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Kootenay Project

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The Ledgend Property (1735 Ha) was the first documented occurrence of nickel-cobalt bearing massive sulphides in the region. Discovered by prospectors in 1981 during construction of a logging road, the showing was not subsequently staked until 1997. The mineralization was described in 1998 by the B.C. Geological Survey as outcropping massive pyrrhotite with nickel and cobalt minerals. The geologist noted that the mineralized horizon could be traced over hundreds of meters along strike. Subsequently largely overgrown, in 2016 the new owners relocated float from the discovery outcrop and grab sampling returned values of 0.15 to 0.76% nickel and 0.01 to 0.09% cobalt, as well as up to 0.53% chrome and anomalous copper and zinc. Subsequent work in 2016 included a soil survey covering an area 500 by 1600 metres at 25 metre spacing on 100 metre lines. This generated a nickel-cobalt anomaly 800 metres in length extending to the southeast of the showing, with the peak of the anomaly (values up to 0.84% nickel) located on a steep slope about 200 metres southeast.

A conformable and probably syngenetic horizon of manganiferous exhalite is associated with the massive sulfides located to date. Sampling has intermittently traced this horizon throughout the length of the soil grid and beyond, from at least 400 metres to the north to some 4,500 metres to the south, where similar conformable sulfide mineralization occurs along a road cut. Another soil grid has been completed covering one kilometre of the southern strike extension. The northern portion of the claims covers two kilometres of the horizon's strike and will be sampled in 2018.

Cardero soil sampling in fall 2017 expanded on the sampling completed in 2016 (the "North Grid") and added a second grid 1.8 kilometres to the south ("South Grid"), collecting 1,218 samples which have produced significant anomalies for follow-up work. In addition, the original discovery outcrop was cleaned and chip sampled perpendicular to foliation, returning 4 metres of 0.22% Ni and 161ppm Co (Plate 1), with a one metre sample running 0.39% Ni and 0.028% Co. A 20-30cm layer of massive to semi-massive pyrite-pyrrhotite occurs between an upper horizon of siliceous biotite schist and lower horizon of talc-tremolite schist. True widths should be close to sample widths, but might vary significantly due to the tight folding.

The mineralization is hosted by northwest-trending, tightly folded sericite and biotite schists, quartzite, and talc-tremolite schist of the Index Formation, a member of the Lardeau Group. Graphitic and manganiferous layers are particularly anomalous in metals, and thought to be seafloor exhalatives generated by submarine hydrothermal fluids. The rock types and style of mineralization are most similar to the Outokumpu and Talvivaara districts in central and eastern Finland.

There is ongoing study as to how shale hosted, or shale associated, Ni-Cu-Zn-Co deposits form. There is now recognition of oceanic detachment faults on the modern day ocean floor that have focused large volumes of black smoker fluids along an ultramafic - volcanic (or sediment) contact. This results in metasomatic alteration of ultramafics to talc-tremolite-chlorite schists along the fault. By this process, distal venting of Ni-rich fluids can form "VMS" deposits far from a spreading ridge, in or under quiet basins where shales deposit. If fault involves a sedimentary package, the fluids can precipitate subsurface, within shales or sandstone, which are later deformed and metamorphosed to black schist and quartzite.

Deposit model for mineralization at Ledgend, and probably the other properties in the project. Modified from Jowitt and Keays (2012): Shale-hosted Ni-(Cu-PGE) mineralisation: A global overview.

North Grid Anomalies

The North Grid generated new anomalies both east and west of the original central anomaly. This grid, centred on the discovery showing, now covers an area 1100 by 2000 metres at 25 metre sample spacing on 100 metre spaced lines. The central nickel-cobalt ("Ni-Co") ("Central Zone") soil anomaly is 800 metres in length extending to the southeast of the showing, with the peak of the anomaly (values up to 0.84% Ni, 0.025% Co) located about 200 metres southeast of the massive sulphides in the discovery outcrop. This anomaly is associated with float of the same talc-tremolite-actinolite schist that occurs as the footwall to the massive sulphides, and which is the altered remnant of high Ni-Co ultramafic rocks. Trenching of the anomaly is planned to test Cardero's interpretation that the source of the nickel is buried massive sulphides.

About 400 metres to the north of the discovery showing, a separate Ni-Co peak at the north end of the anomaly occurs in a recessive area below a cliff of siliceous biotite schist. The same schist forms a large cliff north of, and apparently above, the larger anomaly peak to the south (Figure 3). The two Ni-Co peaks are joined by an adjacent copper anomaly that, at the north end, can be attributed to thin layers of outcropping semi-massive sulphides within quartzite at the Road Showing (Figure 3). Grab rock samples indicate the layers are relatively high in gold (ranging from 0.17 - 0.46 g/t), copper (up to 0.1%), manganese and phosphate, but low in nickel and cobalt.

Northwest trending Cu-Zn-Co-Ni anomalies occur along the western and eastern margins of the soil grid (Figure 3). The stronger eastern anomaly ("East Zone") has the most anomalous copper, cobalt, and nickel outside of the Central Zone. Any outcrops within the anomaly remain to be mapped and sampled.

The West Zone is a two kilometre long, Cu-Zn Co-Ag anomaly open to the north, south and southwest.

Chip sampling of discovery outcrop with layer of semi- massive sulphide from the Ledgend discovery outcrop.

Sample of massive sulphide from the Ledgend discovery outcrop.

South Grid Anomalies

The South Grid, which covers one kilometre of the southern strike extension from the northern grid, generated a broad, 300 by 600 metre Ni-Co-Cu anomaly that is open to the south and west. Levels of nickel and cobalt are lower than the north grid, but the area is less steep and depth to bedrock is likely greater. This grid will be extended to the north and southwest in the next field season.