Taseko Prosperity Gold-Copper Project. Appendix 3-7-H

Size: px
Start display at page:

Download "Taseko Prosperity Gold-Copper Project. Appendix 3-7-H"

Transcription

1 Taseko Prosperity Gold-Copper Project Appendix 3-7-H

2 Appendix 7H Phase 5 Overburden Samples 7H-1 Phase 5 Overburden Sample Sources Testpit Easting Northing Elevation Depth (UTM NAD83) (UTM NAD83) (UTM NAD83) 7AT 456,343 5,701, BT 456,420 5,701, CT 456,479 5,701, Drill Hole Easting Northing Elevation Depth (UTM NAD83) (UTM NAD83) (UTM NAD83) ,369 5,701, Taseko Mines Limited July 2008

3

4

5

6

7 Prosperity GEOLOGY LOG LITHOLOGY MINERALIZATION Code Description Code Description Code Description OVERBURDEN LATE CRETACEOUS INTRUSIVE COMPLEX anh Anhydrite FILL Rock Fill PMPD Post Mineralization Porphyritic Diorite bn Bornite CASE Casing QFP Quartz Feldspar Porphyry - aphanitic cal Calcite TRIC Triconed Bedrock, no recovery QD3 Quartz Diorite - equigranular to subporphyritic cb Carbonate OVB1 Overburden, mostly till QD2 Quartz Diorite - coarse seriate porphyritic cc Chalcocite QD1 Quartz Diorite - heterogeneous fine porphyritic cpy Chalcopyrite QUATERNARY COVER cup Cuprite Pleistocene Glacial Till SEDS Mudstone, Siltstone, Sandstone, and Conglomerate ep Epidote CRETACEOUS SEDIMENTARY ROCKS cu Native Copper TILB Basal Till CRETACEOUS VOLCANIC ROCKS gyp Gypsum CLAYU Clay SUBV Crowded Porphyritic Andesite hem Hematite SICLU Silt/Clay Till FLOW Porphyritic Andesite Flow lim Limonite SILTU Silt BEAT Laminated Andesite Tuff mag Magnetite GRAVU Gravel DEBF Andesite Lapilli Tuff and Debris Flow mol Molybdonite TERTIARY COVER MAT Andesite Tuff - ash tuff pbzn Lead, Zinc Miocene to Pliocene Basalt Flows FAXT Andesite Tuff - crystal tuff po Pyrrhotite py Pyrite BSLT Basalt Flow, vesicular ALTERATION qz Quartz OVB2 Overburden, below BSLT, OVB1 Code Abbreviations sp Sphalerite NON Weakly altered ten Tenorite Colluvium BIO K-Silicate titn Tetra-Tenn FANL Fanglomerate (Limonitic) KSP Orthoclase to Tourmaline FAN Fanglomerate SER Sericite-Ankerite Glacial Lacustrine Sediments QTZ Silicification GRAV Gravel PRO Propylitic SICL Silt/Clay Mix PHY Phyllic CLAY Clay ARG Argillic SILT Silt ALB Albite STRUCTURE INTENSITY Code Description Code Description Code Description bed Bedding brx Broken Zone T Trace cren Crenulations dyke Mini Dyke <5m W Weak fold Folded frac Fractured M Moderate gc Ground Core gg Gouge S Strong Hole ID Page 1 of 4 DRILL HOLE INFORMATION Coordinate System Easting Northing Elevation MINE GRID Collar Azimuth Collar Dip Planned Depth Final Depth Overburden (m) Casing (ft) Tricone (ft) 0.00 Down-hole Survey Data Depth (m) Azimuth Inclination Method Drilling Data Bit Size From To Length HQ Professional/Technician Data Person Start Date End Date Collar Survey Drill Contractor Geology By PT Geotechnical Log PT Specific Gravity Casing Cemented Plugged Rehab. Pad in / out yes / no yes / no yes / no Degree of Success of Drilling 26-Nov-07 replitho_fulllog:report HUNTER Responsible DICKINSON Mineral INC. Development

8 Prosperity GEOLOGY LOG Log by Peter Tipple Peter Tipple Date 17-Nov-07 Hole ID Page 2 of 4 I N T E R V A L (ft) From To Overburden, not sampled. Rock Code OVB1 Poorly sorted overburden unit with combination of 20% ground cobbles. 60% black-dark grey poorly graded sand. 20% 1-2cm pebbles. Sharp transtion into dark grey stiff clay unit CLAYU Dark grey stiff homogenous clay unit. Scaly microfracture polygonal exfoliation which develops into a consistent 55TCA bedding cleavage in last 1m of unit. Embedded 30% clay supported 3-50mm predominantly subrounded light grey heterolithic gravel in uppermost 8.85m. Embedded 25% clay supported black 2-40mm angular to subrouded basaltic heterolithic gravel in last 0.68m of unit. Sharp transition into unconsolidated basal till interval with mostly black basaltic gravelly sand/silty sand with heterolithic size pebbles/gravel TILB Basal till interval with poorly consolidated (mostly black) also lightdark grey-orange-brown gravelly sand/silty sand with heterolithic size pebbles/gravel. ~60% coarse grained black sand. 35% black-grey 2-30mm subrounded heterolithic gravel. 5% black silty-sand. Sharp transition into generally cohesive clay matrix supported silty sand/gravel with intervals of unconsolidated sand and gravel SICLU Cohesive black soft clay/silt matrix 26-Nov-07 I N T E R V A L From To A L T E R A T I O N Major Minor 1 M I N E R A L I Z A T I O N % % % % S T R U C T U R E No sampling from 0-4.1m Major CA Minor Comments Clay matrix supported subunit with 30% embedded 3-50mm subrounded fine to coarse gravel lithofragments Narrowly spaced homogeneous bedding cleavage of 55TCA with 2mm spacing bed S 55 Embedded 25% clay/silt matrix supported black 2-40mm angular to subrouded gravel sized basalt lithofragments replitho_fulllog:report HUNTER Responsible DICKINSON Mineral INC. Development

9 Prosperity GEOLOGY LOG Log by Peter Tipple Peter Tipple Date 17-Nov-07 Hole ID Page 3 of 4 I N T E R V A L (ft) From To Rock Code supported till with embedded 10% <2mm-3mm coarse sand and small sized gravel. Sharp transition into fairly homogeneous black sandy/silt till which exhibits poor cohesion with little clay cementation. Minor amounts of 2-5mm black-grey-brown heterolithic gravel SILTU Fairly homogeneous black basalt framework supported silty-sand till which exhibits poor cohesion due to absence of clay cementation. Most core recovery exhibits slumping of sediments with occasional 20cm intervals of weakly cohesive sand/silt. 80% subrounded-angular fine-grained to coarse grained sand. 10% 2-5mm black-grey-brown heterolithic gravel. 10% silt/clay. Sharp transition into stiff-very stiff cohesive homogeneous black clay unit CLAYU stiff-very stiff cohesive homogeneous black clay unit. No heterolithic embedded sediments. Moderately spaced dominant 55TCA bedding cleavage occurring every ~5cm. Transition into pooly consolidated black-brown-grey fine-coarse grained sand and gravel TILB Very poorly consolidated black-greybrown heterolithic fragments from coarse grained sand/gravel with little clay cemetation. 60% 2-30mm angular-subrounded black-brown-grey gravel. 35% fine-coarse grained sand. 5% silt/clay. Transition into interval with total lost 26-Nov-07 I N T E R V A L A L T E R A T I O N Major Minor 1 M I N E R A L I Z A T I O N % % % % S T R U C T U R E Major CA Minor Comments From To erval of unconsolidated black-grey <2mm-40mm coarse sand and gravel. 50cm of lost recovery with ground 41.76m bed S replitho_fulllog:report HUNTER Responsible DICKINSON Mineral INC. Development

10 Prosperity GEOLOGY LOG Log by Peter Tipple Peter Tipple Date 17-Nov-07 Hole ID Page 4 of 4 I N T E R V A L (ft) From To Rock Code recovery and ground lithofragments from cave in TRIC I N T E R V A L From To A L T E R A T I O N Major Minor 1 M I N E R A L I Z A T I O N % % % % S T R U C T U R E Major Minor CA Comments Total lost recovery with ground lithofragments from drill hole cave in. Transition into highly cohesive matrix supported conglomerate with angularsubrounded heterolithic gravel of highly diverse composition SEDS Matrix supported conglomerate unit with variable 20-70% subrounded heterolithic 2-20mm brown-grey-blackpurple-orange pebbles/gravel. Matrix is composed of 30-80%black-dark grey clay. Conglomerate unit is fairly cohesive but exhibits low strength m. 26-Nov-07 replitho_fulllog:report HUNTER Responsible DICKINSON Mineral INC. Development

Drill locations for the 2015 program are highlighted in the geology map below.

Drill locations for the 2015 program are highlighted in the geology map below. 2015 Exploration Program The exploration program plan at KSM for 2015 was designed to improve the understanding of block cave targets and support engineering/environmental aspects of development scenarios.

More information

LITHOLOGY REPORT - Detailed -

LITHOLOGY REPORT - Detailed - (m) (m) Lithology Sample # Length 50 0.00 11.76 10 Casing Minor Interval: 0.00 0.54 10A Casing above ground (Air) 0.54 11.76 10G Casing through gravel or overburden (Ground) 11.76 40.80 1c Interbedded

More information

DISCOVERY OF MINERALISED PORPHYRY & MAGNETITE-COPPER-GOLD AT KAMARANGAN

DISCOVERY OF MINERALISED PORPHYRY & MAGNETITE-COPPER-GOLD AT KAMARANGAN MEDUSA MINING LIMITED ABN: 60 099 377 849 Unit 7, 11 Preston Street Como WA 6152 PO Box 860 Canning Bridge WA 6153 Telephone: +618-9367 0601 Facsimile: +618-9367 0602 Email: admin@medusamining.com.au Internet:

More information

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

APPENDIX III. COMPOSITION AND SOURCE OF DETRITAL SAND LAYERS FROM THE GUAYMAS BASIN 1 APPENDIX III. COMPOSITION AND SOURCE OF DETRITAL SAND LAYERS FROM THE GUAYMAS BASIN J. Eduardo Aguayo> instituto Mexicano del Petróleo, Mexico, D.F., Mexico QAL 0 After: Geological chart, Instituto de

More information

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

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;

More information

Notes: Note. Township of GODSON Report NQ: 12. Diamond Dniiing. Hole NQ Footage Date. July/56. July/56. Aug/56. Aug/56. Claim NQ 487' K ' l-a

Notes: Note. Township of GODSON Report NQ: 12. Diamond Dniiing. Hole NQ Footage Date. July/56. July/56. Aug/56. Aug/56. Claim NQ 487' K ' l-a Diamond Dniiing S2F«4NW«194 12 GODSON 010 Township of GODSON Report NQ: 12 Work performed by: KENNCO EXPLORATIONS (CANADA) LTD. Claim NQ Hole NQ Footage Date Note K 25434 l 487' July/56 l-a 48' July/56

More information

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

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

More information

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

SOUTH CERRO AZUL STRATIGRAPHIC SECTION. Upper Cerro Azul flow of the Servilleta Basalt (Tsbcau) Lower Sandlin unit (Tsl) Figure A3-01 cobbles claysilt general grain size sand pebbles vf f m c vc SOUTH CERRO AZUL STRATIGRAPHIC SECTION Top at 18 m. Upper Cerro Azul flow of the Servilleta Basalt (Tsbcau) 15 Basalt: Very dark

More information

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

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

More information

Hydro One (Sept 2014) Hydro One (Sept 2014) Hydro One (Sept 2014)

Hydro One (Sept 2014) Hydro One (Sept 2014) Hydro One (Sept 2014) TABLE 1 WELL CONSTRUCTION DETAILS MOE WWR No Well ID Location Installation Date Status Easting Coordinates Northing Source Elevation Screened Interval Screened Material Borehole Well Stick-up Ground Top

More information

COMPOSITIONAL TERMS: FELSIC : light colored INTERMEDIATE : medium shades MAFIC : dark colored ULTRAMAFIC : rare (composition of the mantle)

COMPOSITIONAL TERMS: FELSIC : light colored INTERMEDIATE : medium shades MAFIC : dark colored ULTRAMAFIC : rare (composition of the mantle) GEOLOGY 306 Laboratory NAME: Instructor: TERRY J. BOROUGHS SECTION: Common Rocks (Chapter 2) For this assignment, you will require: a streak plate, glass plate, magnet, dilute hydrochloric (HCl) acid,

More information

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

Rock Identification. invisible rhyolite andesite basalt komatiite. visible granite diorite gabbro peridotite Rock Identification The samples in this lab are arranged into four groups: igneous, sedimentary, metamorphic, and unknown. Study the igneous, sedimentary, and metamorphic collections to get an idea of

More information

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

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

More information

EPS 50 Lab 4: Sedimentary Rocks

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

More information

CEE 437 Lecture 10 Rock Classification. Thomas Doe

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

More information

Sediment and sedimentary rocks Sediment

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

More information

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.

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;

More information

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

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')

More information

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

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,

More information

IOCG Style Alteration of the Amargosa Prospect Baja California Norte, Mexico

IOCG Style Alteration of the Amargosa Prospect Baja California Norte, Mexico IOCG Style Alteration of the Amargosa Prospect Baja California Norte, Mexico MacIntyre, T., Eckberg, E., Morgan, C., Enns, S., Cruise, M., & Hitzman, M. GSA 2005 Salt Lake City, Utah Outline Location Methods

More information

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) 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

More information

-/ttr- Hor. - ill 86 A. II II II 111 li 111 DIAMOND DRILL CORE LOGGING SHEETS 9. Ol^**a. ILJJ If ^ /^jjg^jrs c DESCRIPTION ^~"~ ~.

-/ttr- Hor. - ill 86 A. II II II 111 li 111 DIAMOND DRILL CORE LOGGING SHEETS 9. Ol^**a. ILJJ If ^ /^jjg^jrs c DESCRIPTION ^~~ ~. DIAMOND DRILL CORE LOGGING SHEETS 9 86 A PROPERTY: Solarus HOLE NO.: KL-04-01 LOCATION: Longlac LENGTH: 354.8 m PROJECT NUMBER: NORTHING: 1+40N ELEVATION: 0 UTM northing: 5514255 COLLAR ORIENTATION (AZIMUTH

More information

Lab 2: Rocks Page 1 of 8

Lab 2: Rocks Page 1 of 8 Lab 2: Rocks Page 1 of 8 LAB 2: ROCK IDENTIFICATION DUE: Friday, Feb. 25 Directions About 90 rocks specimens will be on tables in the classroom. The rocks will be arranged on the lab tables during class,

More information

Practice Test Rocks and Minerals. Name. Page 1

Practice Test Rocks and Minerals. Name. Page 1 Name Practice Test Rocks and Minerals 1. Which rock would be the best source of the mineral garnet? A) basalt B) limestone C) schist D) slate 2. Which mineral is mined for its iron content? A) hematite

More information

QQQ-4 QQQ-3. Apr/78 Apr/78. Diamond Drilling. Claim N9 Hole NO Footage Date Note P ,0' P ' (2) Notes: (1) #132-78

QQQ-4 QQQ-3. Apr/78 Apr/78. Diamond Drilling. Claim N9 Hole NO Footage Date Note P ,0' P ' (2) Notes: (1) #132-78 Diamond Drilling 42B01SE0018 22 PENHORWOOD 010 Township of PENHORWOOD Report NO 22 Work performed by: Geophysical Engineering Limited Claim N9 Hole NO Footage Date Note P 504953 P 504938 QQQ-4 QQQ-3 220,0'

More information

DRILL HOLE # BH-BGC13-FN-01

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,

More information

A Sedimentary Rock is..

A Sedimentary Rock is.. Sedimentary Rocks A Sedimentary Rock is.. rock formed from the lithification or crystallization of: 1. Minerals in solution 2. Organic remains 3. Materials produced by living things (biochemical) 4. Clastic

More information

TECK EXPLORATION LTD DIAMOND DRILL LOG

TECK EXPLORATION LTD DIAMOND DRILL LOG Hole ST97-1 Sheet 1 of 8 42D9NW24 2.19129 PIC TECK EXPLORATION LTD. 1 DIAMOND DRILL LOG Job 163 H.T.S. 42 D/9 Property wnship. Claim No. Stenlund Pic wnship 18629/18622 Location: Line 923E.. Station 77N

More information

GEOLOGY AND LITHOGEOCHEMISTRY OF THE CHILKO-TASEKO LAKES AREA* BY G.

GEOLOGY AND LITHOGEOCHEMISTRY OF THE CHILKO-TASEKO LAKES AREA* BY G. B Ministry of Energy, Mines and Petroleum Resources GEOLOGICAL BRANCH MINERAL RESOURCES DIVISION NOTES TO ACCOMPANY OPEN FILE - GEOLOGY AND LITHOGEOCHEMISTRY OF THE CHILKO-TASEKO LAKES AREA* BY G. P. McLAREN

More information

Mud Sand Gravel. Clastic Textures

Mud Sand Gravel. Clastic Textures Sed Rocks Self-Instruction Lab Name Geology 100 Harbor Section Please see the questions online before you begin. Sedimentary rocks are usually identified in the field by their stratification or layering,

More information

COPPERSTONE RESOURCES AB INTERCEPTS ZONE OF CHALCOPYRITE-ARSENOPYRITE- BORNITE MINERALIZATION AT SVARTLIDEN IN FIRST DEEP DRILLHOLE FROM 720m-810m

COPPERSTONE RESOURCES AB INTERCEPTS ZONE OF CHALCOPYRITE-ARSENOPYRITE- BORNITE MINERALIZATION AT SVARTLIDEN IN FIRST DEEP DRILLHOLE FROM 720m-810m COPPERSTONE RESOURCES AB INTERCEPTS ZONE OF CHALCOPYRITE-ARSENOPYRITE- BORNITE MINERALIZATION AT SVARTLIDEN IN FIRST DEEP DRILLHOLE FROM 720m-810m In mid-january 2017 Copperstone Resource published a geological

More information

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

DIAMOND DRILLING. CLAIM No, HOLE No, FOOTAGE DATE NOTE. NOTES: (i) # ios- 80 WORK PERFORMED BY: ASARCO EXPLORATION OF CANADA LIMITED DIAMOND DRILLING 52A15NE8006 11 WOLF LAKE 010 AREA! WOLF LAKE REPORT No,: WORK PERFORMED BY: ASARCO EXPLORATION OF CANADA LIMITED CLAIM No, HOLE No, FOOTAGE DATE NOTE TB 49585H TB 495874 WR l WR 2 587.0

More information

Engineering Geology. Igneous rocks. Hussien Al - deeky

Engineering Geology. Igneous rocks. Hussien Al - deeky Igneous rocks Hussien Al - deeky 1 The Geology Definition of Rocks In Geology Rock is defined as the solid material forming the outer rocky shell or crust of the earth. There are three major groups of

More information

SECOND DRILL HOLE IHAD2 INTERSECTS MINERALIZED TAPLEY HILL FORMATION AND MINERALIZED BASEMENT IRON FORMATION

SECOND DRILL HOLE IHAD2 INTERSECTS MINERALIZED TAPLEY HILL FORMATION AND MINERALIZED BASEMENT IRON FORMATION Suite 304, 22 St Kilda Road St Kilda Vic 3182 Ph: +61 3 9692 7222; Fax: +61 3 9529 8057 For Immediate Release 14 th September 2007 SECOND DRILL HOLE IHAD2 INTERSECTS MINERALIZED TAPLEY HILL FORMATION AND

More information

I m good. Thank you.

I m good. Thank you. I m good. Thank you. The Rock Cycle Ag Earth Science Chapter 3.1 A natural occurring, inorganic crystalline material with a unique chemical composition. mineral A consolidated mixture of minerals rock

More information

Cowal Gold Corridor Opening Other Doors

Cowal Gold Corridor Opening Other Doors Cowal Gold Corridor Opening Other Doors 1 Objectives The Doors of the Corridor local geology of Cowal Gold Corridor Styles and controls on mineralisation within the Corridor Vein paragenesis Summary of

More information

Geology, Alteration and. Petrogenesis

Geology, Alteration and. Petrogenesis The Mutooroo Copper Deposit: Geology, Alteration and Petrogenesis Graham S. Teale Consultant t Andrew T. Price Havilah Resources NL The speaker would like to thank Havilah Resources NL for the opportunity

More information

Mud Sand Gravel. Clastic Textures

Mud Sand Gravel. Clastic Textures Sed Rocks Self-Instruction Lab Name Geology 100 Harbor Section Read the sedimentary rocks chapter before you start. Sedimentary rocks are usually identified in the field by their stratification or layering,

More information

Lecture Outline Wednesday - Friday February 14-16, 2018

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

More information

Geology for Engineers Rocks

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 -

More information

Which sample best shows the physical properties normally associated with regional metamorphism? (1) A (3) C (2) B (4) D

Which sample best shows the physical properties normally associated with regional metamorphism? (1) A (3) C (2) B (4) D 1 Compared to felsic igneous rocks, mafic igneous rocks contain greater amounts of (1) white quartz (3) pink feldspar (2) aluminum (4) iron 2 The diagram below shows how a sample of the mineral mica breaks

More information

CEE 437 Lecture 11 Rock Classification. Thomas Doe

CEE 437 Lecture 11 Rock Classification. Thomas Doe CEE 437 Lecture 11 Rock Classification Thomas Doe Translation of Mineral Properties to Rock Properties Comparison of mineral properties to rock properties Rocks have lower strength, especially tensile

More information

19 00' N 70 20' W Loma La Cuaba volcanic edifice 70 00' W Pueblo Viejo District (location of Fig. 2) Loma Navisa volcanic edifice 69 40' W & S a m a n á B a y 0 10 20 Kilometers 18 50' N Guaimarote Hatillo

More information

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

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

More information

A Sedimentary Rock is..

A Sedimentary Rock is.. Sedimentary Rocks A Sedimentary Rock is.. rock formed from the lithification or crystallization of: 1. Minerals in solution 2. Organic remains 3. Materials produced by living things (biochemical) 4. Clastic

More information

The Cobalt Rainbow. Airborne geophysical maps show that a north trending aeromagnetic high suggests further undiscovered mineralisation.

The Cobalt Rainbow. Airborne geophysical maps show that a north trending aeromagnetic high suggests further undiscovered mineralisation. The Cobalt Rainbow The property is located on Greenstone Creek, approximately 4.8 kilometres south west of the creek mouth. The property is located about 24 km due west of Campbell River, in the east-central

More information

it AUSIMM COBAR MINING SEMINAR

it AUSIMM COBAR MINING SEMINAR Straits Resources Limited it AUSIMM COBAR MINING SEMINAR Brownfields Exploration at Girilambone: Understanding the Mineralised Systems August 2010 Phil Shields / Phil Jones LOCATION TRITTON OPERATIONS

More information

Igneous Rocks. Sedimentary Rocks. Metamorphic Rocks

Igneous Rocks. Sedimentary Rocks. Metamorphic Rocks Name: Date: Igneous Rocks Igneous rocks form from the solidification of magma either below (intrusive igneous rocks) or above (extrusive igneous rocks) the Earth s surface. For example, the igneous rock

More information

How to Identify and Properly Classify Drill Cuttings

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

More information

Page 4.1 Overview 4-3

Page 4.1 Overview 4-3 Chapter 4 Contents Page 4.1 Overview 4-3 4.2 Soil Classification 4-3 4.2.1 Coarse Grained Soils 4-4 4.2.2 Fine-Grained Inorganic Soils 4-7 4.2.3 Organic Fine Grained Soils 4-7 4.2.4 Angularity 4-10 4.2.5

More information

GEOLOGY OF THE NICOLA GROUP BETWEEN MISSEZULA LAKE AND ALLISON LAKE

GEOLOGY OF THE NICOLA GROUP BETWEEN MISSEZULA LAKE AND ALLISON LAKE GEOLOGY OF THE NICOLA GROUP BETWEEN MISSEZULA LAKE AND ALLISON LAKE (92H/15E. 10E1 By V. A. Preto INTRODUCTION Mapping was continued southward from the area covered in 1973 and an additional 55 square

More information

ENVI.2030L Rock Identification

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

More information

Discovery of Thick Zone of Magnetite-Rich M Veins Strengthens Potential for Nearby Porphyry

Discovery of Thick Zone of Magnetite-Rich M Veins Strengthens Potential for Nearby Porphyry Thursday s Gossan Copper-Gold Porphyry Diamond Drilling Update Discovery of Thick Zone of Magnetite-Rich M Veins Strengthens Potential for Nearby Porphyry ~100m intercept of magnetite-rich M -veins and

More information

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 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

More information

Sediment. Weathering: mechanical and chemical decomposition and disintegration of rock and minerals at the surface

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

More information

Applications and Investigations in Earth Science Seventh Edition

Applications and Investigations in Earth Science Seventh Edition INSTRUCTOR MANUAL Stanley C. Hatfield Southwestern Illinois College Applications and Investigations in Earth Science Seventh Edition Tarbuck Lutgens Pinzke Exercise One The Study of Minerals MATERIALS

More information

Rocks Rock- A group of minerals, glass, mineroid bound together in some way.

Rocks Rock- A group of minerals, glass, mineroid bound together in some way. Rocks Rock- A group of minerals, glass, mineroid bound together in some way. All rocks fit into one of three categories: Igneous- formed by the cooling and hardening of hot molten rock Sedimentary- formed

More information

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

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

More information

3. GEOLOGY. 3.1 Introduction. 3.2 Results and Discussion Regional Geology Surficial Geology Mine Study Area

3. GEOLOGY. 3.1 Introduction. 3.2 Results and Discussion Regional Geology Surficial Geology Mine Study Area 3. GEOLOGY 3.1 Introduction This chapter discusses the baseline study of the geology and mineralization characteristics of the mine study area. The study consolidates existing geological data and exploration

More information

Review - Unit 2 - Rocks and Minerals

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.

More information

Work performed by: RALPH E. ALLERSTON (NEWMONT)

Work performed by: RALPH E. ALLERSTON (NEWMONT) 41Pt4NE8843 24 SOTHMAN 010 Diamond Drilling Township OF SOTHMAN Report NQ; Work performed by: RALPH E. ALLERSTON (NEWMONT) Claim N9 Hole NO Footage Date Note L. 332897 L. 332898 H-l-73 H-2-73 613' 587'

More information

SOIL CLASSIFICATION CHART COARSE-GRAINED SOILS MORE THAN 50% RETAINED ON NO.200 SIEVE FINE-GRAINED SOILS 50% OR MORE PASSES THE NO.200 SIEVE PRIMARY DIVISIONS GRAVELS MORE THAN 50% OF COARSE FRACTION RETAINED

More information

: Other [ ] 309.0' 349.0' 359.0' 349.0'

: Other [ ] 309.0' 349.0' 359.0' 349.0' 2F68NW8ee8 26 KAWASHEGAMUK LAKE 0 DIAMOND DRILLING AREA: KAWASHEGAMUK LAKE REPORT NO: 26 WORK PERFORMED FOR: International Platinum Corporation RECORDED HOLDER: Same as above [xx] : Other [ ] Claim Hole

More information

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

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

More information

Quiz 1. 3) Which of the following planetary bodies has the least number of impact craters on its surface? A) Mercury B) Mars C) the Moon D) Earth

Quiz 1. 3) Which of the following planetary bodies has the least number of impact craters on its surface? A) Mercury B) Mars C) the Moon D) Earth Quiz 1 1) Earth's atmosphere is unique among the moons and planets in that A) it has a nitrogen (N2) rich atmosphere. B) it is rich in oxygen (O2) and nitrogen (N2). C) it is rich in carbon dioxide because

More information

Copperstone Technical Report Update on 2018 Drilling Campaign

Copperstone Technical Report Update on 2018 Drilling Campaign 2018 Copperstone Technical Report Update on 2018 Drilling Campaign Chris McKnight Copperstone Resources AB 5/16/2018 Highlights Mineralisation consisting of interspersed chalcopyrite veins (assay results

More information

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

Table DR 1: Description of the lithologic succession encountered by the Enkingen (SUBO 18) drill core. DR20130138 G. Arp et al. SUPPLEMENTARY FILES (GSA Data Repository) Figure DR 1: Facies types of the Enkingen (SUBO 18) drill core. (A) Facies 1 clay-rich conglomeratic sandstone, 18.32-18.50 m depth. (B)

More information

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 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

More information

Version 1 Page 1 Barnard/George/Ward

Version 1 Page 1 Barnard/George/Ward The Great Mineral & Rock Test 1. Base your answer to the following question on the table below which provides information about the crystal sizes and the mineral compositions of four igneous rocks, A,

More information

Rocks Reading this week: Ch. 2 and App. C Reading for next week: Ch. 3

Rocks Reading this week: Ch. 2 and App. C Reading for next week: Ch. 3 Reading this week: Ch. 2 and App. C Reading for next week: Ch. 3 I. Environmental significance II. Definition III. 3 major classes IV. The Rock Cycle V. Secondary classification VI. Additional sub-classes

More information

Rocks Environmental Significance. Rocks Reading this week: Ch. 2 and App. C Reading for next week: Ch. 3. Rocks Definition of a rock

Rocks Environmental Significance. Rocks Reading this week: Ch. 2 and App. C Reading for next week: Ch. 3. Rocks Definition of a rock Reading this week: Ch. 2 and App. C Reading for next week: Ch. 3 Environmental Significance I. Environmental significance II. Definition III. 3 major classes IV. The Rock Cycle V. Secondary classification

More information

Sedimentology & Stratigraphy. Thanks to Rob Viens for slides

Sedimentology & Stratigraphy. Thanks to Rob Viens for slides Sedimentology & Stratigraphy Thanks to Rob Viens for slides Sedimentology The study of the processes that erode, transport and deposit sediments Sedimentary Petrology The study of the characteristics and

More information

Alteration and Mineralization at Daralu Porphyry Copper Deposit, South of Kerman, Southeast Iran

Alteration and Mineralization at Daralu Porphyry Copper Deposit, South of Kerman, Southeast Iran Alteration and Mineralization at Daralu Porphyry Copper Deposit, South of Kerman, Southeast Iran Mosayeb Salehian* and Majid Ghaderi Department of Geology, Tarbiat Modares University, Tehran, Iran *Email

More information

ANNEX VIII: APPENDIX E MINERALOGY RESULTS

ANNEX VIII: APPENDIX E MINERALOGY RESULTS ANNEX VIII: APPENDIX E MINERALOGY RESULTS Tables Table E-1 Mineralogical Analysis of Waste Rock Samples... 1 Table E-2 Mineralogical Analysis of Kimberlite Coarse Reject Samples... 3 E-i Table E-1 Mineralogical

More information

Earth Science Chapter 6 Rocks

Earth Science Chapter 6 Rocks Earth Science Chapter 6 Rocks I. Rocks and the Rock Cycle * Material that makes up the solid part of the Earth. * Made of a variety of different combinations of minerals and organic matter. A. Three Major

More information

SECOND and THIRD YEAR ASSESSMENT REPORT PROSPECTING LICENCE M, ROCK CUT PROPERTY, NTS 1N/12, NEWFOUNDLAND. ROY FRENCH (licence holder )

SECOND and THIRD YEAR ASSESSMENT REPORT PROSPECTING LICENCE M, ROCK CUT PROPERTY, NTS 1N/12, NEWFOUNDLAND. ROY FRENCH (licence holder ) SECOND and THIRD YEAR ASSESSMENT REPORT Of PROSPECTING On LICENCE 013704M, ROCK CUT PROPERTY, NTS 1N/12, NEWFOUNDLAND. By ROY FRENCH (licence holder ) Work Conducted: Sept. 17, 2008 Nov. 03, 2009 Total

More information

The 3 types of rocks:

The 3 types of rocks: Igneous Rocks and Intrusive Igneous Activity The 3 types of rocks:! Sedimentary! Igneous! Metamorphic Marble 1 10/7/15 SEDIMENTARY ROCKS Come from rocks sediments (rock fragments, sand, silt, etc.) Fossils

More information

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:

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

More information

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

More information

GEOL 101 Lecture 7. Weathering, Sediments. Rock Cycle. Least Stable. Most Stable. Weathering Ch. 5. Physical. Chemical

GEOL 101 Lecture 7. Weathering, Sediments. Rock Cycle. Least Stable. Most Stable. Weathering Ch. 5. Physical. Chemical GEOL 101 Lecture 7 Weathering, Sediments S. Kite Photo Bear Butte S.P., SD Rock Cycle Weathering Ch. 5 Physical (later) Chemical (now) Bowen s Reaction Series vs. Goldich s Weathering Series for sand-size

More information

As compaction and cementation of these sediments eventually occur, which area will become siltstone? A) A B) B C) C D) D

As compaction and cementation of these sediments eventually occur, which area will become siltstone? A) A B) B C) C D) D 1. A student obtains a cup of quartz sand from a beach. A saltwater solution is poured into the sand and allowed to evaporate. The mineral residue from the saltwater solution cements the sand grains together,

More information

Appendix 3. Sample Descriptions

Appendix 3. Sample Descriptions 39 Appendix 3. Sample Descriptions 41 Appendix 3. Sample descriptions. HRM-01 Bates Lake Area 11D/13 (0423452/4956547) HRM-02 Bates Lake Area 11D/13 (0423010/4957749) HRM-03 Bates Lake Area 11D/13 (0422900/4957059)

More information

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

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

More information

Unit 2: Minerals and Rocks Practice Questions

Unit 2: Minerals and Rocks Practice Questions Name: Date: 1. Which mineral is white or colorless, has a hardness of 2.5, and splits with cubic cleavage? 6. Base your answer(s) to the following question(s) on the photograph of a sample of gneiss below.

More information

Clastic Textures. I. What is the sorting of sample numbers 60, 61, and 62? Answers on last page.

Clastic Textures. I. What is the sorting of sample numbers 60, 61, and 62? Answers on last page. Sed Rock s Sel f-instruction N ame Geology 100 Harbor Secti on Sedimentary rocks are usually identified in the field by their stratification or layering, which originates by the successive deposition of

More information

RR#7 - Multiple Choice

RR#7 - Multiple Choice 1. Which mineral is mined for its iron content? 1) hematite 2) fluorite 3) galena 4) talc 2. Which rock is composed of the mineral halite that formed when seawater evaporated? 1) limestone 2) dolostone

More information

Table 174AX Bethany Beach

Table 174AX Bethany Beach 1 12-May-00 5-10 3.65 73 Sand; 2.2 ft contact, sandy silty clay Sinepuxent 2 12-May-00 10-15 4.20 84 Fine-very fine sand and clay Sinepuxent 3 12-May-00 15-20 3.60 72 Fine-very fine sand and clay Sinepuxent

More information

Rocks. 3.1 The Rock Cycle. 3.1 The Rock Cycle. 3.1 The Rock Cycle. The Rock Cycle. I. Rocks

Rocks. 3.1 The Rock Cycle. 3.1 The Rock Cycle. 3.1 The Rock Cycle. The Rock Cycle. I. Rocks Rocks Tarbuck Lutgens 3.1 The Rock Cycle 3.1 The Rock Cycle I. Rocks Rocks are any solid mass of mineral or mineral-like matter occurring naturally as part of our planet. Types of Rocks 1. Igneous rock

More information

MEMO. TO: Dennis Lapoint CC: FROM: Eriaan Wirosono DATE: April, 20 th 2014 SUBJECT: Exploration activity report March-April 2014_EW

MEMO. TO: Dennis Lapoint CC: FROM: Eriaan Wirosono DATE: April, 20 th 2014 SUBJECT: Exploration activity report March-April 2014_EW TO: Dennis Lapoint CC: FROM: Eriaan Wirosono DATE: April, 20 th 2014 SUBJECT: Exploration activity report March-April 2014_EW MEMO 1. Highlights and Productivity Overview pan sampling on target Areas 1

More information

GUIDELINES ON THE DESCRIPTION AND CLASSIFICATION OF ROCKS OF THE TUEN MUN FORMATION

GUIDELINES ON THE DESCRIPTION AND CLASSIFICATION OF ROCKS OF THE TUEN MUN FORMATION GUIDELINES ON THE DESCRIPTION AND CLASSIFICATION OF ROCKS OF THE TUEN MUN FORMATION Rod Sewell Hong Kong Geological Survey GEO/CEDD Objectives to review all known lithologies of the Tuen Mun based on literature

More information

Sedimentary Structures in Metamorphic Rocks

Sedimentary Structures in Metamorphic Rocks Maine Geologic Facts and Localities November, 2006 Primary Sedimentary Structures in Some Metamorphic Rocks Text by Thomas K. Weddle, Department of Agriculture, Conservation & Forestry 1 Photo by Thomas

More information

Sedimentary Rocks and Processes

Sedimentary Rocks and Processes Sedimentary Rocks and Processes Weathering Sedimentary Processes Breakdown of pre-existing rock by physical and chemical processes Transport Movement of sediments from environments of relatively high potential

More information

CREATING VALUE THROUGH DISCOVERY IN SOUTH AMERICA. Lara Copper Project. Lara 45%-Owned Property in Southern Peru

CREATING VALUE THROUGH DISCOVERY IN SOUTH AMERICA. Lara Copper Project. Lara 45%-Owned Property in Southern Peru CREATING VALUE THROUGH DISCOVERY IN SOUTH AMERICA Lara Copper Project Lara 45%-Owned Property in Southern Peru 1 Forward Looking Statements Except for statements of historical fact relating to the Company,

More information

ST ANDREW GOLDFIELDS LTD. Assessment Report. WZ Garrison Diamond Drilling Program

ST ANDREW GOLDFIELDS LTD. Assessment Report. WZ Garrison Diamond Drilling Program ST ANDREW GOLDFIELDS LTD. Assessment Report WZ Garrison Diamond Drilling Program Garrison Township, Larder Lake Mining Division Thomas Gallo 5/6/2015 TABLE OF CONTENTS Introduction 1 Location, Access &

More information

Chapter 6 Pages of Earth s Past: Sedimentary Rocks

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

More information

Module 9 Sedimentary Rocks

Module 9 Sedimentary Rocks Module 9 Sedimentary Rocks SEDIMENTARY ROCKS Rocks formed from material derived from preexisting rocks by surfacial processes followed by diagenesis There are two main classes of sedimentary rocks Clastic

More information

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 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

More information

=%REPORT RECONNAISSANCE OF CHISHOLM LAKE PROSPECT. October 25, 1977

=%REPORT RECONNAISSANCE OF CHISHOLM LAKE PROSPECT. October 25, 1977 =%REPORT ON FIELD RECONNAISSANCE OF CHISHOLM LAKE PROSPECT October 25, 1977 Bruce D. Vincent Imperial Oil Limited, Minerals - Coal, CALGARY, ALBERTA CHISHOLM LAKE PROSPECT Introduction The Chisholm Lake

More information

Rich Saddle North Au-Cu-Ag Porphyry Expands by 275m Along Strike and 250m Down-Dip

Rich Saddle North Au-Cu-Ag Porphyry Expands by 275m Along Strike and 250m Down-Dip GT Gold Drills 281 Metres of 0.65 g/t Au, 0.38% Cu, 1.38 g/t Ag (1.24 g/t AuEq 1 ) Within 685 Metres 2 of 0.40 g/t Au, 0.26% Cu, 1.03 g/t Ag (0.81 g/t AuEq) in Step-out Hole TTD098 Rich Saddle North Au-Cu-Ag

More information