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

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

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

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

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

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

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

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

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

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

u. S. Geological Survey,

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

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

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

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

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

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

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

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

Log of Monitoring Well D58B

o _10 10 _ eo

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

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

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

Sedimentation & Stratigraphy. Lab 3: Heavy Mineral Analysis Using the Franz Magnetic Separator

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

SOUTH CERRO AZUL STRATIGRAPHIC SECTION. Upper Cerro Azul flow of the Servilleta Basalt (Tsbcau) Lower Sandlin unit (Tsl)

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

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.

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


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

Appendix 3. Sample Descriptions

Sandstone Petrography

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:

Physical Geology 101 Laboratory MINERALS II Silicate and Carbonate Rock-Forming Minerals

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

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

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

Chapter - IV PETROGRAPHY. Petrographic studies are an integral part of any structural or petrological studies in

SOME STAGES IN THE DISINTEGRATION OF GLAUCONITE Baw;eurN Grltrnslnrva, U niaer si,ty of V ir ginia.

INTER VAL SHEET. From-To Elevation in feet

Lab 4: Mineral Identification April 14, 2009

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

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

APPENDIX III. COMPOSITION AND SOURCE OF DETRITAL SAND LAYERS FROM THE GUAYMAS BASIN 1

ENVI.2030L Rock Identification

GY 402 Sedimentary Petrology (2016) Mature Siliciclastic Sedimentary Rock Thin-sections

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

Paleo Lab #4 - Sedimentary Environments

Sedimentology & Stratigraphy. Thanks to Rob Viens for slides

u. S. Highway 1 1/4 south

ANNEX VIII: APPENDIX E MINERALOGY RESULTS

Weathering and Clast Production Geol 113

REMARKS. NANNOFOSSIL CLAYSTONE, CLAYSTONE, and CALCAREOUS SANDY SILTSTONE

32. GEOCHEMISTRY OF CARBON: DSDPLEG31

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

Sediment and sedimentary rocks Sediment

N o s ample

1. Gravel-size 2. Sand-size 3. Silt-size 4. Clay-size 5. Microcrystalline 6. Macrocrystalline

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

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

SYENITE, IJOLITE, CARBONATITE, ULTRAMAFIC ROCKS AND LAMPROPHYRE

SEDIMENTOLOGY AND STRATIGRAPHY: processes, environments and deposits

Geology for Engineers Rocks

Igneous Rocks. Sedimentary Rocks. Metamorphic Rocks

or & J Enterprises J E. G. Taylor

ALLEGHENY COLLEGE DEPARTMENT OF GEOLOGY STUDENT HANDBOOK

Review - Unit 2 - Rocks and Minerals

DIAMOND DRILLING. CLAIM No, HOLE No, FOOTAGE DATE NOTE. NOTES: (i) # ios- 80 WORK PERFORMED BY: ASARCO EXPLORATION OF CANADA LIMITED

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

Petrographic Investigation of Two Float Samples from the Goldstake Property, Northern Ontario. Prepared for: Mr. Robert Dillman

Rocks and the Rock Cycle notes from the textbook, integrated with original contributions

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

Sedimentary Environments Chapter 8

DIV I SION OF MI NERAL RESOURCES OFFICE ADDRESS,

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

Lab 6 - Identification of Metamorphic Rocks

GY 402: Sedimentary Petrology

9. SEDIMENTARY ROCKS OF THE JAN-MAYEN RIDGE

Rock Identification. invisible rhyolite andesite basalt komatiite. visible granite diorite gabbro peridotite

ROCK CLASSIFICATION AND IDENTIFICATION

Minerals and Rocks Chapter 20

EPS 50 Lab 4: Sedimentary Rocks

Sedimentary and Metamorphic Rocks: Interpreting Ancient Environments of Painted Canyon (Lab 2)

Emily and Megan. Earth System Science. Elements of Earth by weight. Crust Elements, by weight. Minerals. Made of atoms Earth is mostly iron, by weight

Date Submitted: June General Nature of Report: Examination of Placer Samples

Table DR 1: Description of the lithologic succession encountered by the Enkingen (SUBO 18) drill core.

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

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

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

EFFECTS OF DIKES AND DISPLACEMENT MOVEMENTS ON SEDIMENTS IN CAPITAN QUADRANGLE, NEW MEXICO

SAMPLE: Peak List: Pos. [ 2Th.] Rel. Int. [%] FWHM [ 2Th.] d-spacing [Å] Height [cts]

UmllluIfiW, SfOLOGICAL SURVEY

WELl. LOGS OF THE COASTAL PLAIN OF GEORGIA

A Study Guide for Learning. Rock Identification. Geology Department Green River Community College

INTER VAL SHEET. Date rec 'd: 8 / 7 / 67 Sample In te r val: f r om 0 to : 2 90 '

CUTTINGS SUMMARY FOR THE MINNESOTA DEPARTMENT OF NATURAL RESOURCES SOUTH-CENTRAL DRILLING PROGRAM

Crust Elements. Elements of Earth. Minerals. Crystals. Interconnected Rocks and minerals Interior processes Erosion and deposition Water and air

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

Transcription:

() 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 greenish cast ("salt- and- pepper" sand); slightly argillaceous and silty; medium-grained, moderately sorted; pelletal, fresh black glauconite (about 50%) and clear to green-stained, subangular to subrounded quartz (about 50%); accessory mineral suite includes undetermined amounts of magnetite, micas, orange and pink garnet, brown, and green epidote, pyrite in fine-grained lumps and in massive tubular forms, tourmaline, zircon; moderate amount abraded, chalky pelecypod fragments; foraminifera moderately abundant (Robulus and Nonion). Sand - gray ("salt- and- pepper" sand); slightly argillaceous and silty; fine- grained, moderately sorted; pelletal, fresh black glauconite (30-40%) and angular to subangular, clear to green-stained quartz (60-70%); small amounts yellowish, partially altered microcline and dark-green biotite; accessory mineral suite includes magnetite, garnet, muscovite, zircon, and pyrito- carbonaceous material; scattered, chalky pelecypod fragment and a few foraminifera. Mattaponi Formation (?) (300-840') () 300-315 310-315 Sand - brown; slightly argillaceous; medium- to coarse-grained, moderately sorted, subangular; quartz with about 10% glauconite; small amounts feldspar, magnetite, garnet, and greenish mus covite; scattered, chalky pelecypod fragments and foraminifera. Sand - reddish-brown; coarse- to very-coarse-grained, wellsorted, subangular to subrounded; quartz with 5-15% slightly altered microcline and microperthite and 5% fresh, fine- grained glauconite; partial coatings of hematite on much of the quartz and feldspar; accessory minerals include magnetite, muscovite, and a little goethite and garnet.

C) (J ej 315-330 330-345 345-360 360-375 375-390 390-405 405-420 420-435 435-450 450-465 465-480 - 2 - Sand - reddish-brown; medium- to coarse-grained, moderately sorted, subangular to subrounded; quartz with 5-10% slightly altered alkaline feldspar and up to 5% fine- to medium- grained, fresh glauconite; partial coatings of hematite common; small amounts magnetite, muscovite and iron oxides. Sand - brown; very-fine- to very-coarse-grained, poorly sorted, subangular; arkosic quartz sand with small percentage finegrained glauconite and trace of muscovite and magnetite; some hematite present as coatings on grains. Sand - brown; moderately silty; very-fine- to coarse-grained, moderately sorted (skewed fine), angular to subangular; quartz with 5% white feldspar and 5% fresh greenish-black glauconite; traces of magnetite, pyrite, muscovite; a few pelecypod shell fragments. Sand - brown; moderately argillaceou s and slightly silty; fineto coarse-grained, rather poorly sorted, angular to s ubr ourried; slightly arkosic quartz sand with 5-10% fresh, greenish-black glauconite; traces of magnetite, muscovite, earthy hematite; small amount abraded chalky shell fragments, and a few foraminifera fragments. Sand - brown; moderately argillaceous and silty; mediumto coarse-grained, fairly well sorted, subangular; slightly arkosic quartz sand with 10-20% fresh, greenish-black glauconite; small amounts magnetite, hematite, muscovite; scattered chalky shell fragments and a few foraminifera. No sample. Sand - brown; moderately argillaceous and silty; fine- to coarsegrained, moderately sorted, angular to subangular; slightly arkosic quartz sand with about 5% fresh, greenish-black glauconite; small amounts magnetite, hematite, muscovite; scattered chalky shell fragments and a few foraminifera. but with considerable very-coarse-grained sand, more poorly sorted, and with a trace of phosphorite. Sand - brown; moderately argillaceous and slightly silty; veryfine- to coarse-grained, rather poorly sorted, angular to subrounded; slightly arkosic and glauconitic quartz sand; earthy hematite relatively abundant; a few foraminifera.

- 3 - C) 480-495 Sand - brown; moderately argillaceous and slightly silty; very-fine- to coarse- grained, rather poorly sorted, angular to subrounded; slightly arkosic and glauconitic quartz sand; earthy hematite relatively abundant; a few foraminifera. B;3.yber:ryEstates 495-510 but more argillaceous, less glauconitic. 510-525 Sand - brown; argillaceous (variegated clay), and slightly silty; medium- to coarse-grained, moderately sorted, subangular; slightly arkosic (microcline) quartz sand with about 5% fresh glauconite; abundant earthy hematite (clay fraction?); small amounts magnetite, white chert, muscovite; a few chalky shell fragments and poorly preserved foraminifera. 525-540 but much more argillaceous. 540-555 Clay -brown (variegated under microscope); sandy, glauconitic; earthy hematite (clay fraction?) abundant; small amounts feldspar, white chert, and magnetite; a few chalky shell fragments. 555-570 (J 570-585 585-600 600-615 615-630 630-645 but darker includes Robulus. colored, sandier; sparse fossil assemblage 645-660 660-675 675-690 690-705 Sand - brown; argillaceous (variegated clay); very-fine- to verycoarse-grained, poorly sorted, subangular; quartz sand with about 5% fresh, greenish-black glauconite; earthy iron oxides abundant; trace of chalky shell debris. Sand - brown; slightly to moderately argillaceous; medium- to coarse-grained, moderately sorted, subangular; quartz sand with about 10% gray to white microcline and microperthite, and 1-2% glauconite, small amount earthy hematite; a few chalky shell fragments.

() 705-720 - 4 - Sand - brown; slightly to moderately argillaceous; medium- to coarse-grained, moderately sorted, subangular; quartz sand with about 100/0 gray to white microcline and microperthite, and 1-20/0 glauconite, small amount earthy hematite; a few chalky shell fragments. 720-735 but more argillaceous (relatively drab brown clay). 735-750 Sand - brown; slightly argillaceous; fine- to coarse-grained, moderately sorted, angular to subangular; quartz sand with about 100/0 gray to white microcline and about 100/0 glauconite; small amounts earthy hematite, magnetite; scattered chalky shell fragments. 750-765 but coarser grained. cj 765-780 780-795 795-810 810-825 825-840 Sand - brown; slightly argillaceous; fine- to coarse-grained, rather poorly sorted, subangular; slightly arkosic, slightly glauconitic quartz sand; small amount earthy hematite and trace of muscovite; small amount chalky pelecypod shell fragments. Sand - brown; argillaceous; fine- to coarse-grained, rather poorly sorted, subangular; quartz sand with about 50/0 white microcline and 10/0 fresh glauconite; trace of muscovite; scattered chalky pelecypod shell fragments, and a few foraminifera. Potomac Group (840-1005') (.~ 840-855 855-870 870-885 885-900 Sand - buff; slightly argillaceous; medium-grained, well-sorted, angular; arkosic (about 100/0 fresh, white rriicrocline) and small amounts of fresh glauconite, magnetite; and earthy hematite; trace of pyrite. Sand - brown; moderately argillaceous and silty; medium- to coarse-grained, rather poorly sorted, subangular; quartz sand with about 50/0 each of feldspar and glauconite; small amount earthy hematite; traces of muscovite and magnetite; scattered chalky pelecypod shell fragments.

- 5-900-915 915-930 930-945 945-960 Sand - brown; argillaceous (variegated clay) and silty; mediumto coarse-grained, rather poorly sorted, subangular; quartz sand with about 50/0 each of feldspar and glauconite; small amount earthy hematite; traces of muscovite and magnetite; scattered chalky pelecypod shell fragments. Sand - brown; argillaceous; poorly sorted and variably rounded; slightly arkosic and glauconitic; small amount earthy hematite; traces of mica and platey black phosphorite; scattered chalky shell fragments, and a few foraminifera. Sand - buff; medium- to coarse-grained, well-sorted, subangular; clean quartz sand with about 50/0 fresh white microcline and small amounts of earthy hematite, magnetite, and fine- to mediumgrained greenish-black glauconite. Sand - brown; slightly argillaceous; medium- to coarse-grained, fairly well sorted, subangular; quartz sand with about 50/0 fresh white microcline and small amount of fine- grained glauconite; trace of muscovite; trace of chalky shell debris. 960-975 but with less feldspar and only a few grains of glauconite. 975-990 990-1005 1005-1050 Sand - gray, with violet cast; medium- to coarse-grained, well-sorted, subangular; moderately arkosic clean quartz sand with a few grains of glauconite and trace of brown epidote. No sample. GEOLOGIC SUMMARY 0-240 240-300 300-840 840-1005 1005- losh ROCK UNIT No sample Aquia Formation Mattaponi Formation (?) Potomac Group No sample TIME ROCK UNIT Eocene Upper Cretaceous- Paleocene Lower Cretaceous (J Virginia Division of Mineral Resources Robert H. TeHke, Geologist May 21, 1965