Detailed Summary Report

Export Report

Assessment Report: 16952

Property Name

Silver Pond
16952a.pdf
16952b.pdf
16952c.pdf
16952f.pdf
16952g.pdf

Location

NAD 83	57° 19' 00.00'' N, 127° 13' 05.00'' W 57.316667, -127.218056 UTM: Easting 607321, Northing 6354041, Zone 9 (North)
NAD 27	57° 19' 00.21'' N, 127° 12' 59.44'' W 57.316724, -127.216512 UTM: Easting 607418, Northing 6353839, Zone 9 (North)
NTS	094E06E, 094E06W
BCGS	094E034

Mining Divisions

Omineca

Mining Camp

Toodoggone Camp

Title

Report on 1987 Exploration Program

Report Year

1987

Number of Pages

389

Statements of Work

n/a

Affidavit Date

1987-11-04

Off Confidential

1988-11-04

Claims

Asap, Silver Cloud 1-3, Silver Creek, Silver Grizzly Fr., Silver Marten, Silver Peak Fr., Silver Pond, Silver Pond Fr., Silver Sun

General Work Categories

Drilling, Geochemical, Geological, Geophysical, Physical

Operators

Nexus Res.

Owners

St. Joe Canada Inc.

Authors

Vogt, A.H.
Kennedy, David Roy

MINFILE Nos

094E 069, 094E 075

Commodities

Silver, Gold

Work Done

Drilling	Diamond surface	98 hole(s); NQ; 12936.0 m; No. of maps: 89; Scale(s): 1:1000, 1:500
Geochemical	Rock	485 sample(s); No. of maps: 2; Scale(s): 1:5000
	Elements Analyzed For	Silver, Gold
	Sampling/assaying	5893 sample(s)
	Elements Analyzed For	Silver, Gold
	Soil	66 sample(s)
	Elements Analyzed For	Silver, Gold
Geological	Geological	4050.0 ha; No. of maps: 1; Scale(s): 1:10 000
Geophysical	Induced Polarization	19.3 km; No. of maps: 5; Scale(s): 1:1250, 1:2500
	Magnetic, ground	10.0 km; No. of maps: 1; Scale(s): 1:1000
	Resistivity (alone)	10.0 km; No. of maps: 3; Scale(s): 1:1000
Physical	Line/grid	100.0 km; No. of maps: 1; Scale(s): 1:10 000
	Reclamation	1.0 ha
	Trench	30 trench(es); 3000.0 m; No. of maps: 3; Scale(s): 1:1000, 1:2500, 1:500

Keywords

Related Report(s)

14700, 10047, 8300

File(s)

16952a.pdf
16952b.pdf
16952c.pdf
16952f.pdf
16952g.pdf

Geological Summary

The property is underlain by Middle Jurassic Toodoggone volcanics. The gently northwest dipping volcanic rocks are crosscut by subvertical rhyolitic dykes. Epithermal gold-silver mineralization and associated hydrothermal alteration is structurally controlled by a system of northwest to north-northwest trending, steeply dipping faults.