TORONTO, Feb. 23, 2021 /CNW/ - First Cobalt Corp. (TSXV:
FCC) (OTCQX: FTSSF) (the "Company") is pleased to announce that a
geophysical survey of its Iron Creek cobalt-copper deposit in
Idaho, USA has identified several
new drill targets. Data provides further support for a resumption
of drilling to expand the Iron Creek deposit and test new targets
over a 2-kilometer radius within the Property.
Highlights:
- High chargeability zones were detected along strike of the Iron
Creek cobalt-copper deposit, presents an opportunity to more than
double the strike length of the current mineralization
- Additional high chargeability anomalies detected in the
footwall of Iron Creek, highlighting the potential for new
mineralization within the resource area
- Drilling to resume to test the new targets, with a view to
expanding the Iron Creek cobalt-copper resource and explore the
possibility for new discoveries on the property
Trent Mell, President & Chief Executive Officer,
commented:
"The Idaho Cobalt Belt is America's best opportunity to
rapidly develop a domestic supply of this critical mineral. With
cobalt in sulfate form trading above $30/lb, this U.S. asset can become an attractive
source of cobalt for the electric vehicle market. Following a
remarkable year of growth in the European EV market, North America is poised to follow suit.
Fast-tracking the Iron Creek Project is consistent with our
strategy of producing the world's most sustainable cobalt.
"The geophysical survey has been successful in identifying
new targets on our Idaho property
and potentially extending known cobalt-copper mineralization of the
Iron Creek deposit. We are excited by the prospectivity of our land
package and we will resume drilling over the summer months. These
anomalies will be priority drill targets along with the extensive
cobalt-copper mineralization on surface at the nearby Ruby Zone, which we also control."
2020 Geophysical Survey Results
A total of thirteen lines were surveyed at the Idaho Property
using Induced Polarity and Resistivity geophysical methods.
Previous bore-hole electromagnetic surveys have shown both
cobalt-rich and copper-rich mineralization are conductive. The IP
and Resistivity methods were used to also detect disseminated-style
mineralization to outline the full width of a potential metal
resource.
The Iron Creek deposit has been traced by drilling over a
900-meter strike extent. The eastern and western portions of the
cobalt-copper resource were surveyed separately to test extensions
to mineralization, including mineralization that was believed to
extend below cover. Results indicate that the mineralization
extends 700 metres beyond the copper-rich western zone and over 300
metres into the cobalt-rich eastern zone (Figure 1).
Some overlap of lines was completed over previously drilled
areas to characterize the chargeability and resistivity responses
to mineralization. The data were processed and integrated in the 3D
resource model to spatially relate the geophysical response to
mineralization and the metasedimentary rocks. Chargeability
correlates well with cobalt-rich pyrite mineralization in areas
previously drilled, demonstrating the method is applicable for
direct detection of this style of mineralization. The high
chargeability response near surface in the west and east of the
Iron Creek deposit is considered to trace mineralization below the
Challis Volcanics cover, as the anomalies persist to depth although
reduced in intensity.
Table 1. Interpretation of Chargeability Anomalies (from
Figure 1)
Anomaly
|
Interpretation of
Chargeability
|
Length
(m)
|
1 & 3
|
Eastern extension of
the Iron Creek cobalt-copper resource from surface down to below
300 metres
|
300
|
2
|
Iron Creek footwall
mineralization along a separate metasedimentary horizon
|
100 (open to
west)
|
4
|
Disseminated
mineralization at surface traced below the cover rocks
|
300
|
5 & 7
|
Footwall Zone
associated with disseminated mineralization at surface; anomaly #5
may be the eastern correlation along this metasedimentary
horizon
|
400
|
6
|
Western extension of
the Iron Creek cobalt-copper resource from surface and below the
cover rocks
|
750
|
8
|
Weakly anomalous
response from disseminated mineralization along a separate
metasedimentary horizon
|
300
|
9
|
Weakly anomalous
response from disseminated mineralization along a separate
metasedimentary horizon
|
400
|
Nine discrete chargeability anomalies have been interpreted. The
geophysical survey results are also interpreted to highlight
north-south trending faults previously identified by bedrock
mapping. The continuity of the high chargeability anomalies reflect
a minor offset on these faults at the margins of the Challis that
are interpreted to displace the mineralized zone southward.
A drilling program is currently being designed to test for the
extensions of the Iron Creek cobalt-copper resource. The areas with
high chargeability anomalies considered to be associated with
mineralization along this horizon have been prioritized for this
program. Further ground geophysical surveys are also planned to
better resolve the anomalies at depth below cover and cover the
area between high chargeability anomalies associated with the
Footwall Zone.
Iron Creek Cobalt-Copper Resource
Iron Creek is a high grade underground primary cobalt deposit on
patented property in the United
States. It currently has an Indicated Resource of 2.2
million tonnes at 0.32% cobalt equivalent (0.26% cobalt and 0.61%
copper) for 12.3 million pounds of contained cobalt and an Inferred
Resource of 2.7 million tonnes at 0.28% cobalt equivalent (0.22%
cobalt and 0.68% copper) for an additional 12.7 million pounds of
contained cobalt. The resource estimate used a 0.18% cobalt
equivalent cutoff grade.
Drilling has outlined the strike extent of mineralization to
over 900 metres and down-dip to over 650 metres. Mineralization
remains open along strike and down-dip, suggesting strong potential
for significant future resource growth. Thick mineralized zones of
up to 30 metres of true thickness reflect broad stratabound
lithological controls.
Iron Creek mineralization occurs as lenses and pods of pyrite,
the dominant phase hosting cobalt, that are primarily concordant to
the sedimentary layering in the host rocks. Chalcopyrite, the only
copper mineral phase, is disseminated and also occurs as stringers
cutting pyrite mineralization within the zone of
mineralization.
The host rocks to mineralization are a finely inter-bedded
sequence of siltstone and argillite with intermittent, less than
30cm thick, quartzite layers. Ripple and dune sedimentary
structures are well-preserved throughout the mineralized sequence.
A higher proportion of quartzite layers have been mapped above and
below the mineralized zone at surface marking the stratigraphic
hangingwall and footwall to mineralization.
To learn more about the Iron Creek Project, please refer to the
Company's 2019 corporate video, which can be found at
www.youtube.com/watch?v=DAaL4o8ijiw&feature=emb_logo.
Qualified Person Statement
Dr. Frank Santaguida, P.Geo., is
the Qualified Person as defined by National Instrument 43-101 who
has reviewed and approved the contents of this news release. Dr.
Santaguida is employed as Vice President, Exploration for First
Cobalt.
About First Cobalt
First Cobalt owns North
America's only permitted primary cobalt refinery. Cobalt
refining is a critical component to the development and
manufacturing of batteries for electric vehicles and forms a
foundational piece of the next generation of the North American
auto sector and other electrified consumer and industrial
applications. First Cobalt owns the Iron Creek cobalt project in
Idaho, USA and controls
significant silver and cobalt assets in the Canadian Cobalt Camp,
including more than 50 past producing mines.
On behalf of First Cobalt Corp.
Trent Mell
President & Chief Executive Officer
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Exchange) accepts responsibility for the adequacy or accuracy
of this release.
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SOURCE First Cobalt Corp.