British Columbia Ministry of Energy, Mines and Natural Gas and Responsible for Housing
News | The Premier Online | Ministries & Organizations | Job Opportunities | Main Index

MINFILE Home page  ARIS Home page  MINFILE Search page  Property File Search
Help Help
File Created: 14-Aug-1986 by Gary R. Foye (GRF)
Last Edit:  06-Mar-2025 by Del Ferguson (DF)

Summary Help Help

NMI
Name HARDSCRABBLE CREEK Mining Division Cariboo
BCGS Map 093H012
Status Past Producer NTS Map 093H04E
Latitude 053º 08' 05'' UTM 10 (NAD 83)
Longitude 121º 39' 18'' Northing 5888102
Easting 589980
Commodities Gold, Tungsten Deposit Types C01 : Surficial placers
Tectonic Belt Omineca Terrane Slide Mountain, Barkerville
Capsule Geology

The HARDSCRABBLE CREEK placer occurrence is located on the alluvial fan of Hardscrabble Creek above its confluence with Willow River, approximately 6 kilometres northwest of the community of Wells.

Placer gold deposits of the Quesnel Highland region, including the former rich producers of the Barkerville camp, have accounted for a large proportion of British Columbia's alluvial gold production. With the exception of a few producers in the Wingdam area, which are underlain by Upper Triassic sediments correlative with the Nicola Group, almost all the deposits are underlain by the Upper Proterozoic to Lower Paleozoic Snowshoe Group. These predominantly metasedimentary rocks have been metamorphosed to greenschist facies.

Placer gold deposits in the region are generally found in relatively young Pleistocene gravels. The morphology and mineral associations of the gold suggest that it was derived locally, the most obvious sources are the numerous auriferous veins in the Downey succession of the Snowshoe Group.

At least part of the placer mining done on Hardscrabble Creek involved underground work. The area is mainly underlain by Snowshoe Group rocks but the contact with Slide Mountain Group rocks is nearby.

"Data from the Cariboo mining district indicate that supergene leaching of gold dispersed within massive sulphides by Tertiary deep weathering followed by Cenozoic erosion is the most likely explanation for the occurrence of coarse gold nuggets in Quaternary sediments" (Exploration in British Columbia 1989, page 147).

Historically the property has been worked since the 1880s with the main project being the drifting of a drainage tunnel along bedrock from a point just northeast of the confluence of Hardscrabble Creek, and the Willow River. This adit extended north for a distance of some 625 metres terminating very near the north end of placer claim 1711 (Assessment Report 21199). Considerable drifting was done in and around the north end following the sinking of a 19 metre shaft as well as at the south end where a shaft was sunk to the 28 metre level.

From 1879 to 1895 the estimated combined production of Hardscrabble and Sugar Creeks totaled about 5,180 ounces (161,098 grams).

In 1991, Dragon Mountain Placers prospected and sampled their placer claims on Hardscrabble Creek. It was thought that the previous old-time high-graded the gutter of the creek, leaving most of the valley fill in place.

In 2022, 1244338 BC Ltd. reviewed LiDAR data to detect the documented drain tunnel from the 1800's placer workings. Following field verification, a seismic survey was conducted across the alluvial fan of Hardscrabble Creek. The survey uncovered shelf features at depths of 16 to 18 metres which serve as a target for a drill program.

Bibliography
EMPR AR 1879-1895-tables; 1879-237; 1881-393; 1884-420; 1885-488; 1893-1038; 1894-727; 1897-465; 1900-737; 1901-961;
1902-60; 1947-122
EMPR ASS RPT 21199, 40620
EMPR BULL 28, pp. 22,26
EMPR EXPL 1989, pp. 147-169
EMPR FIELDWORK 1990, pp. 331-356; 1992, pp. 463-473
EMPR P. 2003-1, pp. 77-96
EMPR PFD 681607
EMPR OF 1991-17; 1999-3
GSC MEM 149, p. 210
GSC MAP 1424A

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY