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FIRST YEAR
ASSESSMENT REPORT ON MIGUEL’S HILL PROPERTY CENTRAL NEWFOUNDLAND
Licence # 014102M N.T.S. 2D/12
For
Department of Mines and Energy P. O. Box 8700
St. John’s NL A1B 4J6
For
almar consultants 31 Prince Street
Clarenville NL A5A 1W4
By
Alexander S. Duffitt 31 Prince Street
Clarenville NL A5A 1W4
Summary The Miguel’s Hill Property is held by almar consultants and consists of 4 claims on 1 licence. This property was staked on information emerging of uranium discoveries in similar rock types and age on the Baie Verte Peninsula. Unfortunately my current work and research of previous work has not been encouraging and no future work is planned.
Table of Contents
Introduction page 1 Location, Access and Physiography page 2 Present Work page 2 Geology page 1-2 Recommendations page 6 Appendix A Sample descriptions, and co-ordinates Appendix B Personnel and Expenses Appendix C Assay results and certificates Figure 1 Location Newfoundland page 3 Figure 2 Property location and geology page 4 Figure 3 Rock sample locations page 5
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Miguel’s Hill Introduction: The Miguel’s Hill Property is held by almar consultants and consists of 4 claims on 1 licence. This property was staked on information emerging of uranium discoveries in similar rock types and age on the Baie Verte Peninsula. These claims are located 12-15 km south of the town of Grand Falls-Windsor. Regional Geology: The island of Newfoundland has been subdivided into three major tectono-stratigraphic zones. The eastern Avalon Zone consists of a late Precambrian to Ordovician shallow marine sequence of clastic and carbonate sediments. Along the western side of the island the Humber Zone consists of a similar platform assemblage of Canbro-ordovician Clastic and carbonate sediments. Between these two zones is the Central Mobile Belt of the late Cambrian to Devonian, strongly deformed volcanics, sediments and intrusives. This zone has been further subdivided into the Western Dunnage Zone and the eastern Gander Zone. The Dunnage Zone records the history of the Proto-Atlantic Ocean (Iapetus) from initial generation of mid-ocean ridge ophiolitic sequences to island arc subduction, volcanism and sedimentation. The Gander zone is thought to be an Andean-type plate margin which marked the eastern boundary of the Proto-Atlantic Ocean. The Stony Lake volcanics lie within the eastern portion of the Dunnage Zone and are the youngest volcanics preserved in this zone. They comprise a lithologically and geochemically homogeneous series of felsic flows, pyrochlastics and associated sedimentary rocks which unconformably overlie shallow water sediments and minor volcanics of the Botwood group. On the basis of reliable fossil evidence the Botwood Group has been assigned a Silurian age .Zircon date (U/Pb) indicate that the Stony Lake volcanics are approximately the same age as the youngest (Silurian) Botwood Group rocks, and not Devonian as previously thought. The Botwood Group appears to be fault bounded on its West side and may, overall, occupy a large graben. On their southwest boundary, the Stony Lake volcanics unconformably overlie mid-Ordovician, strongly deformed volcanic rocks of the Pipestone Pond complex. The Mount Peyton intrusive suite, a large bimodal (diorite/granite) Devonian or younger batholiths, intrudes the Botwood Group about 10km east of the Stony Lake volcanics.
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A caldera collapse structure was the initial model used to guide exploration in the Stony Lake area. Collapsed calderas are known to host epithermal gold deposits in various areas e.g. the Creede district of Colorado in the southwestern United States. Felsic pyrocalstics provide porous host rocks; tensional features associated with collapse provide further permeability and vertical channels. Heat produced during the waning stage of resurgent intrusive activity drives the groundwater convection system in which metals leached from large volumes of source rock are deposited into near-surface pore spaces at a level determined by the onset of boiling. A re-interpretation of felsic volcanism and stratigraphy in the Springdale area (Coyle and Strong, 1987) has invoked this model and has led to an exploration program by Teck Corporation. Gold deposits and showings in the Baie Verte area, north of Springdale, may be related to this subaerial volcanic regime as a system as a system of deeper, subvolcanic veins. Access and Physiography: This area has excellent access throughout via forest access roads both new and abandon. The area has low relief and is poorly drained. Large barren areas and open bogs alternate with patches of forest, and a few small ponds. There are a number of outcrops of this particular rock while in major portions of this area the overburden can be very thick. Present Work: My sample numbers (170202-5) are denoted on the attached reference maps 2D/12 (Figure # 3), the descriptions and the UTM co-ordinates of the samples are included in Appendix A. Personnel and expenses are contained in Appendix B and the assay results are in Appendix C. The regional geology map is shown in Figure #2.
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Location Map Newfoundland:
Figure # 1
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Geology Map:
Figure # 2
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Sample Location Map:
Figure # 3
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Recommendations: This property was staked on information emerging of uranium discoveries in similar rock types and age on the Baie Verte Peninsula. Unfortunately my current work and research of previous work has not been encouraging and no future work is planned.
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Appendix A
Sampe #` Map Northing Easting Sample Type Sample Descrption
170202 02D/12 N 5393566 m 21 592535 m Rock o/c Red flow banded ryholtic with pyrite +/- 2%170203 02D/12 N 5393742 m 21 592430 m Rock o/c Red flow banded ryholtic with pyrite +/- 2%170204 02D/12 N 5394002 m 21 592273 m Rock o/c Red flow banded ryholtic with pyrite +/- 2%170205 02D/12 N 5394033 m 21 592646 m Rock o/c Red flow banded ryholtic with pyrite +/- 2%
Appendix B
ExpensesMiguel's HillLicence # 014102M
2007
Prospectors Days Value Total:
Sandy Duffitt field work 2.00 $200.00 $400.00Paul Strong field work 2.00 $200.00 $400.00Sandy Duffitt report 1.00 $200.00 $200.00
Gas 1.00 $125.00 $125.00Assays 1.00 $138.77 $138.77Freight charges 1.00 $11.30 $11.30Meals 1.00 $95.00 $95.00Cabin Rental 2 day @75 1.00 $150.00 $150.00ATV Rental 1 machine 2.00 $113.00 $226.00100/day + HSTSub Total $1,746.07
15% Overhead $261.91
Grand Total $2,007.98
Appendix C
1046 Gorham StreetThunder Bay, ON Canada P7B 5X5
Tel: (807) 626-1630Fax: (807) 622-7571
Certificate of Analysis
Thursday, October 4, 2007
Duffitt, Alexander31 Prince St.Clarenville, NF, CANA5A1W4Email#: [email protected], [email protected]
Date Received: Aug 30, 2007
Date Completed: Oct 4, 2007
Job #: 200730076
Reference:
Sample #: 27 Rock
Acc # Client ID Au
ppbPt
ppbPd
ppbRh
ppb
3793 170202 <5 24 <10
3794 170203 <5 <15 <10
3795 170204 <5 27 <10
3796 170205 <5 <15 <10
3797 170206 <5 <15 <10
3798 170207 <5 <15 <10
3799 170208 <5 <15 <10
3800 170209 <5 22 <10
3801 170210 <5 <15 <10
3802 170211 <5 <15 <10
3803 Dup 170211 6 <15 <10
3804 170212 20 <15 <10
3805 170213 <5 <15 <10
3806 170214 <5 <15 <10
3807 170215 15 <15 <10
3808 170216 <5 <15 <10
3809 170217 <5 <15 <10
3810 170218 <5 18 <10
3811 170219 <5 16 <10
3812 170220 <5 <15 <10
3813 170221 <5 19 <10
3814 Dup 170221 <5 30 <10
3815 170222 <5 <15 <10
3816 170223 <5 <15 12
Page 1
1046 Gorham StreetThunder Bay, ON Canada P7B 5X5
Tel: (807) 626-1630Fax: (807) 622-7571
Certificate of Analysis
Thursday, October 4, 2007
Duffitt, Alexander31 Prince St.Clarenville, NF, CANA5A1W4Email#: [email protected], [email protected]
Date Received: Aug 30, 2007
Date Completed: Oct 4, 2007
Job #: 200730076
Reference:
Sample #: 27 Rock
Acc # Client ID Au
ppbPt
ppbPd
ppbRh
ppb
3817 170224 <5 16 <10
3818 170225 166 <15 <10
3819 170226 82 25 <10
3820 170227 26 <15 <10
3821 170228 12 45 <10
PROCEDURE CODES: AL4AU3, AL4ICPAR, AL4U
Certified By: ______________________
Derek Demianiuk H.Bsc., Laboratory Manager
The results included on this report relate only to theitems testedThe Certificate of Analysis should not be reproducedexcept in full, without the writtenapproval of the laboratory
AL907-0098-10/04/2007 9:22 AM
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Duffitt, AlexanderDate Created: 07-10-11 02:20:03 PMJob Number: 200730076Date Received: Aug 30, 2007Number of Samples: 27Type of Sample: RockDate Completed: Oct 4, 2007Project ID:
Accur. # Client Tag Ag Al As B Ba Be Bi Ca Cd Co Crppm % ppm ppm ppm ppm ppm % ppm ppm ppm
3793 170202 <1 0.7 11 61 9 <1 14 0.35 <4 <1 2533794 170203 <1 0.25 <2 69 11 <1 7 0.14 <4 <1 4363795 170204 <1 2.51 3 67 19 <1 18 0.84 <4 20 2663796 170205 <1 3.31 5 65 32 <1 20 3.14 <4 24 585
* The results included on this report relate only to the items tested* This Certificate of Analysis should not be reproduced except in full, without the written approval
of the laboratory.*The methods used for these analysis are not accredited under ISO/IEC 17025
Cu Fe K Li Mg Mn Mo Na Ni P Pb Sb Seppm % % ppm % ppm ppm % ppm ppm ppm ppm ppm
40 1.87 0.06 13 0.15 438 7 0.06 4 <100 97 <5 <58 0.94 0.06 <1 0.2 144 <1 0.02 7 <100 40 <5 513 4.21 0.18 22 1.95 877 5 0.06 74 446 174 <5 <532 5.93 0.28 28 2.5 1542 8 0.11 86 595 259 8 6
Si Sn Sr Ti Tl V W Y Zn% ppm ppm ppm ppm ppm ppm ppm ppm
0.07 <10 9 <100 2 <2 <10 6 800.05 <10 8 <100 <1 9 <10 2 190.11 <10 22 2866 <1 64 <10 16 790.16 <10 94 3058 3 88 <10 26 79
