Piedmont and Blue Ridge Crystalline rocks with glacial cover.

Slides:



Advertisements
Similar presentations
Rocks and Minerals.
Advertisements

1 rock forming minerals quartz feldspar amphibole pyroxene mica clay calcite gypsum.
Metamorphic Rocks Two Words Not Happy Birthday!!.
Aquifers of the U.S. Fractured RockAquifers of the U.S.
Types of Rocks Sedimentary Igneous Metamorphic. Sedimentary Rock Write the term and what you believe it to mean.
Rocks & Minerals Review
Chapter 8 Fetter, Applied Hydrology 4 th Edition, 2001 Geology of Groundwater Occurrence.
CHAPTER 2 MINERALS AND ROCKS.
Interception on trees, impermeable surfaces Infiltration into soil Interflow downslope along B horizon Overland flow during heavy rain Recharge reaches.
Matching Metamorphi c Rocks with their Sedimentar y Source Rocks.
Karst Chemistry I. Definitions of concentration units Molality m = moles of solute per kilogram of solvent Molarity [x]= moles of solute per kilogram.
GEOLOGY OF THE PIEDMONT IN NEW JERSEY J. Michael Pollock New Jersey Audubon Adapted for Summer Field Studies 2012.
TEMPLATE DESIGN © Carbon Sequestration: Super Critical CO 2 ’s effect on subsurface brines in the Illinois Basin Daniel.
Unit 5 – Weathering, Erosion, & Deposition Review
Hydrogeochemistry “Geochemistry of Natural Waters”
Rocks and Minerals. I. Rocks vs Minerals A. Rock – solid part of earth, make up lithosphere B. ALL rocks are made of minerals 1. Monomineralic – rocks.
Rock Cycle. Goals You will be able to identify the basic characteristics of different types of rocks You will be able to label and identify all of the.
Minerals and Rocks. Lecture Outline What are minerals? What are minerals? Common rock-forming minerals Common rock-forming minerals Physical properties.
Rocks and Minerals Atoms, Elements, Isotopes, Ions, and Compounds Minerals–General Types of Minerals Rocks.
Geologic Framework Development in Fractured Bedrock EPA Region II Fractured Rock Training January 14, 2014 Pierre Lacombe.
CE 410 CE 410 Soil Mechanics u LESSON OBJECTIVES  Explain in engineering terms the difference between rock and soil.  Explain what is soil composed of.
Properties of Oilfield Waters Lectures # 30 – 31 PETE 310.
Water chemistry overview 4 Oct 2001 Announcements –Canoe trip!! –Exam next Wednesday –College certified drivers? Today's lecture –The idea of budgets –Factors.
Chapter 2 Rocks.
Do Now 2/26 1.How do you find the Hardness of a Mineral? 1-2 Mineral Can be scratched with your fingernail 2-3 Mineral can be scratched with a penny 4-5.
Cycles of the Earth. EARTH RECYCLES ALL MATTER FORMING ITS OUSIDE LAYERS –Analyze cycles based on the “reservoirs” that hold matter and the movement of.
Types of Rocks Chapter 31 There are three main types of rocks:
Virginia Physical Geography
Virginia Physical Geography. The Physiographic Provinces of Virginia Virginia has had a long, complex geologic history, over 1.1 billion years Events.
Structure of the Earth and Mineralogy Environmental Science Earth Science Unit Environmental Science Earth Science Unit.
EPA Region II Fractured Rock Training January 14, 2014 Pierre Lacombe
Difference Between a Rock and a Mineral
ROCKS. What is a rock? ► A mixture of minerals ► OR organic material.
Review for rocks and minerals
Focus on the Headwaters The Shenandoah Watershed Study / The Virginia Trout Stream Sensitivity Study Rick Webb Department of Environmental Sciences University.
Aquifers in Alluvial Sediment River valley draining glaciated area Rivers draining area in west with high Pleistocene rainfall Fault-bounded basins in.
1 A Geologic Safari of the East African Rift and the Newark Basin: Why these areas are more alike than you know Part 3: Focus on New Jersey Margaret H.
Hydrogeology in the Limpopo Basin
Metamorphic Rocks A.Evidence of metamorphism B.The ingredients of metamorphism C.Classifying metamorphic rocks D.Metamorphism of shale (& other parent.
Minerals, Rocks and Fossils. What is a mineral? Naturally occurring Naturally occurring Non-organic Non-organic Characteristic chemical composition Characteristic.
Rocks. Parts of presentation: 1. What is rock 2. Classes of rocks 3. The Rock cycle.
Carrin Williams. Pennsylvania’s Aquifers An aquifer is an underground layer of water-bearing permeable rock or unconsolidated materials from which groundwater.
Igneous Sedimentary Metamorphic. Classify these rocks Gneiss Pumice Limestone Slate Shale Obsidian Quartzite Sandstone Basalt Conglomerate Marble Granite.
Georgia Geology Notes – 4 Provinces
Unit 17 STRUCTURE OF THE EARTH. What are the different types of rocks? IGNEOUS ROCKS formed from molten rocks (magma) that flow to the Earth’s surface.
Rocks and the Rock Cycle Geology: The study of rocks, minerals and fossils.
CH 6 Rocks & Rock Cycle Quiz Review. Plagioclase feldspar, biotite, pyroxene, amphibole, and olivine are common minerals in felsic/mafic igneous rocks.
The rock cycle illustrates the process that creates and changes rocks. The rock cycle shows the three types of rock- igneous, metamorphic, and sedimentary-
ES5 Rocks Igneous, Sedimentary, Metamorphic. Standard 5a.
Piedmont and Blue Ridge Crystalline rocks with glacial cover.
Move Discussion from Wednesday to Friday Read for the discussion: ’Climate Change 2001: The Scientific Basis - Summary for Policy Makers’ You can download.
How is concrete different from a conglomerate rock? A. Concrete is human-made and conglomerate forms in nature. B. Concrete is grainy and conglomerate.
Mineral & Rock Review Chapters 3 & 4. Minerals  A naturally occurring, inorganic solid with crystal structure and a definite chemical composition  Families.
NS3310 – Physical Science Studies
Mineral & Rock Review Chapters 3 & 4.
Minerals, Rocks and Fossils
Rock Types November 21, 2011.
Minerals, Rocks and Fossils
Water – The Universal Solvent
Rocks and Minerals Metamorphic rocks.
Minerals, Rocks and Fossils
Mineral & Rock Review Chapters 3 & 4.
Minerals, Rocks and Fossils
Chapter 3 Prentice-Hall Earth Science 2006
Geology of Groundwater Occurrence
Minerals, Rocks and Fossils
The Rock Cycle.
Identify the Rocks Do Now.
Presentation transcript:

Piedmont and Blue Ridge Crystalline rocks with glacial cover

Paleozoic history of southern Piedmont From Hatcher

Metamorphic and igneous rock Sandstone and diabase in rift basins Limestone

Piedmont Chimney rock Blue Ridge Province

flow through fractures

Transition Fractured metamorphic and igneous rock Saprolite

Gneiss, schist bedrock Granite or other intrusive bedrock Distinct transition Gradational transition

Storage and transmission properties High porosity S y ? porosity Low storage cm/s

Saprolite sampled at different depths. Measure density and chemical composition. S.G. decreases from 2.1 in rock to 1.6 in shallow saprolite. S.G. decreases as minerals are altered and mass is removed. 0.5 gm/cc removed during weathering. Chemical concentrations indicate S.G. change largely due to weathering of feldspar to kaolinite as a two-stage reaction.

Porosity Specific yield K cm/sec Granitic Gneiss E-08 Mica Schist E-09 Hornblende-feldspar gneiss E-09 Quartzite E-09 Amphibolite E-09 Laboratory determinations of properties of crystalline rocks. from Randall and others 1966

Saprolite thickness Typically 50 ft, but variable ft w.t ft bgs Frx zones in valleys Flat-lying frx

Saprolite thickness Greatest over valley or highland? Could be either

Ground watersheds

Open Hole Multi-level completion

Important: Exception to the Conceptual Model

Specific capacity Well Performance and Lineaments

Lineaments

Effects of lineaments on well yields in the Piedmont Other effects of location on well yield Factor of 2 to 7 difference in yield Factors from 3 to 25 between valley and hill

Well yields in different rock types and regions in the Piedmont gpm typical Roughly 20 gpm

Effects of well depth and diameter on yield in the Piedmont. Based on Daniels

Glaciated crystalline rocks in northern Appalachians

Other Hydrogeologic Settings in the Piedmont

Stockton Fm. Lockatong Fm. Passaic Fm. Orange Mt. Basalt Feltville Fm. Preakness Basalt Towaco Fm. Hook Mt. Basalt Boonton Fm. Conglomerates Palisade sill

Newark Basin, NJ Mesozoic Basins Sandstone aquifers Shale confining units Redbeds in the Hartford Basin, Conn Conglomerate Basalt Arkose

Carbonate rock aquifers

Water Chemistry Reminder Major Cations: Na +, K +, Ca 2+, Mg 2+ Major Anions: HCO 3 -, Cl -,SO 4 2- TDS: Total Dissolved Solids MCL= 500 mg/l Values: Fresh < 1000 mg/l; brackish ,000; saline; 10, ,000 mg/l Seawater: 35,000 mg/l Hardness: Ca and Mg scaled to Ca on a meq basis –Soft water < 60 mg/l total hardness –Use water softener= mg/l –Very hard >150 mg/l

Milliequivalent Charges/volumes Concmg millimol evalencecharge meqmillimole charge liter Mole weight mgliter

Water quality in Crystalline Rock aquifers

Crystalline rock Triassic Basin Carbonate rock meq/L

Crystalline Rock Triassic Basins Carbonate Aquifers

SC, GA, Al =100 Mgpd