILAND K. Kwansiririkul 1, F. S. Singharajwarapan 2, T. Ramingwong 2, and P. Wongpornchai 2 1 Office of Engineering
WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST. Which graph best shows the relative stream velocities across the stream from A to B?
NAME DATE WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST 1. The diagram below shows a meandering stream. Measurements of stream velocity were taken along straight line AB. Which graph best shows the
Map Patterns and Finding the Strike and Dip from a Mapped Outcrop of a Planar Surface
Map Patterns and Finding the Strike and Dip from a Mapped Outcrop of a Planar Surface Topographic maps represent the complex curves of earth s surface with contour lines that represent the intersection
GEOLOGY AND GEOMORPHOLOGY Level. bachelor Semester. winter ECTS 9
GEOLOGY AND GEOMORPHOLOGY ECTS 9 The subject includes knowledge of the construction of the Earth and the natural processes occurring deeply inside and on the surface of the Earth. It contains characteristics
ESSENTIAL COMPONENTS OF WATER-LEVEL MONITORING PROGRAMS. Selection of Observation Wells
ESSENTIAL COMPONENTS OF WATER-LEVEL MONITORING PROGRAMS Before discussing the uses and importance of long-term water-level data, it is useful to review essential components of a water-level monitoring
Groundwater Flooding: a UK Perspective
Groundwater Flooding: a UK Perspective David Macdonald British Geological Survey Maclean Building Crowmarsh Gifford Wallingford OX10 8BB Tel 01491 838800 NERC All rights reserved Talk outline Definition
Rocks & Minerals. 10. Which rock type is most likely to be monomineralic? 1) rock salt 3) basalt 2) rhyolite 4) conglomerate
1. Of the Earth's more than 2,000 identified minerals, only a small number are commonly found in rocks. This fact indicates that most 1) minerals weather before they can be identified 2) minerals have
Modelling the Discharge Rate and the Ground Settlement produced by the Tunnel Boring
Modelling the Discharge Rate and the Ground Settlement produced by the Tunnel Boring Giona Preisig*, Antonio Dematteis, Riccardo Torri, Nathalie Monin, Ellen Milnes, Pierre Perrochet *Center for Hydrogeology
Guidelines for the Estimation and Reporting of Australian Black Coal Resources and Reserves
Guidelines for the Estimation and Reporting of Australian Black Coal Resources and Reserves 2001 Edition (as referred to in the Joint Ore Reserves Committee Code ( The JORC Code ) 1999 edition) Prepared
Soil and Groundwater Salinization Problems in the Khorat Plateau, NE Thailand - Integrated Study of Remote Sensing, Geophysical and Field Data
Soil and Groundwater Salinization Problems in the Khorat Plateau, NE Thailand - Integrated Study of Remote Sensing, Geophysical and Field Data Probleme der Boden- und Grundwasserversalzung in der Khorat
Development of Rural Drinking Water Security Plan A Case Study from Raipur Block, Bhilwara District, Rajasthan
Development of Rural Drinking Water Security Plan A Case Study from Raipur Block, Bhilwara District, Rajasthan Dr. B. K. Bhadra Scientist/Engr. SF Regional Remote Sensing Centre (RRSC-W) NRSC/ISRO, Dept.
GROUND RESPONSE OF KATHMANDU VALLEY ON THE BASIS OF MICROTREMORS
GROUND RESPONSE OF KATHMANDU VALLEY ON THE BASIS OF MICROTREMORS MADHAB R PANDEY 1 SUMMARY Devastation of Kathmandu valley from historical earthquakes, the M8.3 Bihar - Nepal Great Earthquake of 1934 in
All sediments have a source or provenance, a place or number of places of origin where they were produced.
Sedimentary Rocks, Processes, and Environments Sediments are loose grains and chemical residues of earth materials, which include things such as rock fragments, mineral grains, part of plants or animals,
GPR survey and field work summary in Siilinjärvi Mine during July 2014 Samrit Luoma, Juha Majaniemi, Tiina Nurminen, and Antti Pasanen
GEOLOGICAL SURVEY OF FINLAND Southern Finland Office Espoo 74/2014 31.3.2015 GPR survey and field work summary in Siilinjärvi Mine during July 2014 Samrit Luoma, Juha Majaniemi, Tiina Nurminen, and Antti
River Basin Management in Croatia
River Basin Management in Croatia 2. INTERNATIONAL RIVER BASIN MANAGEMENT HIGH LEVEL SYMPOSIUM Cappadocia/NEVŞEHİR, Turkey 16-18 April 2013 2 Water sector responsibilities are shared among: Croatian Parliament
The ATES Project at Stockholm Arlanda Airport - Technical Design and Environmental Assessment
The ATES Project at Stockholm Arlanda Airport - Technical Design and Environmental Assessment O. Andersson SWECO Environment AB Box 286, 201 22 Malmö, Sweden Tel: +46 40 167214 [email protected]
The Role of Groundwater in Alberta s Tight Water Supply Environment. Ken Baxter, M.Sc., P.Geol. Dan R. Brown, M.Sc., P.Geol.
The Role of Groundwater in Alberta s Tight Water Supply Environment Ken Baxter, M.Sc., P.Geol. Dan R. Brown, M.Sc., P.Geol. The Role of Groundwater in Alberta s Tight Water Supply Environment Outline Importance
Understanding Complex Models using Visualization: San Bernardino Valley Ground-water Basin, Southern California
Understanding Complex Models using Visualization: San Bernardino Valley Ground-water Basin, Southern California Zhen Li and Wesley R. Danskin U.S. Geological Survey, [email protected], [email protected],
Weathering, Erosion, and Soils. Weathering and Erosion. Weathering and Erosion
Weathering, Erosion, and Soils 1 The Grand Canyon, a landscape shaped by weathering and erosion 2 Weathering vs. erosion Types of weathering Physical Chemical Rates of weathering and erosion Climate Rock
Can GIS Help You Manage Water Resources? Erika Boghici Texas Natural Resources Information Systems
Can GIS Help You Manage Water Resources? Erika Boghici Texas Natural Resources Information Systems Hydrologic Information System Hydrologic Modeling Arc Hydro Geodatabase Arc Hydro Data Model: combination
GEOLOGIC MAPS. PURPOSE: To be able to understand, visualize, and analyze geologic maps
GEOLOGIC MAPS PURPOSE: To be able to understand, visualize, and analyze geologic maps Geologic maps show the distribution of the various igneous, sedimentary, and metamorphic rocks at Earth s surface in
Geothermal. . To reduce the CO 2 emissions a lot of effort is put in the development of large scale application of sustainable energy.
Geothermal Energy With increasing fossil fuel prices, geothermal energy is an attractive alternative energy source for district heating and industrial heating. In recent years the use of geothermal energy
Eurocode 7 - Geotechnical design - Part 2 Ground investigation and testing
Brussels, 18-20 February 2008 Dissemination of information workshop 1 Eurocode 7 - Geotechnical design - Part 2 Ground investigation and testing Dr.-Ing. Bernd Schuppener, Federal Waterways Engineering
Missouri Regions Shaped by Land Forms and Geology
Missouri Regions Shaped by Land Forms and Geology Lesson Abstract Summary: MO GLE: Subject Areas: The students will use various resources to compare and contrast the geology of each Missouri region to
Groundwater flow systems theory: an unexpected outcome of
Groundwater flow systems theory: an unexpected outcome of early cable tool drilling in the Turner Valley oil field K. Udo Weyer WDA Consultants Inc. [email protected] Introduction The Theory of
INTERPRETATION ADDENDUM CANADIAN MINING COMPANY INC. SUITE 2300-1066 WEST HASTINGS STREET VANCOUVER, BC V6E 3X2 3D INDUCED POLARIZATION
INTERPRETATION ADDENDUM FOR CANADIAN MINING COMPANY INC. SUITE 2300-1066 WEST HASTINGS STREET VANCOUVER, BC V6E 3X2 3D INDUCED POLARIZATION ON THE SAN BERNARDO PROJECT EL GOCHICO GRID Approximate Location:
NuGeneration Ltd Site Investigations
NuGeneration Ltd Site Investigations Introducing the site assessment and radiological characterisation project NuGen has commissioned an engineering consortium - which is a joint venture of IBERDROLA Ingeniería
Examples of Data Representation using Tables, Graphs and Charts
Examples of Data Representation using Tables, Graphs and Charts This document discusses how to properly display numerical data. It discusses the differences between tables and graphs and it discusses various
Chapter 9: Water, Hydrology and Drainage Land West of Uttoxeter
Chapter 9: Water, Hydrology and Drainage Land West of Uttoxeter ENVIRONMENTAL STATEMENT: VOLUME 1 9.1 INTRODUCTION 9.1.1 This Chapter considers the effects of the Project on surface water and groundwater
GIS Data assessment for Region II of Chile Implications for international Water Resource Databases
GIS Data assessment for Region II of Chile Implications for international Water Resource Databases GIS in Water Resources (CE 394K) Term Paper Benjamin Bass December 2 nd, 2011 Wikimedia Commons SITHA
Introduction. The vision of the West Yorkshire Combined Authority (WYCA) Flood Risk Partnership
WYCA SuDS Guidance Introduction As part of the government s continuing commitment to protect people and property from flood risk, the Department for Communities and Local Government and the Department
Curriculum Map Earth Science - High School
September Science is a format process to use Use instruments to measure Measurement labs - mass, volume, to observe, classify, and analyze the observable properties. density environment. Use lab equipment
Influence of various factors on the fluctuation of groundwater level in hard rock terrain and its importance in the assessment of groundwater
Journal of Geology and Mining Research Vol. 3(11) pp. 305-317, November 2011 Available online at http://www.academicjournals.org/jgmr ISSN 2006-9766 2011 Academic Journals Full Length Research Paper Influence
Hot tpot tproject A Demonstration of How Groundwater Chemistry is being Used to Discover a Gravel Covered Gold Deposit
Hot tpot tproject A Demonstration of How Groundwater Chemistry is being Used to Discover a Gravel Covered Gold Deposit April 2, 2009 General Cautionary Statement Warning! The business of Gold Exploration
Plate Tectonics: Big Ideas. Plate Tectonics. Plate Tectonics. The unifying concept of the Earth sciences.
Plate Tectonics: Big Ideas Our understanding of Earth is continuously refined. Earth s systems are dynamic; they continually react to changing influences from geological, hydrological, physical, chemical,
Exploration. Exploration methods
Exploration Activities related to establishing a mineral deposit through geological, geophysical and geochemical methods. It is preceded by Prospecting and followed by Planning & Development. Geological
Assessment of Groundwater Vulnerability to Landfill Leachate Induced Arsenic Contamination in Maine, US - Intro GIS Term Project Final Report
Assessment of Groundwater Vulnerability to Landfill Leachate Induced Arsenic Contamination in Maine, US - Intro GIS Term Project Final Report Introduction Li Wang Dept. of Civil & Environmental Engineering
WHAT IS GIS - AN INRODUCTION
WHAT IS GIS - AN INRODUCTION GIS DEFINITION GIS is an acronym for: Geographic Information Systems Geographic This term is used because GIS tend to deal primarily with geographic or spatial features. Information
CHAPTER 9 CONCLUSIONS AND RECOMMENDED MITIGATION
CHAPTER 9 CONCLUSIONS AND RECOMMENDED MITIGATION 9.1 Conclusions Based on the stability cross-sections down the SE flank of Snodgrass Mountain, most landslides on low- to moderate-gradient slopes have
Construction Effects of the Karun 4 Dam, Iran, on the Groundwater in the adjacent Karstic Aquifer
Construction Effects of the Karun 4 Dam, Iran, on the Groundwater in the adjacent Karstic Aquifer Seyed Mohammad Hosseiny Sohi 1, Manfred Koch 1, Javad Ashjari 2 1 Department of Geohydraulics and Engineering
Water-Table Elevation and Depth to Water Table
Water-Table Elevation and Depth to Water Table By Roberta Adams Minnesota Hydrogeology Atlas Series Atlas HG-03 Report Plate 1, Water-Table Elevation Plate 2, Depth to Water Table St. Paul June 2016 Minnesota
THE PROVISIONAL CENTRAL PRODUCT CLASSIFICATION
THE PROVISIONAL CENTRAL PRODUCT CLASSIFICATION GROUP 867 ARCHITECTURAL, ENGINEERING AND OTHER TECHNICAL SERVICES Excerpt from CPCprov-en-Publication.doc - United Nation Statistic Division Group Class Subclass
