Sample Interval: from 0 to' L20~4~ Total depth ~2~Q~4L- Oil Gas Water~Exploratory. Cutt ing s x Core Other. From-To From-To From- To

INTERV AL SHEET. VDMR Well No.: WELL NO. 699 WWCR #186. Oil Gas, Water_ X,Exp1oratory. From- To 300_ _ _ _

) Page,_-=-H~l,-- Date, 8~-~2~7_-~62=- PROP: PROP : BLUE RIDGE POULTRY AND EGG CXi. #2 COMP: COMP : SYDNOR COUNTY: SHENANDOAH COUNTY: (CDLUMB IA FURNACE) VDMR WELL NO. W699 FROM: TO : INTERV AL SHEET VDMR

GEOLOGIC LOG. sandy. coarse-grained, dark-green autochthonous glauconite; minor amount of sand-grade shell debris, foraminifers rare

OWNER: William E. Hackney o (Rivercliff Subdivision) DRILLER: Pittman wood & Metal Products Co. COUNTY: Nansemond (Driver) VDMR: WWCR: TOTAL DEPTH: 2092 173 607' GEOLOGIC LOG Depth in feet COLUMBIA GROUP

GEOLOGIC LOG Sand - orange-brown, slightly clayey; fine- to medium-grained, very well-sorted, subangular to subrounded; trace of feldspar

OWNER: Fred W. Haislip DRILLER: Douglas & Dickinson, Inc. COUNTY: Northumberland (Burgess) Depth in feet GEOLOGIC LOG VDMR: WWCR: TOTAL DEPTH: 2000 140 673' COLUMBIA GROUP (0-42') 0-10 Sand - orange-brown,

OWNER: Lone Star Cement Corporation DRILLER: R. L. Magette Well Drilling Corp. COUNTY: Norfolk (S. Norfolk). GEOLOGIC LOG. feet.

Lone Star Cement Corporation DRILLER: R. L. Magette Well Drilling Corp. COUNTY: Norfolk (S. Norfolk). W: 2111 C: 165 TOTAL DEPTH: 800' GEOLOGIC LOG Depth feet in 0-40 No Samples YORKTOWN FORMATION (40-360')

, , INTERVAL SHEET WWCR 133. VDMR WELL NO.: Well No

Pa ge 1 INTERVAL SHEET VDMR WELL NO.: Well No. 1184 WWCR 133 Date 11/16/64 Sample Interval: fr om'--_o=-- to 640 PROP : Ditchley Water Works Total Depth_-64.:.0- COMP: Fedderoff Bros. COUNTY: Northumberland

INTERVAL SHEET. Tot aid epth ~9'-'OLf2~ Oil Gas Water~E xplo r atory. Fr om- To

Page ~l INTERVAL SHEET VDMR Well No. :WELL NO: 866 WWCR 878 Date 7~/~2~4~/~6~3~ PROP: Morton's Frozen Foods Well #5 COMP: C. R. Moore COUNTY: Albemarle (Crozet VDMR WELL NO: W - 866 Sample Interval: from

VDMR #1306 WWCR #63 TOTAL DEPTH: 10ISO" OWNER: Bayberry Estates DRILLER: J. T. Ellington COUNTY: King George (Dahlgren) GEOLOGIC LOG No sample.

() DRILLER: J. T. Ellington COUNTY: King George (Dahlgren) VDMR WWCR #63 TOTAL DEPTH: 10ISO" GEOLOGIC LOG 0-240 No sample. Aquia Formation (240-300') 240-255 -255-270 270-285 285-300 Sand - dark-gray with

VDMR Well No GEOLOGIC LOG. Depth in feet. NO sample 0-3 COLUMBIA GROUP 3-5 (3-13')

VDMR Well No. 2214 Well: DVL (Drewryville Property: state road right-of-way Driller: Froehling and Robertson Location: near Drewryville, on Rte. 659 and 0.4 mile N of Rte. 652 Elevation: 50 feet Total

DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER Co. Iollesville, VA WATER WELL COMPLETION REPORT

MAILING ADDRESS, B- 3667 W#: 5141 COMMONWEAL TH OF VIRGINIA C#: 211 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L CALVER, COMMISSIONER Co Iollesville,

) - --' o - 10 No sample No sample No was hed samples

INTERVAL SHEET r'age_...::.1 VDMR WELL NO.: Well No. 1177 WWCR 174 Date_~1~lL/~6 L/6~4~ Sample Interval: from~...::.l~o to 326 PROP : Robinwood Subdivision #2 Total Depth_.::3.::2.::6 COMP: Mitchell's

INTERVAL SHEET. VDMfl. Well No.: Well No. lloo. Tota 1 depth,_~5,-,0",0,- Oil Gas Water~Exploratory' From-To From-To From-To

Page' l'- INTERVAL SHEET VDMfl. Well No.: Well No. lloo WWCR483 Date'_~7~/~2~2~/~64~ PitOP: Town of McGaheysville Well #2 Sydnor COUNTY: Ro ckingham (McGaheysville) VDMR Well No: W-1100 From-To From-To

DIVISION OF MINERAL RESOURCES JAMES L. CALVER, COMMISSIONER WATER WELL COMPLETION REPORT

MAILING ADDRESS, Bc 3667 C. Jiottesville, VA 22903 COMMONWEALTH OF VIRGI N IA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES JAMES L. CALVER, COMMISSIONER WATER WELL

DIVISION OF MINERAL OFFICE ADDRESS, JAMES L. CALVER. COMMISSIONER '-, riottesville, VA WATER WELL COMPLETION REPORT

MAILING ADDRESS, P. 3667 COMMONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT \ VDMR: 2332 WWCR: 79 DIVISION OF MINERAL OFFICE ADDRESS, JAMES L. CALVER. COMMISSIONER '-, riottesville,

DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER

MAILING ADDRESS, B- 3667 COMMONWEALTH OF VIRGI N IA DEPARTMENT OF CONSERVATION AND ECONOM IC DEVELOPMENT W# : 3795 C#: 77 DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER C.

o - 399' ' ' ' ' T. D.

Ii I I' I: VDMRWellNo W-1142 Operator: J W Miloncus Farm: Browning Wynn Well No. : 1 Location: Lee County 3300' N of 36 042'30" 1800' E of 83005' approx Elevation: 1975' (reported altimeter elevation)

u. S. Geological Survey,

VDMR Well No. Operator: Southwestern Oil and 'Gas Company Farm: Hagan Well No.: 1 Location: Wise County 9300' S. of 36 055') 600' E. of 82030,)approximate Elevation: 2500' Total Depth:3751' Drill'ing Comrilenced:

TENANT: Moiling Address: feet. -=d:.:e:.:a:.:d::...,:e:.:n.:;d::...o:;,i::...s=.t,:;,:..-=.r:,::t"'.-=6"'8"'0'-- and mi les ( d i rec lion) 01

COMMONWEALTH OF VIRGINIA W#: 3575 C#: 182 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT MAILING ADDRESS, DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, B 3667 JAMES L. CALVER, COMMISSIONER l : Iollesvilie,

GEOLOGIC LOG " coarse- to very coarse-grained, fairly wellsorted, subangular to rounded.

OWNER: Sydnr Hydrdynamics, Inc. DRILLER: Sydnr Hydrdynamics, Inc. COUNTY: Hanver (Atlee) GEOLOGIC LOG VDMR - 1770 WWCR - 98 TOTAL DEPTH - 370' Depth in Feet COLUMBIA GROUP (0-50) - 10 10-20 20-30 Sand

INTER VAL SHEET. From-To Elevation in feet

INTER VAL SHEET Page 1 of 1 VDMR Well No: 618 Date rec'd : 3 / 23/61 Sample Inte rva1: from 0 'to : 109. 0, PROP : Skeet Rock Darn Site, hole # 1 Number of samples: 32 COMP : Adams and Henry (U. S. Corps

DIV I SION OF MI NERAL RESOURCES OFFICE ADDRESS,

MAILING ADDRESS, B' 3667 C. lol lesville, VA 22903 OF VIRGINIA AND ECONOMIC DEVELOPMENT REPOR T W-425l C- 169 DIV I SION OF MI NERAL RESOURCES OFFICE ADDRESS, WAT ER C OM M ONWEALTH DEPART ME NT OF CONSER

snt s tone, locally shaly,carbonaceous( la:ally)

Company: United Pr oduc inq Co,, Inc. -Farm: Pocahontas Mining Corp. Well No.: 1-1784 Elevation: 2519.4 Total Depth: 5735' Location: Buchanan County 50' S. of 37 015' 200' E. of 81 045' Drilling Commenced:

UNIT DESCRIPTIONS: Artificial Fill, Undocumented (Afu): Locally derived sandy silt and silty sand, locally with clay and varying amounts of gravel and man-made debris. Abundant concrete rubble, in places

COM MONWE ALTH OF VIRGINIA DE PART MENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL R ESO URCES OFFICE ADDRESS, COMPLETION

M A ILING A DDRESS, B ~ " 3667 l Iotte sville, VA 22903 WATER COM MONWE ALTH OF VIRGINIA DE PART MENT OF CONSERVATION AND ECONOMIC DEVELOPMENT COMPLETION REPOR T W# : C#: 44 43 83 DIVISION OF MINERAL R

* Ro t e _~ 3 gal. per min.

COM MONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT W #Z345 C #140 MAILING ADDRESS, DIVISION OF MINERAL.: RESOURCES OFFICE ADDRESS, ~ 3667

o _10 10 _ eo

INTERVAL SH E E T P a g e 1 of 1 Da t e rec'd: 10-1 6-67 P R OP: N & W RR. W ell # 218 VDMR Well N o : 20 2 2 Sa m ple Interval: fr om 0 t o : 65 Num b er o f samples: 7 CaMP: Princ e Georg e T otal D

Lithological variation of Middle Bakken reservoirs in SE Saskatchewan: implications for optimizing multi-stage hydraulic fracturing

Lithological variation of Middle Bakken reservoirs in SE Saskatchewan: implications for optimizing multi-stage hydraulic fracturing Hairuo Qing, Guoxiang Chi, Adam Sturiala Dept of Geology University of

DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER WATER WELL COMPLETION REPORT

MAILING ADDRESS, B~ 3667 C..Iottesville, VA 22903 COM M ONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT W-4232 C-399 DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER,

COM MONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT. Mo i1in9 Address:..:..:=======_====-

MAILING ADDRESS, B0-3667 COM MONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT W-3589 C-356 DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER ( ollesville,

DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER

MAILING ADDRESS, B, 3667 COMMONWEALTH OF VIRGINIA OEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT V DMR: 2313 WWCR: 31 3 DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER

DIV ISION OF MINERAL R ESOURCE S O FF ICE A DDRESS,

MAILING A DDRESS, Box 366 7 C' - Ic tre sville, VA 22903 OWNER: WELL OF V I RG I NI A A N D ECONOM IC DEV E LOPMEN T COMPL ET ION REPORT W- 4394 C-178 DIV ISION OF MINERAL R ESOURCE S O FF ICE A DDRESS,

GEOLOGIC LOG. Sand - orange-brown; coarse- to very- coarse-grained, wellsorted, subrounded; some hyacinth quartz; slightly arkosic.

,] OWNER: Mount Rose Canning Company DRILLER: Sydnor Pump & Well c«., Inc. COUNTY: King George (Montague) VDMR #1367 WWCR #64 TOTAL DEPTH: 915' Upland Sand and Gravel (0-50') GEOLOGIC LOG 0-10 10-20 20-30

COM MONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT. feet

MAILING ADDRESS, B 3667 COM MONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER c.. _.lottesville. VA

) Ro t e _==-_ 503 gal. per min.

.. MAILING ADDRESS, Box 3667 COM MONWEAL TH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT W# 3681 DIV I S ION OF MINERAL R ESOU RC ES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER McCormick

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

DIV ISIO N OF MINERAL RES OURC ES OFFICE A DDRESS,

MAILING AD DRESS, Box 3667 r ' rl oltesvill e, VA 22903 WATER CO M MON WEALTH OF VI R G INI A DE PARTMEN T OF CONSERVATI ON A N 0 ECONOM IC DE V ELOPMEN T REP ORT W-3562 C-156 DIV ISIO N OF MINERAL RES

INTERVAL SHEET. Page 1 of 1. VDMR Well No: Date rec 'd: Sample Interval : from 8' 6" to: 114'6

INTERVAL SHEET Page 1 of 1 Date rec 'd: PROP : BLM A-050367 Hole No.: COMP o Minerals Development Corp. VDMR Well No: 2128 Sample Interval : from 8' 6" to: 114'6 Number of samples: 50 Total Depth: 11 4'6"

Factors Contributing to High Gamma-Ray Levels in Early Miocene Bhuban and Boka Bil Sandstone Reservoirs of Titas-15 Well

Dhaka Univ. J. Sci. 59(2): 209-216, 2011 (July) Facrs Contributing High Gamma-Ray Levels in Early Miocene Bhuban and Boka Bil Sandsne Reservoirs of Titas-15 Well M. Mostafizur Rahman 1, Badrul Imam 1,

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

9$ -,,00. DY'f. of lii)'wt{rs - ~, - J"I. .1f - ~, .,. 9, (( J - -.3,

VIRGINIA DIVISION ~F MINERAL RESOURCES Box 3667. Charlottesville. VA 22903 INTERVAL SHEET Page I of I Date rec'd Date Processed: PROPERTY: V(.. COMPANY: \to ~T DY'f. of lii'wt{rs COUNTY: Jq~ L.-i'f. iv'.1

C OM M ON WE AL T H OF VIR GI N IA DEPARTM ENT OF CONSER VATION AND ECONOMIC

MAILING ADDRESS, B- 3667 C.. ot tes vllle, VA 229 03 WAT ER C OM M ON WE AL T H OF VIR GI N IA DEPARTM ENT OF CONSER VATION AND ECONOMIC DIV ISION W# 4 257 C# 13 4 DEVELOPMEN T OF MINERAL RESOURCES OFFICE

Sedimentary Rocks. Weathering. Mechanical & Chemical Weathering. Sediments. Lithification. Deposition. Transport. Erosion.

Lithification Sedimentary Rocks Sediments Deposition Transport Erosion Weathering Weathering The sediments that make up sedimentary rocks are produced by: Mechanical & Chemical Weathering Mechanical Weathering

Log of Monitoring Well D58B

Project: Motiva - Monitoring Well and Soil Boring Data Project Location: Delaware City Refinery Project Number: 20240412.W1000 Log of Monitoring Well D58B Sheet 1 of 7 Date(s) Drilled Drilling Method Drill

Feet. Cape May Core #51 Start depth: 240 ft Stop depth: 245 ft Recovery (ft): 5.1 ft Date: 3/21/94 Described by: JVB, KGM, CL. 5.

SAND; medium to fine sand with abundant silt, homogenous slightly mottled appearance; mica on outside, mostly quartz; few darks; peat layer.9 - ft; cnv - same as above; the last few cores are all the same;

Relationships of the Ordovician. Appalachian Basin. June 21, 2011

Regional Stratigraphic and Facies Relationships of the Ordovician Utica/Point i t Pleasant Interval in the Appalachian Basin June 21, 2011 Ron Riley and Mark Baranoski Stratigraphic Correlation Chart Modified

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

The petrography of sandstone samples from the Upper Greensand Formation in southern England.

BRITISH GEOLOGICAL SURVEY TECHNICAL REPORT Stratigraphy Series IR/05/138 The petrography of sandstone samples from the Upper Greensand Formation in southern England. G.K.Lott (British Geological Survey)

GEOL Lab 9 (Carbonate Sedimentary Rocks in Hand Sample and Thin Section)

GEOL 333 - Lab 9 (Carbonate Sedimentary Rocks in Hand Sample and Thin Section) Sedimentary Rock Classification - As we learned last week, sedimentary rock, which forms by accumulation and lithification

Feet CLAY; silty, greenish gray and clayey fine sand; Color: 5Y 3/1

-. CLAY; silty, greenish gray and clayey fine sand; Color: Y /. -. SAND; fine-medium, clayey, with sandy clay layers; very abundant broken thin, tiny shells; shell hash at several horizons, heavily burrowed;

COMMONWEALTH OF VIRGI N IA wll DEPARTMENT OF CONSERVATION AND ECONOMIC DEV ELOPMENT. Bayberry Estates Well #3 TENANT: Mailing Address : _

MAILING ADDRESS, Box 3667 COMMONWEALTH OF VIRGI N IA wll 4 764 cil 9 0 DEPARTMENT OF CONSERVATION AND ECONOMIC DEV ELOPMENT DIVISION OF MINERAL RESOURCES OFFICE ADDRESS, JAMES L. CALVER, COMMISSIONER C'

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

EPS 50 Lab 4: Sedimentary Rocks

Name: EPS 50 Lab 4: Sedimentary Rocks Grotzinger and Jordan, Chapter 5 Introduction In this lab we will classify sedimentary rocks and investigate the relationship between environmental conditions and

Feet. SAND; clayey, fine grained; shells are common; rounded quartz grains. SHELLS; muddy; almost no sand, shells and fragments common

SAND; clayey, fine grained; shells are common; rounded quartz grains SHELLS; muddy; almost no sand, shells and fragments common SAND; back to medium to fine; has a mottled appearance and looks burrowed;

Lecture Outline Wednesday - Friday February 14-16, 2018

Lecture Outline Wednesday - Friday February 14-16, 2018 Quiz 2 scheduled for Friday Feb 23 (Interlude B, Chapters 6,7) Questions? Chapter 6 Pages of the Past: Sedimentary Rocks Key Points for today Be

APPENDIX 3 (IN SITU TEST LOCATION AND CRITERIA FOR SELECTING VIABLE TEST, SAMPLE FIELD AND LABORATORY DESCRIPTION, MINERALOGY AND CHEMISTRY)

APPENDIX 3 (IN SITU TEST LOCATION AND CRITERIA FOR SELECTING VIABLE TEST, SAMPLE FIELD AND LABORATORY DESCRIPTION, MINERALOGY AND CHEMISTRY) IN SITU TEST LOCATION AND CRITERIA FOR SELECTION VIABE TEST

Va Dept. of Hi g hways (DVMR) 399,03Om East 4, 135, 48Om Nor t h. Ke lvi n Rams ey. Columbi a Group. Yor kt own

Count y : James Cit y VDMR We ll # 6033 We l l: Pr oper ty Owner: Driller : Lo cation : 11Chic II Va Dept. of Hi g hways (DVMR 399,03Om East 4, 135, 48Om Nor t h Altitude Top of Hole : Total Depth: Started

1982/20. Supplementary report on sandstones from Linden sandstone quarry, New Norfolk.

1982/20. Supplementary report on sandstones from Linden sandstone quarry, New Norfolk. Abstract D.C. Green Additional thin sections from quarried blocks and X-ray diffraction scans of clays were made from

Your teacher will show you a sample or diagram of each, and show you a settling column. Draw these, and label your diagrams (8 pts) Ungraded:

From Sand to Stone: How do we recognize and interpret sedimentary rocks in the rock record? (Based closely on the University of Washington ESS 101 Lab 5: Sedimentary Rocks) Introduction: This lab consists

Sandstone Petrography

Description of sandstones in thin section In this week's lab, you will learn the basics of the description and interpretation of sandstones in thin section. For each sample, you should describe the grain

Chapter 6 Pages of Earth s Past: Sedimentary Rocks

Chapter 6 Pages of Earth s Past: Sedimentary Rocks Introduction! Drilling into the bottom of the North Sea, we encounter: " Soft mud and loose sand, silt, pebbles, and shells. Then: " Similar materials

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

6. DATA REPORT: HEAVY MINERAL ANALYSIS OF MIOCENE TO PLEISTOCENE SEDIMENTS (HOLES 1071C, 1071F, 1072A, AND 1073A) 1

Christie-Blick, N., Austin, J.A., Jr., and Malone, M.J. (Eds.) Proceedings of the Ocean Drilling Program, Scientific Results Volume 174A 6. DATA REPORT: HEAVY MINERAL ANALYSIS OF MIOCENE TO PLEISTOCENE

WELL LOG. Siltstone - medium gray (N5) - massive, hard, carbonaceous and micaceous on bedding planes.

o o Operator: Farm: Well No: Location: Elevation: Total Depth: Drilling Commenced: Well Completed: Result: United Producing Company, Inc. Yukon Pocahontas Coal Co., Et Al 9-1674 Buchanan County 14,500'

Rock Identification. Aphanitic Texture (fine grained) Individual crystals are so small that they are not visible to the naked eye

The Identification of Rocks This lab introduces the identification of igneous, sedimentary and metamorphic rocks based on mineralogy (composition) and texture. I. Classification of Igneous Rocks Textures

LITHOSTRATIGRAPHIC SERIES / SUBSERIES BENTHIC UNITS NORDLAND GROUP ELPHIDIUM PLEISTO- CENE EXCAVATUM - NONION CUM ASSEM. GYRIODINA SOLDANII

WELL 36/1-2 DEPTH (mrkb) 900 800 700 600 GAMMA RAY Unit: GAPI 0 100 LITHOLOGY LITHOSTRATIGRAPHIC UNITS NORDLAND GROUP HORDALAND GROUP BALD. - SELE SERIES / SUBSERIES PLEISTO- CENE UPPER OLIGOCENE LOWER

Rocks. Rocks are composed of 1 or more minerals. Rocks are classified based on how they formed (origin). 3 classes of rocks:

ROCKS Rocks If a mineral is a naturally occurring homogeneous solid, inorganically formed, with a definite chemical composi:on and a crystalline structure then what is a rock? Rocks Rocks are composed

DIV ISION OF MINERAL R ESOURCES OFFICE A DDRESS, JAMES L. CALV ER, COMMISS IONER COMPLE TION

MAILING ADD RESS, ~. 3667 C,. ottesville, VA 22 903 WATER C OMMONWEALTH OF VIR GIN I A Moili ng Add r ess: REPORT 1221 E. Br oa d Richmond, VA. w#: c#: 443 2 8 2 DEPARTMENT DF CONSERVATION AND E CDNOMIC

How to Identify and Properly Classify Drill Cuttings

How to Identify and Properly Classify Drill Cuttings (Creating Useful Borehole Logs) Dave Larson Hydrogeology and Geophysics Section Accurate information about the borehole location and a careful description

DRA-3a. DISTRIBUTION OF CLAY MINERALS AND CLAY SIZE MATERIAL IN THE QUESTA ROCK PILES AND ANALOG MATERIAL

. DISTRIBUTION OF CLAY MINERALS AND CLAY SIZE MATERIAL IN THE QUESTA ROCK PILES AND ANALOG MATERIAL V.T. McLemore, March 3, 28 1. STATEMENT OF THE PROBLEM What is the difference between clay and clay sized

ENVI.2030L Rock Identification

ENVI.2030L Rock Identification Name I. Introduction The bulk of the earth's crust is composed of relatively few minerals. These can be mixed together, however, to give an endless variety of rocks - aggregates

Marine Sediments EPSS15 Spring 2017 Lab 4

Marine Sediments EPSS15 Spring 2017 Lab 4 Why Sediments? Record of Earth s history - Tectonic plate movement - Past changes in climate - Ancient ocean circulation currents - Cataclysmic events 1 Classification

DRILL HOLE # BH-BGC13-FN-01

DILL HOLE # BH-BGC3-FN-0 Drill Method: Mud otary/coring Depth To ock (m): N/A Page of 7 eviewed by: AJB 0 GAVEL (GW) Fine to coarse, sandy, well graded, dense, max particle size = 30 mm, angular to subrounded,

Geology 229 Engineering Geology. Lecture 6. Basic Rock Classification and Engineering Considerations (West, Chs. 2, 3, 4, 5)

Geology 229 Engineering Geology Lecture 6 Basic Rock Classification and Engineering Considerations (West, Chs. 2, 3, 4, 5) Outline of this Lecture 1. Rock types and rock cycle 2. Geological and engineering

LAB 2 IDENTIFYING MATERIALS FOR MAKING SOILS: ROCK AND PARENT MATERIALS

LAB 2 IDENTIFYING MATERIALS FOR MAKING SOILS: ROCK AND PARENT MATERIALS Learning outcomes The student is able to: 1. understand and identify rocks 2. understand and identify parent materials 3. recognize

I.S : What s in it and the role of the Geologist

Institute of Geologists of Ireland Pyrite Course I.S. 398-1: What s in it and the role of the Geologist Michael L.J. Maher 4 December, 2013 Responsibilities of Geologist You re only the messenger! Classification

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

Guided Notes Rocks & Minerals

Guided Notes Rocks & Minerals is Mineral 1.What is a Mineral Tests 2.Mineral Properties Cycle 3.Rock Rocks 4.Igneous Rocks 5.Sedimentary Rocks 6. Metamorphic Rocks Reference Tables K. Coder 2015 12. What

UNITED CARBON COMPANY GEOLOGICAL DEPARTMENT. VI."M. Ritter"Lumber Company#l-V Serial No. 1461

UNITED CARBON COMPANY GEOLOGICAL DEPARTMENT WELL NO. 0008 VI.M. RitterLumber Company#l-V Serial No. 1461 Drilled by: Location : Elevation l United Carbon Company (United Producing Company, Inc.) 2200'

STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES State Office Building. Port1 and, Oregon OPEN-FILE REPORT

STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1005 State Office Building Port1 and, Oregon 97201 OPEN-FILE REPORT 0-84-5 BENCH TESTING OF SILICA SAND FROM DEPOSITS IN CLATSOP AND MORROW

CEE 437 Lecture 10 Rock Classification. Thomas Doe

CEE 437 Lecture 10 Rock Classification Thomas Doe Igneous Origins Intrusive Batholithic or plutonic: phaneritic Dikes or sills that chill rapidly: aphanitic Extrusive deposition as melt (lava) pyroclastic

Geology 252, Historical Geology, California State University, Los Angeles - professor: Dr. Alessandro Grippo

LAB # 1 - CLASTIC ROCKS Background: - Mechanical and Chemical Weathering - Production of Clastic Sediment - Classification of Sediment according to size: Gravel, Sand, Silt, Clay - Erosion, Transportation

I.S. 398 GEOLOGICAL TESTING PROCEDURES, RESULTS and BACKGROUND

I.S. 398 GEOLOGICAL TESTING PROCEDURES, RESULTS and BACKGROUND EurGeol Dr John Kelly, PGeo, MIMMM, MIQ Engineers Ireland 5 th November 2013 SWELLING RISK BASICS Pyrite is a form of iron sulphide (FeS 2

Chapter I Basic Characteristics of Soils

Chapter I Basic Characteristics of Soils Outline 1. The Nature of Soils (section 1.1 Craig) 2. Soil Texture (section 1.1 Craig) 3. Grain Size and Grain Size Distribution (section 1.2 Craig) 4. Particle

Sandstone Thin-Section Lab

Overview In this week's lab, you will learn the basics of the description and interpretation of sandstones in thin section. For each of the ten samples listed below, you should describe the following:

WELl. LOGS OF THE COASTAL PLAIN OF GEORGIA

GEORGIA STATE DIVISION OF CONSERVATION DEPARTMENT OF MINES. MINING AND GEOLOGY GARLAND PEYTON. Director THE GEOLOGICAL SURVEY Bulletin Number 70 WELl. LOGS OF THE COASTAL PLAIN OF GEORGIA by Stephen M.

I. Uniformitarianism- James Hutton s 2-part theory states: A. The geologic processes now at work were also active in the past B. The present physical

How Earth s Rocks Were Formed I. Uniformitarianism- James Hutton s 2-part theory states: A. The geologic processes now at work were also active in the past B. The present physical features of Earth were

1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite.

1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite. An arrangement of atoms such as the one shown in the diagram determines

Buchanan Well No. 28 Farrn: Zach Justice. Drillers log (0-4815) Well No.: Gamma Ray log (0-1904) Location: Buchanan County

VDMR Well N. 563 Operatr: United Fuel Gas C. Buchanan Well N. 28 Farrn: Zach Justice Drillers lg (0-4815) Well N.: 8848 Gamma Ray lg (0-1904) Lcatin: Buchanan Cunty Sample lg (2031-3009) 11, 150' S f 37

... EVALUATION AND TARGETING OF GEOTHERMAL ENERGY RESOURCES IN THE SOUTHEASTERN UNITED STATES. Progress Report

,i i w.. i i i i, t'... VP&SU 78ET 27001 7 EVALUATON AND TARGETNG OF GEOTHERMAL ENERGY RESOURCES N THE SOUTHEASTERN UNTED STATES Progress Report John K. Costain Lynn Glover and A. Krishna Sinha Principal

Exercise 3 Texture of siliciclastic sediments

Exercise 3 Texture of siliciclastic sediments Siliciclastic sediments are derived from the weathering and erosion of preexisting rocks. Once a sedimentary particle is loosened from its parent rock, it

2. What is sample 1B? a. chalcopyrite b. plagioclase feldspar c. muscovite d. copper e. magnetite f. galena g. pyrite

HSAG Mineral and Rock Exam 2014 Note: Most sample numbers do NOT match question numbers so be careful. Team: 1. What is sample 1A? a. magnetite b. galena c. pyrite d. chalcopyrite e. copper f. graphite

GEOLOGICAL RECORD. ANR Production Co. #1 VICC N E WI 215-F Wise County, Virginia

Wise County, Virginia Drilling Contractor. Spud. Drilling Completed. Elevation I Record By..Casings Falcon Drilling Co, February 24, 1982 March 18,.1982 Gr 2246.25.' RF 2256.25' Kll 2257.75' Paul Mescher.

A. IGNEOUS Rocks formed by cooling and hardening of hot molten rock called magma (within crust or at its surface).

EARTH SCIENCE 11 CHAPTER 5 NOTES KEY How Earth's Rocks Were Formed Early geologists believed that the physical features of the Earth were formed by sudden spectacular events called CATASTROPHES. Modern

Review - Unit 2 - Rocks and Minerals

Review - Unit 2 - Rocks and Minerals Base your answers to questions 1 and 2 on the diagram below, which shows the results of three different physical tests, A, B, and C, that were performed on a mineral.

(Refer Slide Time: 1:25)

Earth Sciences for Civil Engineering Professor Javed N Malik Department of Earth Sciences Indian Institute of Technology Kanpur Module 2 Lecture No 10 Rock types and their Properties (Part-4) So welcome

& $ CORED mbsf SITE 932 HOLE A. Graphic Lith. Section Age. Sample. Disturb. Meter. Color. Description. Structure. CALCAREOUS CLAY and CLAY

SITE 932 HOLE A Meter 1_ 2_ 3_ 4_ 5_ 6 : 3 α IV.V.V a πt = π 4..-.V. Section Age 1 2 3 4 CC late Pleistocene \ Holocene CORE & & $ Disturb 1H Sample S S S S I M Color 1YR 5/3 2. 4/2 4/1 CORED.-6. mbsf

Geology for Engineers Rocks

89.325 Geology for Engineers Rocks Name I. Introduction The bulk of the earth's crust is composed of relatively few minerals. These can be mixed together, however, to give an endless variety of rocks -

There is a close connection between Geology and Architecture: The Study of Geology is particularly appropriate for the

Stone Identification There is a close connection between Geology and Architecture: The Study of Geology is particularly appropriate for the architect, who, in applying the various materials of the Earth

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

GEOL.3250 Geology for Engineers Sedimentary & Metamorphic Rocks

GEOL.3250 Geology for Engineers Sedimentary & Metamorphic Rocks Name I. Introduction The bulk of the earth's crust is composed of relatively few minerals. These can be mixed together, however, to give