Except
as otherwise noted in the Companys Annual Information Form and the Companys
financial statements and related managements discussion and analysis of
financial condition and results of operations of the Company that are
incorporated by reference into this Prospectus (see Documents Incorporated by
Reference), the financial information contained in such documents is expressed
in Canadian dollars.
The
high, low, average and closing exchange rates for the United States dollar in terms
of Canadian dollars for each of the financial periods of the Company ended
September 30, 2017, December 31, 2016, December 31, 2015 and June 30, 2015,
as quoted by the Bank of Canada, were as follows:
On March 12, 2018, the exchange rate for the United
States dollar in terms of Canadian dollars, as quoted by the Bank of Canada, was
US$1.00 = $1.2830.
DOCUMENTS INCORPORATED BY REFERENCE
The
following documents filed with the securities commission or similar regulatory
authority in each of the provinces of British Columbia, Alberta and Ontario, are
available at
www.sedar.com
and are specifically incorporated by reference
into, and form an integral part of, this Prospectus:
-
the annual information form of the Company dated March 28, 2017 (the
Annual Information Form
);
-
the audited consolidated financial statements of the Company, and the notes
thereto for the year ended December 31, 2016, six months ended December 31,
2015 and the year ended June 30, 2015, together with the independent auditors
report thereon and the associated managements discussion and analysis of
financial condition and results of operations for the year ended December 31,
2016;
5
-
the condensed interim consolidated financial statements, and the notes
thereto, for the three and nine months ended September 30, 2017 and 2016, and
the associated managements discussion and analysis of financial condition and
results of operations for the nine months ended September 30, 2017;
-
the management information circular of the Company dated April 20, 2017
distributed in connection with the Companys annual general and special
meeting of shareholders held on June 1, 2017;
-
the material change report dated January 26, 2017 regarding the closing of
the Companys brokered private placement of common shares; and
-
the term sheet of the Company dated March 13, 2018 with respect to
the Offering (the
Marketing
Materials
).
Material
change reports (other than confidential reports), business acquisition reports,
annual financial statements, interim financial statements, the associated
managements discussion and analysis of financial condition and results of
operations and all other documents of the type referred to in section 11.1 of
Form 44-101F1 of National Instrument 44-101
Short Form Prospectus
Distributions
to be incorporated by reference in a short form prospectus,
filed by the Company with a securities commission or similar regulatory
authority in Canada after the date of this Prospectus and before completion or
withdrawal of the Offering, will be deemed to be incorporated by reference into
this Prospectus. The documents incorporated or deemed to be incorporated herein
by reference contain meaningful and material information relating to the Company
and readers should review all information contained in this Prospectus and the
documents incorporated or deemed to be incorporated by reference herein.
In
addition, to the extent that any document or information incorporated by
reference in this Prospectus is included in a report that is filed or furnished
to the SEC on Form 40-F, 20-F or 6-K (or any respective successor form), such
document or information shall also be deemed to be incorporated by reference as
an exhibit to the registration statement on Form F-10 of which this Prospectus
forms a part. In addition, if and to the extent indicated therein, the Company
may incorporate by reference into the registration statement on Form F-10 of
which this Prospectus forms a part documents that the Company files with or
furnishes to the SEC pursuant to Section 13(a) or 15(d) of the U.S. Exchange
Act.
Any statement contained in a document incorporated or deemed to be
incorporated by reference herein will be deemed to be modified or superseded for
the purposes of this Prospectus to the extent that a statement contained in this
Prospectus or in any subsequently filed document that also is or is deemed to be
incorporated by reference herein modifies or supersedes such statement. Any
statement so modified or superseded will not constitute a part of this
Prospectus, except as so modified or superseded. The modifying or superseding
statement need not state that it has modified or superseded a prior statement or
include any other information set forth in the statement or document that it
modifies or supersedes. The making of such a modifying or superseding statement
will not be deemed an admission for any purpose that the modified or superseded
statement, when made, constituted a misrepresentation, an untrue statement of a
material fact or an omission to state a material fact that is required to be
stated or that is necessary to make a statement not misleading in light of the
circumstances in which it was made.
Copies
of the documents incorporated herein by reference may also be obtained on
request without charge from the Corporate Secretary of Auryn Resources Inc.,
Suite 600, 1199 West Hastings Street, Vancouver, British Columbia, V6E 3T5,
Telephone: 778-729-0600.
MARKETING MATERIALS
The
Marketing Materials are not part of this Prospectus to the extent that the
contents of the Marketing Materials are modified or superseded by a statement
contained in this Prospectus. Any template version of any marketing
materials (each as defined in National Instrument 41-101
General
Prospectus Requirements
) filed under the Companys profile on SEDAR at
www.sedar.com
after the date of this
Prospectus and before the termination of the distribution under the Offering
(including any amendments to, or an amended version of, the Marketing Materials)
will be deemed to be incorporated by reference into this Prospectus.
6
THE COMPANY
The
Company was incorporated under the name Georgetown Capital Corp. under the
Business Corporations Act
(British Columbia) on June 9, 2008. The Company
was a Capital Pool Company under the policies of the TSX Venture Exchange. The
Company completed a qualifying transaction with Full Metal Minerals USA Inc. in
February 2011. On October 15, 2013, the Company changed its name to Auryn
Resources Inc.. The Companys registered and records office is located at 1500
Royal Centre, 1055 West Georgia Street, P.O. Box 11117, Vancouver, British
Columbia, V6E 4N7. The Companys head office is located at Suite 600-1199 West
Hastings Street, Vancouver, British Columbia, V6E 3T5.
The
Companys common shares are listed on the TSX and NYSE American under the
trading symbol AUG.
The
Company has five wholly-owned subsidiaries, North Country Gold Corp., Homestake
Resource Corporation (
Homestake
) and Homestake Royalty Corp., all
incorporated under the laws of British Columbia, and Corisur Peru S.A.C.
(
Corisur
) and Sombrero Minerales S.A.C., both incorporated under the
laws of Peru.
The
Companys principal mineral property is the Committee Bay gold project (the
Committee Bay Project
) located in Nunavut, Canada. It is comprised of
more than 380,000 hectares situated along the Committee Bay Greenstone Belt
approximately 180 km NE of the Meadowbank mine operated by Agnico Eagle Mines
Limited and extends more than 300 km northeast.
The
Company also holds a 100% interest in the Homestake Ridge project (the
Homestake Ridge Project
) located within the Iskut-Stewart-Kitsault
belt, in northwestern British Columbia. The Homestake Ridge Project is comprised
of approximately 7,500 hectares and is located in the Kitsault Mineral district
of British Columbia. The Homestake Ridge Project is located 32 km southeast of
Stewart, British Columbia at the southern extent of the Cambria ice field,
accessible by fixed wing aircraft or helicopter.
The
Company has acquired the rights to a portfolio of gold and copper projects
located in the Tacna province of Southern Peru (including the Sombrero
gold-copper project, the Banos del Indio gold project, Huilacollo and Curibaya)
(collectively, the
Peruvian Portfolio
). The Peru Portfolio encompasses
more than 50,000 hectares within the prolific Pliocene Au/Ag epithermal and
Miocene Cu/Au porphyry belts.
Further
information regarding the business of the Company, its operations and its
mineral properties, including the Committee Bay Project, the Homestake Ridge
Project, and the Peruvian Portfolio can be found in this Prospectus under the
heading Mineral Properties, as well as in the Companys Annual Information
Form and the materials incorporated by reference into this Prospectus. See
Documents Incorporated by Reference.
MINERAL PROPERTIES
Committee Bay, Nunavut, Canada
On
June 16, 2017, the Company filed a technical report entitled Technical Report
on the Committee Bay Project, Nunavut Territory, Canada with an effective date
of May 31, 2017 with respect to its Committee Bay Project (the
Original 2017
Committee Bay Technical Report
). On November 3, 2017, the Company filed an
amended and restated technical report entitled Technical Report on the
Committee Bay Project, Nunavut Territory, Canada dated October 23, 2017 with an
effective date of May 31, 2017 with respect to its Committee Bay Project
prepared by David A. Ross, M.Sc., P.Geo of Roscoe Postle Associates Inc.
(
RPA
) (the
Amended 2017 Committee Bay Technical Report
). The
Amended 2017 Committee Bay Technical Report amended the Original 2017 Committee
Bay Technical Report to remove an incorrect reference to the previous 2013
mineral resource estimate being current and to confirm that the current mineral
resource estimate in the Amended 2017 Committee Bay Technical Report, which is
effective May 31, 2017, reflected updated metal price, exchange rate and
operating cost assumptions.
7
The following information on the Committee Bay Project is a summary of the
Amended 2017 Committee Bay Technical Report and is qualified by reference to the
Amended 2017 Committee Bay Technical Report in its entirety. Readers are
encouraged to review the Amended 2017 Committee Bay Technical Report under the
Companys profile at
www.sedar.com
. This
information supersedes the information on the Committee Bay Project included in
the section of the Annual Information Form entitled Committee Bay Project. The
information derived from the Amended 2017 Committee Bay Technical Report
supersedes the information derived from the technical report entitled Technical
Report on the Three Bluffs Project, Nunavut Territory, Canada dated August 17,
2015 (the
2015 Committee Bay Technical Report
). For clarity, the
Company is not relying on any information derived from the 2015 Committee Bay
Technical Report in this Prospectus.
Property Description and Location
The
Committee Bay Project is located in the eastern part of the Kitikmeot Region of
Nunavut, approximately 430 km northwest of the town of Rankin Inlet, Nunavut.
The Committee Bay Project is only accessible by air, either from Rankin Inlet or
Yellowknife, Northwest Territories. The Committee Bay Project is centered at
approximately 7,400,000m N and 570,000m E (NAD 83, Zone 15N) in 1:250,000 scale
map sheets 56J (Waker Lake), 56K (Laughland Lake), 56O (Arrowsmith River) and
56P (Ellice Hills).
Land Tenure
As
of the effective date of the Amended 2017 Committee Bay Technical Report, the
Committee Bay Project consists of three non-contiguous blocks totalling 44 crown
leases, 274 claims and one sub-surface exploration agreement covering IOL
totalling approximately 427,978 ha. Auryn reports that the leases, claims and
the sub-surface exploration agreement are in good standing. Applications are
pending for an additional 13 leases totalling approximately 13,714.5 ha.
On
March 20, 2015, Auryn announced that it had entered into a definitive joint
venture agreement with North Country Gold Corp. (
NCG
) whereby it could
earn a 51% interest in NCGs Committee Bay Project by incurring $6 million in
expenditures over a 30 month period. Of that amount, $500,000 was a firm
commitment to be spent within 12 months. Auryn also agreed to buy 10 million of
NCG shares at a price of $0.05 each as part of a non-brokered private placement.
On
June 30, 2015, Auryn announced that it had entered into a letter agreement with
NCG whereby it would acquire all the NCG shares that it did not already own in
exchange for 13.8 million shares of Auryn valued at approximately $20.4 million.
The Auryn shares issued as part of the agreement constituted approximately 30.7%
of Auryns outstanding shares. On September 25, 2015, Auryn announced that it
had completed the agreement and that NCG had become a subsidiary of Auryn.
Accessibility
The
Committee Bay Project is located 430 km northwest of Rankin Inlet, Nunavut.
Access to Rankin Inlet is achieved via regularly scheduled commercial flights
(Canadian North and/or First Air) from Yellowknife, Northwest
Territories;Winnipeg, Manitoba; and Ottawa, Ontario. Rankin Inlet and Baker Lake
are serviced seasonally by barge and ship. The hamlets of Baker Lake, Naujaat
(Repulse Bay), Gjoa Haven, Taloyoak, and Kugaaruk (Pelly Bay) are accessible by
scheduled commercial flights.
At
the Three Bluffs camp site, Hayes Camp, an esker airstrip is accessible by Twin
Otter fixedwing aircraft on oversized tires from June through early September.
Parts of the Hayes River area are accessible to float-equipped fixed-wing
aircraft by late June. Fixed-wing and helicopter charters may be arranged either
from Rankin Inlet or from Yellowknife. In order to facilitate the mobilization
of large quantities of equipment and supplies for exploration programs, a 5,000
ft airstrip (ice-strip) is constructed each spring on Sandspit Lake at Hayes
Camp.
8
Climate
The
Committee Bay Project is located in the Wager Bay Plateau Ecoregion of the
Northern Arctic Ecozone (Marshall and Schutt, 1999). This ecoregion is
classified as having a low arctic ecoclimate. Summers are short and cold, with
mean daily temperatures above freezing only in July and August. Snow cover
usually lasts from September to June, but it can fall during any month. Most of
the lakes are icebound until approximately mid-July.
Precipitation
is moderate throughout the year, but drifting of snow in the winter can result
in considerable localized accumulations, particularly on the sides of hills. Fog
is often a problem near the coast and at higher elevations particularly during
the late spring to early summer and the fall months.
Table
1 illustrates the major climatic data for the three closest Environment Canada
weather stations, Repulse Bay, Pelly Bay and Gjoa Haven, located approximately
235 km to the east, 220 km to the north, and 290 km to the northwest,
respectively.
TABLE 1 CLIMATIC DATA
Auryn Resources Inc.
Committee Bay Project
|
Repulse Bay
|
Pelly Bay
|
Gjoa Haven
|
Mean January temperature
|
-31.3°C
|
-33°5C
|
-33.8°C
|
Mean July temperature
|
8.8°C
|
9.3°C
|
11.6°C
|
Extreme maximum temperature
|
28.0°C
|
29.0°C
|
33.6°C
|
Extreme minimum temperature
|
-50.0°C
|
-51.5°C
|
-50.6°C
|
Average annual precipitation
|
311.3 mm
|
261.3 mm
|
272.5 mm
|
Average annual rainfall
|
123.8 mm
|
116.6 mm
|
163.4 mm
|
Average annual snowfall
|
215.4 cm
|
146.2 cm
|
126.5 cm
|
|
|
|
|
Source: Environment Canada
|
|
|
|
Local Resources
Most
services are available in Baker Lake, Kugaaruk, and Rankin Inlet, including:
groceries; hotel accommodations; expediting services; and some camp supplies.
Anything that is not locally available can be shipped in via daily scheduled air
services.
The
Rankin Inlet area is a hub of mining activity in the region. Exploration and
mining suppliers and contractors are available from Manitoba and the Northwest
Territories. General labour is readily available from the local communities.
Existing Infrastructure
There
is no permanent infrastructure at the Committee Bay Project. Auryn maintains
three camps to support seasonal exploration campaigns in various portions of the
Committee Bay Project, namely the Hayes Camp (100 person capacity), the Bullion
Camp (20 to 40 person capacity) and the Ingot Camp (10 person capacity). The
Committee Bay Project also benefits from a 914 m, graded, esker airstrip at the
Hayes Camp, a permitted, seasonally prepared 1,580 m winter ice airstrip, which
is constructed on the adjacent Sandspit Lake, and 320m tundra airstrip at the
Bullion Camp. A drill water system is maintained at the Three Bluffs site.
History
Key
historical events are:
-
1961 and 1967: Mapping done in the area by the Geological Survey of Canada
(GSC);
9
-
1970: King Resources Company conducted reconnaissance geological mapping
and sampling in the Laughland Lake and Ellice Hills areas. Follow-up work
includes geophysics and detailed mapping, trenching, and sampling;
-
1970, 1974, and 1976: Cominco Ltd. carried out reconnaissance and detailed
geological mapping, ground geophysics, and sampling in the Hayes River area;
-
1971: The Aquitaine Company conducted airborne electromagnetic (EM) and
magnetometer surveys;
-
1972 to 1977: Detailed re-mapping of the area was done by the GSC;
-
1979: Urangesellschaft Canada Ltd. carried out reconnaissance airborne
radiometric surveys and prospecting for uranium in the Laughland Lake area;
-
1986: Wollex carried out geological mapping and rock sampling in the West
Laughland Lake area;
-
1992: GSC conducted geological re-assessment of the mineral potential of
the Prince Albert Group;
-
1994: Channel sampling carried out over the Three Bluffs area but the
results were lost;
-
1996: Terraquest Ltd. conducted a high-resolution airborne magnetometer
survey;
-
1997 to 1998: P.H. Thompson Geological Consulting Ltd. conducted regional
geological mapping in the Three Bluffs area;
-
1999 to 2002: GSC conducted a multi-disciplinary study of the Committee Bay
Greenstone Belt; and
-
1992 to 2012: APEX carried out prospecting, rock sampling, gridding,
airborne and ground geophysics, geological mapping, and reverse circulation
and diamond drilling on several of the gold targets including Three Bluffs,
Three Bluffs West, West Plains, Anuri, Inuk, Antler, and Hayes.
Past Production
There
has been no previous production from the Committee Bay Project.
Geology and Mineralization
The
Committee Bay area, situated in the Churchill Structural Province, is underlain
by Archean and Proterozoic rocks and extensively covered by Quaternary glacial
drift. It comprises three distinct Archean subdomains (Prince Albert Group,
Northern Migmatite, and Walker Lake Intrusive Complex).
The
Committee Bay Greenstone Belt (the
CBGB
), which hosts the gold
occurrences discussed in the Amended 2017 Committee Bay Technical Report, is
composed of Prince Albert Group rocks. These are bounded by the wide,
northeast-striking Slave-Chantrey mylonite belt to the northwest and by the Amer
and Wager Bay shear zones to the south. Two major fault systems, the
northeast-striking Kellet fault and the northwest-striking Hayes River fault,
intersect the central portion of the CBGB and cut the Prince Albert Group rocks.
Gold occurrences in the CBGB appear to be spatially related to the major shear
systems and their sub-structures indicating the potential for the
re-mobilization of mineral-bearing fluids along these structures.
The
regional strike of rock units in the West Laughland Lake area is generally north
but shows a degree of variability. Units, generally vertically dipping in much
of the CBGB, have a more moderate to shallow dip at Four Hills. Rocks generally
strike northeast from Four Hills east to Committee Bay. In the Hayes River area,
the east-striking Walker Lake shear zone is the dominant structure. Dips in the
Hayes River area are generally sub-vertical and there is evidence of flexural
shear and silicification along lithological contacts between iron formation and
talc-actinolite schist (meta-komatiite). Rocks of the Curtis River
area, approximately 120 km northeast of the Hayes River area, strike northeast
and dip sub-vertically.
10
The
iron formations that host the Three Bluffs, Antler, Hayes, and Ledge gold
occurrences have unique lithological associations with their contact rocks and
do not appear to be stratigraphically equivalent.
Three
low, rounded, rusty outcrops, called West, Central, and East, comprise the Three
Bluffs gold occurrence. Gold mineralization is hosted in gossanous,
predominantly oxide, silicate, and sulphide facies iron formations. Iron
formation thicknesses range from 25 m to 30 m at the West Bluff to 55 m at the
Central Bluff. The Three Bluffs iron formation maintains a thickness of 10 m for
a minimum strike length of 1.8 km and is at least 55 m thick for 700 m. The iron
formations are poorly banded to massive with locally shared, quartz-veined
intervals of up to three metres near lithological contacts. Chlorite and epidote
alteration indicates either lower amphibolite grade metamorphism
(epidote-amphibolite facies) or the result of retrograde greenschist facies
metamorphism associated with gold deposition. Local mineralization, composed of
disseminated pyrite and pyrrhotite, can occupy up to 50% of the rock volume.
Exploration Status
The
Three Bluffs deposit is at the Mineral Resource development stage. The remainder
of the Committee Bay Project is at the early exploration stage.
During
2017, the Company announced the results from its Rotary Air Blast (
RAB
)
drill program at THE Committee Bay Project. The results received represent
approximately 30,000 meters across approximately 150 drill holes targeting areas
away from the existing Three Bluffs deposit. Highlights from the drilling are as
follows:
-
Aiviq prospect - 12.2 meters of 4.7g/t Au (including 3.05 meters of 18.09
g/t Au) intersected in an interpreted silicified shear zone;
-
Aarluk prospect - 4.57 meters of 2.52 g/t gold was intersected in banded
iron formation;
-
West Plains prospect - 9.15 meters of 3.48g/t Au (including 6.1 meters of
4.93 g/t Au), 9.15 meters of 2.89g/t Au and 6.10 meters of 2.54g/t Au
(including 1.53 meters of 7.48 g/t Au) all intersected in banded iron
formation; and
-
Inuk prospect - 25 meters of 1.15g/t Au (including 3.05 meters of 4.13g/t
Au) 400 meters away from the historic intercept of 12.6 meters of 16.04 g/t Au
within sulphidized banded iron formation.
Committee Bay RAB Drilling QA/QC Disclosure
Intercepts
were calculated using a minimum of a 0.25 g/t Au cut off at beginning and end of
the intercept and allowing for no more than four consecutive samples (six
meters) of less than 0.25 g/t Au.
Analytical
samples were taken using 1/8 of each 5ft (1.52m) interval material (chips) and
sent to ALS Lab in Yellowknife, Northwest Territories and Vancouver, British
Columbia for preparation and then to ALS Lab in Vancouver, British Columbia for
analysis. All samples are assayed using 30g nominal weight fire assay with
atomic absorption finish (Au-AA25) and multi-element four acid digest
ICP-AES/ICP-MS method (ME-MS61). Quality Assurance/Quality Control
(
QA/QC)
programs using internal standard samples, field and lab
duplicates and blanks indicate good accuracy and precision in a large majority
of standards assayed.
In
2015 and 2016, Auryn completed a total of 95 RAB holes for approximately 13,045
m and seven diamond drill holes for approximately 3,715 m on the Committee Bay
Project. This drilling was located on new prospects and did not affect the
current Mineral Resources.
11
Mineral Resources
The
Mineral Resources at the Committee Bay Project are estimated to be approximately
2.07 million tonnes of Indicated Mineral Resources grading 7.85 g/t Au,
containing 524,000 ounces of gold, and 2.93 million tonnes of Inferred Mineral
Resources grading 7.64 g/t Au, containing 720,000 ounces of gold. Compared to
the previous Mineral Resource estimate prepared by RPA in 2013, the tonnage has
decreased and the grades have increased due to a higher cut-off grade based on
the current metal price, exchange rate, and operating cost assumptions.
The
estimate was carried out using a block model method constrained by wireframe
gradeshell models, with Inverse Distance Cubed (ID3) weighting. Two sets of
wireframes and block models were employed: one contemplated open pit mining and
the other, underground mining. A lower set of cut-off criteria were used for the
open pit versus the underground to reflect the lower costs that should be
incurred by mining from surface. To fulfil the resource criteria of reasonable
prospects for eventual economic extraction, a preliminary pit shell was
generated from the open pit model. Blocks from the open pit model captured
within this shell were considered eligible for reporting as open pit resources.
The same pit shell was applied to the underground model, except that blocks from
this model were included in the resource only if they were outside of the shell.
Mineral Reserves
There
are no mineral reserves on the Committee Bay Project.
Adjacent Properties
The
Committee Bay Project is contiguous with claims held by various companies and
individuals. None of the adjacent claims are known to host mineralized zones
comparable to the Three Bluffs deposit. No reliance was placed on any
information from adjacent properties in the estimation and preparation of the
Mineral Resources reported in Amended 2017 Committee Bay Technical Report.
Adjacent properties are therefore not deemed material.
Conclusions
The
Committee Bay Project is located within the granite-greenstone rocks of the
Archean Prince Albert group, a component of the Rae Domain within the Western
Churchill Province. The Three Bluffs gold deposit is characterized by a thick
interval of iron formation that appears to form the nose of an upright isoclinal
antiform. The majority of the gold mineralization is hosted in silicate, oxide,
and/or sulphide facies iron formation. Gold mineralization has also been
identified in shear hosted quartz veins in sedimentary and volcanic rocks.
Drilling
has outlined mineralization with three-dimensional continuity, and size and
grades that can potentially be extracted economically. Project geologists have a
good understanding of the regional, local, and deposit geology and controls on
mineralization. The geological models are reasonable and plausible
interpretations of the drill results.
Exploration
protocols for drilling, sampling, analysis, security, and database management
meet industry standard practices. The drill hole database was verified by RPA
and is suitable for Mineral Resource estimation work.
The
previous resource model prepared by RPA in April 2013 remains representative of
the mineralization. There has been no new drilling in the immediate area of
those resources. The cut-off grades were adjusted based on an updated metal
price, exchange rate, and operating cost assumptions and the updated Mineral
Resource was assigned a new effective date of May 31, 2017.
Mineral
Resources for the Three Bluffs deposit were estimated assuming combined open pit
and underground mining methods. At cut-off grades of 3.0 g/t Au for open pit and
4.0 g/t Au for underground, Indicated Mineral Resources are estimated to total
2.07 Mt at an average grade of 7.85 g/t Au containing 524,000 ounces gold. At the same cut-off grades, Inferred Mineral Resources are
estimated to total 2.93 Mt at an average grade of 7.64 g/t Au containing 720,000
ounces gold. The open pit Mineral Resources were constrained by a preliminary
pit shell generated in Whittle software. Underground Mineral Resources are
reported at the high cut-off grade outside of the pit shell.
12
The
limited metallurgical testwork conducted so far suggests that the gold can be
recovered by conventional means, such as a combination of gravity and flotation
followed by cyanide leaching of the concentrate. In RPAs opinion, however,
additional metallurgical testwork is warranted.
The
Committee Bay Project covers virtually all of the Committee Bay supracrustal
belt which hosts a regionally significant and highly prospective corridor for
gold. Previous exploration on the Committee Bay Project did not effectively
screen the large property holdings. Auryns exploration strategy is both
successful and cost effective. Auryns work in 2015 and 2016, which covers
approximately 85% of the current property holdings, was able to highlight 17
significant gold in till anomalies, several of which are located away from any
previously known gold occurrences. There is good potential to discover
additional mineralization and to add to the resource base on the Property.
Recommendations
RPA
has reviewed and concurs with Auryns proposed exploration programs and budgets.
Phase 1 of the recommended work program will include a desktop review of the
2015 and 2016 exploration results in an effort to define the most effective
exploration program to determine the source of the recently identified 17 gold
in till anomalies. The field portion of Phase 1 will consist of boulder mapping,
detailed infill till sampling, and ground magnetics to identify the highest
probability targets which will be immediately drill tested. In addition to the
target follow-up, Phase 1 exploration should include the completion of the
regional till sampling and drone programs over the remaining 15% of the CBGB.
The
Phase 1 program is anticipated to include collection of 17,000 detailed infill
till samples and 2,350 regional till samples and completion of 1,200 km2 of
drone coverage and 25,000 m of RAB drilling. The Phase 1 program is estimated to
cost approximately $20 million. Details of the recommended Phase I program can
be found in Table 2 below.
TABLE 2 PROPOSED BUDGET PHASE 1
Auryn
Resources Inc. Committee Bay Project
Item
|
|
$
|
|
PHASE 1
|
|
|
|
Head Office Expenses
|
|
228,000
|
|
Project Management/Staff Cost
|
|
2,462,000
|
|
Expense Account/Staff Travel
|
|
1,771,000
|
|
Lease Payments
|
|
157,000
|
|
Till Sampling
|
|
685,000
|
|
Ground Magnetics
|
|
200,000
|
|
Drone Surveying
|
|
93,000
|
|
RAB Drilling
|
|
4,863,000
|
|
Assaying/Analyses
|
|
1,084,000
|
|
Camp Costs
|
|
650,000
|
|
Air Support
|
|
5,936,000
|
|
Subtotal
|
|
18,129,000
|
|
Contingency
|
|
1,813,000
|
|
TOTAL
|
|
19,942,000
|
|
13
A
Phase 2 exploration program, contingent on the results of Phase 1, will mainly
consist of drilling. Initially, all of the Three Bluffs drill core should be
re-logged so that controls on mineralization can be better understood. Following
that, 5,000 m to 10,000 m of exploration diamond drilling is proposed at Three
Bluffs to test for the continuity of high grade mineralization at depth and
along strike from the current deposit. In addition to the focused work at Three
Bluffs, it is recommended that any significant RAB drill intersections from the
Phase 1 program be followed up with additional RAB drilling and focused diamond
drilling. It is also anticipated that additional targets will be identified
during the completion of the regional program and these will have to be targeted
using a systematic approach, which includes boulder mapping, detailed infill
till sampling, and ground magnetics.
The
Phase 2 exploration program is anticipated to include the completion of both
diamond and RAB drilling, along with the collection of surface samples. The
recommended Phase 2 program is estimated to cost between $20 million and $25
million. Details of the recommended Phase 2 program can be found in Table 3
below
.
TABLE 3 PROPOSED BUDGET PHASE 2
Auryn
Resources Inc. Committee Bay Project
Item
|
|
$
|
|
PHASE 2
|
|
|
|
Head Office Expenses
|
|
250,000
|
|
Project Management/Staff Cost
|
|
2,500,000
|
|
Expense Account/Staff Travel
|
|
1,800,000
|
|
Lease Payments
|
|
157,000
|
|
Till Sampling
|
|
500,000
|
|
RAB Drilling
|
|
2,000,000
|
|
Diamond Drilling
|
|
6,000,000
|
|
Assaying/Analyses
|
|
1,000,000
|
|
Resource Estimate Update
|
|
65,000
|
|
Metallurgical Test Work
|
|
100,000
|
|
Air Support
|
|
6,000,000
|
|
Camp Costs
|
|
700,000
|
|
Subtotal
|
|
21,172,000
|
|
Contingency
|
|
2,117,000
|
|
TOTAL
|
|
23,289,000
|
|
Homestake Ridge, British Columbia, Canada
On
October 12, 2017, the Company filed a technical report entitled Technical
Report on the Homestake Ridge Project, Skeena Mining Division, Northwestern
British Columbia dated September 29, 2017 with an effective date of September
1, 2017 (the
Original 2017 Homestake Ridge Technical Report
) with
respect to the Homestake Ridge Project located in the Skeena Mining Division,
northwestern British Columbia, Canada. On November 3, 2017, the Company filed an
amended and restated technical report with respect to its Homestake Ridge
Project entitled Technical Report on the Homestake Ridge Project, Skeena Mining
Division, Northwestern British Columbia dated October 23, 2017 with an
effective date of September 1, 2017 prepared by David A. Ross, M.Sc., P.Geo. and
Paul Chamois, M.Sc.(A), P.Geo. of RPA (the
Amended 2017 Homestake Ridge
Technical Report
). The Amended 2017 Homestake Ridge Technical Report
amended Section 6 of the Original 2017 Homestake Ridge Technical Report in order
to clarify that (i) certain resources originally referred to as Historical
Estimates had been reported in prior NI 43-101 technical reports, and
accordingly were not Historical Estimates within the meaning of NI 43-101, and
(ii) to remove reference to the previous historical 2013 resource estimate
remaining current, given that the Original 2017 Homestake Ridge Technical
Report and the Amended 2017 Homestake Ridge Technical Report provided and
updated resource estimate with an effective date of September 1, 2017.
14
The purpose of the Original 2017 Homestake Ridge Technical Report and Amended
2017 Homestake Ridge Technical Report was to support the disclosure of an
updated Mineral Resource estimate. RPA visited the property from August 26 to
28, 2017. The effective date of the updated Mineral Resource estimate is
September 1, 2017.
The
following information on the Homestake Ridge Project is a summary of the Amended
2017 Homestake Ridge Technical Report and is qualified by reference to the
Amended 2017 Homestake Ridge Technical Report in its entirety. Readers are
encouraged to review the Amended 2017 Homestake Ridge Technical Report under the
Companys profile at
www.sedar.com
. The
information derived from the Amended 2017 Homestake Ridge Technical Report
supersedes the information derived from the technical report entitled Technical
Report on the Homestake Ridge Project, an Updated Mineral Resource, Kitsault,
British Columbia dated effective June 7, 2013 and readdressed November 15, 2016
(the
2013 Homestake Ridge Technical Report
). For clarity, the Company
is not relying on any information derived from the 2013 Homestake Ridge
Technical Report in this Prospectus.
Property Description and Location
The
Homestake Ridge Project covers 7,547.15 ha and is located approximately 32 km
southeast of Stewart, British Columbia, and approximately 32 km north-northwest
of the tidewater communities of Alice Arm and Kitsault, BC. The property is
located within NTS 1:50,000 scale topographic map 102/P13. It is centred at
approximately 55° 45' 12.6" N latitude and 129° 34' 39.8" W longitude on Terrain
Resource Integrated Management (TRIM) maps 103P072 and 103P073 and lies within
Zone 9 of the UTM projection using the NAD83 datum.
Land Tenure
The
Homestake Ridge Project comprises four non-contiguous blocks consisting of seven
crown grants and 36 mineral claims covering a total area of 7,547.15 ha in the
Skeena Mining Division. The crown grants include surface rights, while the
mineral claims do not include surface rights.
On
June 14, 2016, Auryn announced that it had entered into a binding letter
agreement whereby it would acquire all the issued and outstanding common shares
of Homestake. On September 8, 2016, Auryn announced that it had completed a plan
of arrangement and that Homestake had become a wholly-owned subsidiary of Auryn.
Homestake holds a 100% interest in the Homestake Ridge Project, subject to
various royalty interests on certain claims held by vendors, with some claims
requiring annual royalty payments.
Accessibility
The
Homestake Ridge Project is located 32 km southeast of Stewart, BC, at the
southern extent of the Cambria ice field. Access to the Homestake Ridge Project
from the town of Kitsault is by boat/barge to the community of Alice Arm. From
there, an upgraded tractor trail follows an old railway bed for a distance of 32
km into the area of the past producing Dolly Varden silver mine, approximately
four kilometres from the southern boundary of the Homestake Ridge Project. From
there, overgrown mule trails lead to the historic workings of the Vanguard and
Homestake areas of the Homestake Ridge Project. Helicopters are available for
charter from either Prince Rupert, Terrace, or Stewart.
Climate
Climate
in the area is classified as Oceanic or Marine West Coast and is characterized
by moderately cool summers and mild winters with a narrower annual range of
temperatures compared to sites of similar latitude. Climate data derived from
the closest monitoring station (Nass Camp) indicates that temperatures range
from an average low of -6.6°C in January to an average high of 21.6°C in July.
The mean temperature for the year is 5.3°C.
15
The
area receives 1,065 mm of precipitation each year (expressed in mm of water).
Rainfall peaks in October with 165 mm. Snowfall is highest in December and
January when accumulations are 92 cm and 91 cm respectively. The property is
reported to be covered in snow from late September to late June. Precipitation
and heavy fog often impact on airborne access to the Homestake Ridge Project.
Local Resources
The
Homestake Ridge Project is located north of the historic mining towns of
Kitsault and Alice Arm. Both towns are located at Alice Arm, a branch of the
Observatory Inlet and part of the Portland inlet system which hosts Canadas
most northerly, ice-free, deep sea port at Stewart.
Sprott
Power Corp. (Sprott Power) initiated development of six hydroelectric projects
in the Upper Kitsault Valley. To facilitate the construction, roads and bridges
are being upgraded in that area. Sprott Power is also redeveloping shutdown
hydroelectric utilities in the area including the Kitsault dam and powerhouse.
The Government of British Columbia has announced the resurfacing of 18 km of
Highway 113, which will improve access to Kitsault from Terrace.
Labour
and supplies for the Homestake Ridge Project can be brought in from Terrace,
which lies 185 km to the south, along Highway 113. Terrace has a population of
12,109 (2001 census) and hosts wide range of supplies, services, and trained
labour. Terrace is serviced by three air carriers with daily scheduled flights.
Existing Infrastructure
There
is no permanent infrastructure at the Homestake Ridge Project. A temporary camp
capable of housing 40 people was established at 55°44.406 N and 129°35.128 W
for the duration of the 2017 exploration program.
History
The
Homestake Ridge Project comprises two areas of historic exploration. The
Homestake and the Vanguard groups have been tested by past explorers starting in
the early 1900s after the discoveries at Anyox and in the Stewart region. Claims
were first staked at the Homestake group between 1914 and 1917. In 1925, the
original claims were given Crown Grant status.
In
1939, the property was optioned by British Lion Mines Ltd. British Lion Mines
Ltd. conducted extensive trenching and excavated two (Smith and Myberg) adits,
shipping eight tonnes of selected ore that returned 1,120 g Au, 1,617 g Ag, 63.5
kg Pb, 303 kg Zn and 599 kg Cu from the Homestake group of claims. This is the
only known production from the property.
In
1947, a cross-cut adit was begun on the Nero claim (operator unknown) that
formed part of the Vanguard group. Work continued until the early 1950s when the
claims were abandoned.
In
1964, Dwight Collison of Alice Arm staked the area, conducted surface trenching,
limited underground work, and drilled seven holes for an aggregate of 58.2 m, on
the Lucky Strike and Cascade claims which make up part of the Homestake group.
In 1966, Canex Aerial Exploration Ltd. undertook an exploration program and in
1967, Amax Exploration conducted and extended examination of the Vanguard group.
In
1979, Newmont Exploration of Canada Ltd. optioned part of the property, which
excluded the original Homestake and Vanguard claims and targeted near surface
massive sulphides. Newmont Exploration of Canada Ltd. terminated the option in
late 1980. Caulfield Resources Ltd. explored the Vanguard group in 1981, but no
subsequent work was done.
Homeridge
Resources Ltd. optioned the property in 1984, but no work was done. The claims
were allowed to lapse in 1986, were re-staked and optioned to Cambria Resources
Ltd., which completed geological mapping, lithogeochemical sampling, trenching
and 4.3 line km of IP and resistivity surveys.
16
The ground was optioned to Noranda Exploration
Company Limited. Between 1989 and 1991, Noranda Exploration Company Limited
consolidated ground by optioning more area including the Cambria, Homestake, and
Vanguard claims. Geological mapping and geophysical surveys were conducted and
twelve diamond drill holes were cored for a total of 1,450.05 m.
Teck
Resources Limited acquired the current Homestake Ridge property in 2000 via
option agreements and staking. From 2000 to 2002, Teck Resources Limited
conducted geochemical and geological surveys, trenching, and drilling for
volcanogenic massive sulphide (VMS) deposits.
Homestake
(formally Bravo Venture Group) optioned the property from Teck Resources Limited
in 2003. Homestakes work, prior to 2009, consisted of the compilation of
historic data, the performance of geochemical and geophysical surveys,
geological mapping, and the drilling of 27,289 m in 120 NQ2 and BTW diamond
drill holes. In 2007, Homestake released a NI 43-101-compliant Mineral Resource
estimate at a 0.5 g/t AuEq cut-off grade which totalled 11.9 Mt in the Inferred
category grading 2.36 g/t Au, 15.0 g/t Ag, and 0.11% Cu.
From
2008 to 2009, resumed diamond drilling and was successful in confirming the
known mineralized zones as well as discovering the Homestake Silver Zone located
approximately 700 m to the southeast of the Main Homestake deposit.
In
2010, Scott Wilson RPA prepared an updated NI 43-101 compliant Mineral Resource
estimate for the Homestake Ridge Project at a 3 g/t AuEq cut-off grade which
totalled 888,000 t in the indicated category grading 6.69 g/t Au, 47.2 g/t Ag
and 0.15% Cu and 2.34 Mt in the inferred category grading 4.62 g/t Au, 106 g/t
Ag and 0.13% Cu.
From
2010 to 2012, Homestake completed additional surface exploration including
further mapping, soil and rock sampling, 13.54 line km of IP surveying, and
diamond drilling resulting in the identification of new exploration targets and
the significant expansion of Mineral Resources estimate on the Homestake Ridge
Project.
In
April of 2011, Homestake announced the results of an updated Mineral Resource
estimate at the Homestake Silver Zone by RPA, which resulted in a significant
increase in the inferred resources of the previous estimate. The reported
resource at a 3.0 g/t AuEq cut-off grade totalled 888,000 t in the indicated
category grading 6.69 g/t Au, 47.2 g/t Ag and 4.1 Mt in the inferred category
grading 4.62 g/t Au, 103 g/t Ag.
In
2011 a new discovery was made 800 m to the southwest of, and parallel to, the
Main Homestake and Homestake Silver deposits. This area, known as the South Reef
target was tested by three holes with all three intersecting +30 g/t Au
mineralization.
During
2012, Homestake completed two phases of drilling focussed on the delineation and
extension of the South Reef target. The second phase of drilling was funded by
Agnico Eagle Mines Limited as part of an option agreement (see below). The 2012
drilling was successful in identifying an approximate 250 m strike by 250 m down
dip before ending in, or being offset by, a major fault structure.
Mineralization is open along the strike to the northwest. Other targets remain
on the property.
Agnico
Eagle Mines Limited optioned the property from Homestake in 2012. From 2013 to
2014, Agnico Eagle Mines Limited completed exploration consisting of
prospecting, reconnaissance geological mapping, soil sampling, a limited amount
of ground geophysical (magnetics and IP) surveying and diamond drilling
consisting of 16 holes totalling approximately 6,525 m. The drilling suggested
that the Slide Zone is concordant with the Homestake Main and Homestake Silver
zones and trends north northwesterly and dips steeply to the northeast. The
option was subsequently terminated.
Past Production
In
1939, British Lion Mines Ltd. shipped eight tonnes of selected ore that returned
1,120 g Au, 1,617 g Ag, 63.5 kg Pb, 303 kg Zn, and 599 kg Cu from the Homestake
group of claims. This is the only known production from the Homestake Ridge
Project.
17
Geology and Mineralization
The
Homestake Ridge Project is located within a lobe of Upper Triassic to Middle
Jurassic strata exposed along the western edge of the Bowser Basin within the
Stikinia Terrane of the Intermontane Belt. Stikinia formed in the Pacific Ocean
during Carboniferous to Early Jurassic (320 Ma to 190 Ma) and collided with
North America during the Middle Jurassic.
The
Homestake Ridge Project occurs within the metallogenic region known as the
Stewart Complex. Described as the contact of the eastern Coast Plutonic Complex
with the west-central margin of the successor Bowser Basin, the Stewart Complex
ranges from Middle Triassic to Quaternary in age and is comprised of
sedimentary, volcanic and metamorphic rocks.
The
Homestake Ridge Project covers the transition between the sedimentary and
volcanic rocks of the Upper Triassic to Lower Jurassic Stuhini Group, a complex
sequence of Lower to Middle Jurassic sedimentary, volcanic and intrusive rocks
of the Hazelton Group and sedimentary rocks of the Upper to Middle Jurassic
Bowser Lake Group.
The
Lower Hazelton rocks comprise fine-grained to feldspar-hornblende phyric
volcanic and volcaniclastic rocks of andesite to latite/trachyte composition and
may include some phases of hypabyssal monzonite. This lower stratigraphy of the
Hazelton Group extends along the length of the Homestake Ridge from the Main
Homestake Zone to the Vanguard Copper showings and is the host rock and footwall
sequences to the three known mineral deposits, the Main Homestake, Homestake
Silver and South Reef zones as well as numerous other showings.
The
cessation of Hazelton volcanism and continued sub-basin development resulted in
a rapid facies changes into calcareous sandstones, grits, and conglomerates
progressing upwards to thinly laminated and alternating beds of black graphitic
and pyritic mudstones and light grey siltstones or very fine-grained sandstones
(possible pyjama beds) correlated to the Salmon River formation.
In
the northern part of the property at the headwaters of Homestake Creek,
rhyolitic volcanic rocks occur at the base of the Salmon River sediments.
The
eastern part of the property is dominated by the Middle to Upper Jurassic Bowser
Basin Group which conformably overlies the thin bedded graphitic argillites of
the Salmon River formation.
Structure
on the property largely reflects northeast-southwest compression that has
continued from the Jurassic to present day. Recent drilling and mapping suggest
that the local stratigraphy has undergone several deformation events including
uplift and local extension of the Stuhini and lower Hazelton stratigraphy. Large
northeast trending ankerite bearing faults have been mapped and related to
Tertiary east-west extension.
Exploration Status
Since
acquiring the Homestake Ridge Project, Auryn has completed a limited amount of
induced polarization surveying, a soil sampling program and a 15,000 meter
diamond drill program. On December 12, 2017, the Company announced the results
of its 15,000-meter core drilling program at the Homestake Ridge Project. The
program targeted 2 of 7 target areas identified away from the existing deposits
and was successful in identifying the plunge of the high-grade South Reef zone.
Highlights include 30 meters of 2.00 g/t Au (including 4m @ 6.03g/t Au & 2m
@ 11.80 g/t Au), 10 meters of 4.12 (including 2m @ 18.01 g/t Au), 18m of 1.29g/t
Au (including 4m of 4.18g/t Au), 8m of 2.67 g/t Au (including 2m of 7.4 g/t),
and 14m of 1.23g/t Au. These results identified the geometry of the high-grade
mineralization at the South Reef main zone that remains open to the northwest
and importantly have identified an emerging parallel high-grade structure (Upper
zone) 175 meters to the north of the main zone. These results do not have a
material impact of the Homestake Ridge Resource statement presented in Table 4.
18
Homestake Ridge Drilling QA/QC Disclosure
Intercepts
were calculated using a minimum of a 0.2 g/t Au cut off at beginning and end of
the intercept and allowing for no more than four consecutive meters of less than
0.2 g/t Au.
Analytical
samples were taken by cutting NQ diameter core into equal halves on site and
sending one of the halves to ALS Laboratories in Terrace, BC, Vancouver, BC or
Thunder Bay, ON for preparation and analysis. All samples are assayed using 30g
nominal weight fire assay with atomic absorption finish (Au-AA23) and
multi-element four acid digest ICP-AES/ICP-MS method (ME-MS61). Where AA23
results were > 5 g/t Au the assay were repeated with 30g nominal weight fire
assay with gravimetric finish (Au-GRA21). QA/QC programs using internal standard
samples, field and lab duplicates and blanks indicate good accuracy and
precision in a large majority of standards assayed.
Mineral Resources
The
current Mineral Resource estimate for the Homestake Ridge Project is summarized
in Table 4 below.
TABLE 4 - MINERAL RESOURCE STATEMENT AS AT SEPTEMBER 1, 2017
Auryn Resources Inc. Homestake Ridge Project
Classification
|
Tonnage
|
Gold
|
Gold
|
Silver
|
Silver
|
Copper
|
Copper
|
|
(Mt)
|
(g/t)
|
(oz)
|
(g/t)
|
(Moz)
|
(%)
|
(Mlb)
|
Indicated
|
0.624
|
6.25
|
125,000
|
47.9
|
1.0
|
0.18
|
2.4
|
Inferred
|
7.245
|
4.00
|
932,000
|
90.9
|
21.2
|
0.11
|
16.9
|
Notes:
|
|
1.
|
CIM Standards were followed for Mineral
Resources.
|
2.
|
Mineral Resources are estimated at a cut-off grade of 2.0
g/t AuEq.
|
3.
|
Assumptions used to calculate AuEq values are described
in the Amended 2017 Homestake Ridge Technical Report.
|
4.
|
Mineral Resources are estimated using a long-term gold
price of US$1,300 per ounce, and a US$/C$ exchange rate of 1.2.
|
5.
|
A minimum horizontal width of two metres was
used.
|
6.
|
Bulk density ranges from 2.66 t/m3 to 2.85 t/m3 depending
on the domain.
|
RPA
updated the Mineral Resource estimate for the Homestake Ridge Project at a
cut-off grade of 2 g/t (AuEq). Grades for gold, silver, copper, arsenic and
antimony were estimated into the blocks using ID3 weighting. Three block models,
one for each of the three main deposit zones, were created in 2013 using GEMS
software. Block size for all models was 5 m x 5 m x 5 m. The wireframe models
were constructed in Surpac by Homestake personnel working in consultation with
RPA. The assay data comprised drilling and trench sampling results from programs
conducted by Homestake.
The
main areas of the deposit are the Homestake Main Zone, the Homestake Silver
Zone, and the South Reef Zone. The Homestake Main Zone is the more copper-rich
of the zones, with both gold-rich and silver-rich variants and an apparent trend
of increasing copper grade with depth. The Homestake Main Zone consists of a
broad corridor of sub-parallel anastomosing zones which strike approximately
137° and dip steeply to moderately to the northeast. Most of the zones dip at
75° to 80°, flattening to 45° in the central section between elevations 750 MASL
and 900 MASL. Widths range from centimetre-scale to four metres in true
thickness. Locally, the zones are observed to jog abruptly in a left-lateral
sense which is attributed to cross-faulting. These disruptions can be 30 m or
more. The Homestake Main Zone has been traced on surface and in drill intercepts
for a strike length of 750 m, and a vertical extent of approximately 500 m.
Mineral Reserves
There
are no Mineral Reserves at the Homestake Ridge Project.
Adjacent Properties
The
Homestake Ridge Project is contiguous with claims held by a number of companies
and individuals:
19
-
Dolly Varden Resources
- located approximately 25 km north of Alice
Arm, the Dolly Varden property comprises 9,374 ha and includes two former
producing silver mines - the Dolly Varden Mine and the Torbrit Mine. The
property is owned by Dolly Varden Silver Corporation, which holds surface
rights over some of these mineral claims. The Dolly Varden property adjoins
the southern boundary of the property and is underlain by similar a
volcano-sedimentary stratigraphy belonging mostly to the lower and middle
Jurassic Hazelton Group.
-
Kinskuch Property
- Homestake optioned the claim group in March
2011. Homestake could earn an 85% interest by making advanced minimum royalty
payments totaling $580,000 and spending $3,000,000 in work on the property
over a four-year period. The remaining 15% interest could be purchased from
the optionor for $2,000,000 and granting a 2% net smelter return
(
NSR
) royalty, of which 1% may be purchased for $1,000,000. The
vendors are an independent group that staked and previously explored the
claims. Subsequently, Homestake let this option lapse and no longer has an
interest in the property.
-
Avanti Mining Inc.
- Located at the head of Alice Arm, the property
is the host of the rehabilitated Kitsault open pit mine. The property is 100%
owned by Avanti Kitsault Mine Ltd., a wholly owned subsidiary of Avanti Mining
Inc. A 1% NSR is held by Aluminerie Lauralco Inc. which may be purchased for
US$10 million within 90 days of the presentation of a bankable feasibility
study.
Conclusions
The
Homestake Ridge Project is located within the prolific Iskut-Stewart-Kitsault
Belt which hosts several precious and base metal mineral deposits. Diverse
mineralization styles include stratabound sulphide zones, stratabound
silica-rich zones, sulphide veins, and disseminated or stockwork sulphides.
Mineralization is related to Early Jurassic feldspar-hornblende-phyric
sub-volcanic intrusions and felsic volcanism and commonly occurs with zones of
pyrite-sericite alteration. Numerous genetic models can be proposed for the area
and local deposits present a broad range of characteristics.
Drilling
has outlined mineralization with three-dimensional continuity, and size and
grades that can potentially be extracted economically. Project geologists have a
good understanding of the regional, local, and deposit geology and controls on
mineralization. The geological models are reasonable and plausible
interpretations of the drill results. Exploration protocols for drilling,
sampling, analysis, security, and database management meet industry standard
practices. The drill hole database was verified by RPA and is suitable for
Mineral Resource estimation work.
RPA
updated the Mineral Resource estimate for the Homestake Ridge Project using the
block model dated December 31, 2012 and a AuEq cut-off grade based on adjusted
metal price, exchange rate and operating cost assumptions. No new drilling
information has been received within the resource area and therefore a new
effective date of September 1, 2017 was assigned to the Mineral Resource
estimate. Data from the drilling being carried out in the late summer and fall
of 2017 is expected to be received in October or November of 2017, and the
Mineral Resource model and statement will be updated.
Mineral
Resources were estimated considering a potential underground mining scenario. At
a cut-off grade of 2 g/t AuEq, Indicated Mineral Resources were estimated to
total 0.624 Mt at average grades of 6.25 g/t Au, 47.9 g/t Ag, and 0.18% Cu. At
the same cut-off grade, Inferred Mineral Resources were estimated to total 7.245
Mt at average grades of 4.00 g/t Au, 90.9 g/t Ag, and 0.11% Cu. There are no
Mineral Reserves estimated on the Homestake Ridge Project.
The
wireframe models of the mineralization have done a reasonably good job of
segregating the various zones (domains) within the deposit. The sample
statistics show that there are still multiple populations within some of the
domains. In RPAs opinion, this may be due to higher grade zones within the
relatively lower grade wireframes. Additional interpretive work may be able to
segregate these higher grade domains, which would result in more robust grade
interpolations.
20
Results from metallurgical test work suggest that the expected recoveries from a
combined gravity/flotation processing plant would be: 85% to 93% for gold; 75%
to 88% for silver; 85% to 90% for copper.
Recommendations
Exploration
work carried out at the Homestake Ridge Project by previous operators and Auryn
has identified significant gold, silver and base metal mineralization. Previous
operators focused on stratabound mineralization models similar to that of Eskay
Creek. Homestake highlighted several key structures that appear to be the main
control on mineralization throughout the property. Work expanded the previously
known mineralization in addition to identifying previously unknown
mineralization corridors within the Homestake Ridge Project boundaries.
Following up on these structures and structural corridors is highly recommended.
A two phase multi-year program is recommended to complete additional exploration
and resource definition drilling followed by a preliminary economic assessment.
RPA
has reviewed and concurs with Auryns proposed exploration programs and budgets.
Phase 1 of the recommended work program will build on the results of the 2017
exploration program by expanding and infilling both newly discovered zones of
mineralization as well as known deposits with the aim of completing an updated
mineral resource estimate. To complete Phase 1, it is recommended that a 20,000
m diamond drilling program be completed. Details of the recommended Phase I
program can be found in Table 5 below.
TABLE 5 - PROPOSED BUDGET PHASE 1
Auryn
Resources Inc. Homestake Ridge Project
Item
|
$
|
PHASE 1
|
|
Head Office Expenses and Property Holding Costs
|
500,000
|
Geologic and Support Staff Cost
|
2,000,000
|
Geophysical and Drone Surveys
|
250,000
|
Surface Sampling and XRF
|
500,000
|
Diamond Drilling
|
7,500,000
|
Assaying/Analyses
|
1,125,000
|
Camp Costs
|
650,000
|
Helicopter Support
|
2,500,000
|
Engineering and Baseline Studies
|
500,000
|
Subtotal
|
15,525,000
|
Contingency
|
1,552,500
|
TOTAL
|
17,077,500
|
A
Phase 2 exploration program, contingent on the results of Phase 1, will also be
diamond drill focussed with the goal of determining the extent of mineralization
around the existing deposits and increasing the confidence level in certain
areas of the resource by way of additional in-fill drilling. The goal of the
Phase 2 drilling would be to bring the resource to the point that it could
support the preparation of a preliminary economic assessment in 2019. In
addition to the resource targeted drilling, it is recommended that satellite
mineralized zones be investigated to determine their significance as the
Homestake Ridge Project advances. It is recommended that the Phase 2 program
consist of 20,000 m of drilling in addition to environmental, engineering and
metallurgical studies as required to support a preliminary economic assessment.
Details of the recommended Phase 2 program can be found in Table 6 below:
21
TABLE 6 - PROPOSED BUDGET PHASE 2
Auryn
Resources Inc. Homestake Ridge Project
Item
|
$
|
PHASE 2
|
|
Head Office Expenses and Property Holding Costs
|
750,000
|
Geologic Staff and Support Staff Cost
|
3,000,000
|
Geophysical and Drone Surveys
|
250,000
|
Surface Sampling and XRF
|
350,000
|
Diamond Drilling
|
7,500,000
|
Assaying/Analyses
|
1,125,000
|
Engineering and Baseline Studies
|
1,500,000
|
Helicopter Support
|
2,500,000
|
Camp Costs
|
750,000
|
Subtotal
|
17,725,000
|
Contingency
|
1,772,500
|
TOTAL
|
19,497,500
|
Peruvian Portfolio
On October 11, 2017, the Company
filed a technical report entitled Technical Report for the Huilacollo Project,
Tacna Province, Southern Peru dated October 10, 2017 with an effective date of
September 29, 2017 (the
2017 Huilacollo Technical Report
) with respect
to its Huilacollo property (the
Huilacollo Property
) prepared by
Michael B. Dufresne, M.Sc., P.Geolo., P.Geo. and Bahram Bahrami, B.Sc., P.Geo.
of APEX Geoscience Ltd. (
APEX
).
The following information on the
Huilacollo Property is derived from a summary of the 2017 Huilacollo Technical
Report and is qualified by reference to the 2017 Huilacollo Technical Report in
its entirety. The 2017 Huilacollo Technical Report is incorporated herein by
reference and readers are encouraged to review the 2017 Huilacollo Technical
Report under the Companys profile at
www.sedar.com.
Property Description and Location
The Huilacollo Property
encompasses 5 contiguous concessions totalling 3,300 hectares (
ha
) in
the Tacna Province of southern Peru approximately 10 km northwest of the border
with Chile and 55 km northeast of the City of Tacna, Peru.
Land Tenure
Auryn holds its interest in the
Huilacollo Property through Corisur which acquired the rights to the Huilacollo
Property in three separate transactions with private Peruvian companys/owners.
Corisur may acquire 100% interest in the 5 concessions, subject to an NSR, and
through a combination of work expenditures and cash payments. A summary of the
three transactions is described as follows:
|
|
In June 2016, Corisur acquired the Huilacollo 1 and
Huilacollo 2 concessions (2,000 ha) through an option agreement with a
local Peruvian company, Inversiones Sol S.A.C Under the Huilacollo option,
Corisur may acquire 100% interest of the Huilacollo Property, subject to
an NSR, and through a combination of work expenditures and cash payments
that total US$15.75 million, as detailed in Table 7 below. The Huilacollo
NSR is 1.5% and 2.5% for precious metals and base metals, which is buyable
for US$2.5 million and US$7.0 million, respectively;
|
22
TABLE 7 HUILACOLLO OPTION EXPENDITURES AND CASH
PAYMENTS
Due
Dates
|
|
|
Property
|
|
|
Work
Expenditures
|
|
|
|
|
Payments
|
|
|
|
|
Effective Date (May 11, 2016)
|
paid
|
|
US$ 250,000
|
|
|
US$
-
|
|
May 11, 2018
|
|
|
500,000
|
|
|
2,000,000
|
|
May 11, 2019
|
|
|
-
|
|
|
3,000,000
|
|
May 11, 2020
|
|
|
250,000
|
|
|
-
|
|
May 11, 2021
|
|
|
250,000
|
|
|
2,000,000
|
|
May
11, 2022
|
|
|
7,500,000
|
|
|
-
|
|
Total
|
|
|
US$ 8,750,000
|
|
|
US$ 7,000,000
|
|
|
|
In August 2017, Corisur acquired 3 additional concessions
(1,100 ha) through transactions with private Peruvian owners; the
concessions are known as the Tacora, Tacora Sur and Andamarca concessions.
Corisur can acquire 100% interest in the 3 concessions with direct
payouts, and the concessions are subject to individual
royalties:
|
|
|
|
|
|
|
o
|
Under the terms of the Tacora acquisition agreement,
Corisur paid US$200,000 on signing of the public deed transferring the
concessions in favor of Corisur. The Tacora concessions are subject to a
0.5% NSR, 50% of which is buyable for US$0.5 million; and
|
|
|
|
|
|
|
o
|
Under the terms of the Andamarca acquisition agreement,
Corisur paid US$450,000 on signing of the public deed transferring the
concession in favor of Corisur. The Andamarca concession is subject to
1.5% NSR, 50% of which is buyable for US$2.5
million
|
The Huilacollo Property is located within a special economic
zone situated within 50 km of the Peruvian border. As a non-resident company,
Auryns right to ultimately exploit these licenses or register its interests
require approval from the Peruvian government in the form of a Supreme Decree.
Auryn is in the process of submitting its applications with respect the approval
and anticipates receiving the approval prior to exercising it rights to take
ownership over Corisur.
Accessibility
Access
to the Huilacollo Property from Lima takes about 4.5 hours of travel using
commercial airlines and a vehicle. There are daily flights between the cities of
Lima and Tacna in the south. Flight time is approximately 1.5 hours. The easiest
access to the Huilacollo Property is via the Tacna-La Paz International Road. At
kilometre 108, a branch road to the west leads to the property. After about 1.5
hrs, the main part of the Huilacollo Property is visible from the road. Once on
the Huilacollo Property, access is by dirt drill roads or foot. Total driving
time from Tacna is approximately 3 hours.
Climate
Weather
is typical of high altitude regimes (the Huilacollo Property is at 17º 39
Latitude South). Cold temperatures and dry conditions dominate during the months
of May through September while heavy rain, hail and snow can all occur from
November to April. Temperatures vary between a few degrees centigrade below zero
during the night, up to 20°C during the day in the last months of the year
although colder temperatures are possible. The thermal chill factor, however,
may be much lower due to the common wind. Temperature and precipitation
statistics are not available for the Huilacollo Property.
Tacna,
which is located some 120 km away and at a much lower elevation, has a mild
desert climate (BWn, according to the Köppen climate classification) with
average high and low temperatures of 23.5°C and 12.6°C. The nearest community
with readily available weather statistics is Talabaya located approximately 1.5
hrs north of the Huilacollo Property. Talabaya is significantly cooler than
Tacna with average high and low temperatures of 12.0°C and 8.0°C. The rainy
season is mainly between November and April, reaching its peak average
precipitation in January at 198 mm. Peak snowfall days occur in May and July
averaging 7.5 cm (6 days) and 6.1 cm (4 days), respectively. The amount of daily
sunlight is fairly constant at this latitude; between 111 hrs/month (March) to
146 hrs/month (November).
23
Local Resources and Infrastructure
There
are no permanent buildings or infrastructure on the Huilacollo Property. A
temporary camp capable of housing 40 people was established for the duration of
the 2017 exploration program. The Town of Talabaya is the nearest locale to
purchase supplies. Talabaya is located 1.5 hrs north of the project area on the
international road. The Town of Palca is located about 2 hrs from the project on
the International Road. It has approximately 2,000 inhabitants with telephone
lines and daily bus connections to Tacna.
Tarata,
the capital city of the Pachía District, is located to the north of the project
and can be reached in 2.5 hours. There are daily bus connections with
surrounding communities, plus telephone and internet connections in Tarata.
Fuel, food and basic lodging are available, as is some heavy equipment such as
bulldozers. A limited supply of unskilled workers is also available in Tarata. A
high-wattage power line crosses about 5 km north of the property boundary.
The
Huilacollo Property is being assessed by Auryn for its oxide gold-silver
mineralization potential within a property-wide area of hydrothermally altered
volcanics (roughly 4 by 6 km). The deposit type is believed to be consistent
with epithermal gold/silver (Au/Ag) mineralization. The Huilacollo Property is
situated in a documented epithermal gold and silver volcanic belt of Southern
Peru that is known to host significant gold deposits including the Pucamarca
Mine, which is located 15 km south of the Huilacollo Property, is currently in
production and is owned by Minsur.
History
Much
of the following details for the historic exploration is taken from a prior
technical report. Early exploration/mining was carried out in the southeastern
part of the current Huilacollo Project (within the Huilacollo 2 concession).
This area was the site of mining activity focused on high-grade base and
precious metal veins. The largest accessible remaining workings is an adit that
is approximately 42 m in length. The remainder of the workings are caved-in or
flooded. Little is known about this activity except that it occurred before
modern exploration.
In
the late 1970s, a governmental German-Peruvian consortium called Cooperación
Minera Peruano- Alemana explored for porphyry copper-style mineralization at
Santa Elena, which is south of the Huilacollo Property boundary. Geological
mapping, geophysical surveys (Induced Polarization) and the subsequent test
drilling of four diamond drillholes for a total of 900 m were completed.
Argillized and silicified pyritic volcanics with little to no copper were
intersected during drilling, which resulted in work ending on the Huilacollo
Property in 1979 and the claims being abandoned in 1984.
In
the early 1990s the Huilacollo Property was sampled and mapped at a scale of
1:20,000 by Mr. Jaime Suarez, who took 139 rock chip samples that revealed
scattered anomalous gold values. This led to the main Huilacollo concessions
being staked in 1992. Since then, the Huilacollo Property was explored by
Cominco (Peru) S.R.L., a subsidiary of Cominco Ltd., and Balaclava Resources
S.A. in the 1990s. In the 2000s, the Huilacollo Property was explored by Alturas
Minerals S.A.. These companies conducted numerous exploration programs that
included: detailed- to reconnaissance-scaled geological mapping; ground
geophysical surveys; trench and surface sampling along with drilling. The ground
work defined an intense alteration corridor with a spatial extent of
approximately 5 km x 1 km. Four high-sulphidation alteration centers were
identified: Cerro Andamarca, Andamarca Norte, Cerro Huilacollo and Cerro
Colorado. Cerro Andamarca is topographically the highest and may comprise the
upper levels of a high-sulphidation alteration system. The other three centers
show mainly advanced argillic and argillic alteration and the roots of
gold-silver siliceous structures. Two of these zones, Cerro Andamarca and
Andamarca Norte have been drill tested.
24
Geology and Mineralization
The
Huilacollo Property is underlain by an Upper JurassicCretaceous
volcano-sedimentary sequence that has been intruded by predominantly
granodiorite stocks of Upper Cretaceous to Lower Tertiary age. This sequence is
folded and faulted along predominately northwest-southeast lineaments. These
units are overlain by dacitic to andesitic tuffs and flows of the Tarata and
Huilacollo Formations, which are thought to be time equivalents of the Oligocene
to early Miocene Tacaza Group.
The
Huilacollo Property is dominated by the gently folded volcanics of the
Huilacollo Formation, overlain by the Barroso Group. Three lithostratigraphic
packages can be recognized: the oldest and lowermost is an alternating sequence
of volcaniclastics and lavas of andesitic composition, belonging to the upper
part of the Huilacollo Formation. A sequence of rhyolitic pyroclastics (lapilli
and ash fall tuffs, plus volcanic breccia) discordantly overlies this unit. The
youngest and uppermost sequence is dominated by slightly altered dacitic to
andesitic lavas. The middle sequence is either part of the Huaylillas Formation
or the Lower Barroso Group. The upper sequence is probably part of the Upper
Barroso Group.
The
volcanic sequences are cut by intrusive stocks and dykes. Stocks are syenitic-
to monzogranitic in composition and occupy the topographically lower parts of
the property. The dykes tend to have a dacitic composition. Quartz-tourmaline
and sericite alteration is well developed around the contacts of both types of
intrusive. Although there is no conclusive evidence to link them together, it is
likely that the syenitic- to monzogranitic intrusive rocks drove the
high-sulfidation systems on the Huilacollo Property.
Two
steep fault systems cut the gently-dipping volcanic sequence, the first strikes
northwest and the second strikes northeast. These fault systems probably
controlled emplacement of the syenitic- to monzogranitic stocks and the magmatic
hydrothermal breccias. Later movements on these faults may have controlled
supergene processes and the northeast striking set probably acted as
domino-style normal faults that accommodated broadly north-south extension. The
north- and northwest-striking faults appear to spatially control an 5.0 km x 1.0
km belt of intense high sulfidation alteration.
Five
areas of interest, possibly representing separate high-sulfidation hydrothermal
alteration centers, have been defined within the Huilacollo Property: Andamarca
Norte, Cerro Andamarca, Cerro Huilacollo, Cerro Colorado and Corisurs newly
identified Cerro Soroche. Cerro Andamarca is topographically the highest and
comprises the upper levels of a high-sulfidation system. The other four centers
show widespread mainly advanced argillic alteration and siliceous structures
with more localized gold-silver anomalies.
To
date, most of the historical exploration work, and hence potential for economic
epithermal gold mineralization, has been focused on a manto-shaped
shallow-dipping siliceous breccia around the crest of Cerro Andamarca. The zone
can potentially be expanded based on apparent down-faulted extensions to the
east, west and north towards, in particular, Andamarca Norte.
Zones
of high grade gold and silver are controlled by favorable shallow-dipping
pyroclastic volcanic units and by steeply-dipping, silicified and brecciated
structures. Gold-silver grade correlates strongly with the development of the
vuggy silica and massive grey silica alteration, with the abundance of secondary
hematite and limonite after sulfides.
Exploration
Recent
work by Corisur has demonstrated that geophysics, specifically IP surveys, have
assisted in expanding the silicified target zones, which are manifested as high
resistivity and low to moderate chargeability anomalies. The Cerro Andamarca
target is a 700 x 700 m shallow resistivity anomaly that has to date only been
explored by drilling on its eastern margin where the mineralization outcrops on
the hill crest over an area of 400 x 200 m. The Andamarca Norte target is a
1,100 x 350 m, shallow resistivity anomaly that again has only been explored by
widely spaced drilling on its eastern extremity and contains widespread gold in
soil, rock and talus samples. Further sampling along with additional ground
geophysical surveys are warranted for Cerro Andamarca and Andamarca Norte.
25
Extensive
soil/talus sampling by Corisur across the southern two thirds of the Huilacollo
Property area in 2016 has identified significant precious metal geochemical
anomalies at Cerro Huilacollo, Cerro Colorado and Cerro Soroche. The soil/talus
precious metal anomalies warrant follow-up exploration including further
sampling, trenching, ground geophysical surveys followed by drilling.
On
October 23rd, 2017, the Company announced its plans for an initial drill program
at Huilacollo. This program will include a minimum of 5,000 meters across the
north of the Huilacollo project and will focus on the considerable expansion of
the areas around the historic drilling at the top of Andamarca hill. A second
phase of drilling will be planned for 2018 where continuous surface sampling,
spectral analysis, and trenching is ongoing. Results from this surface program
will define additional drill targets across the recently defined 1.8 kilometers
of greater than 50 ppb gold in soil anomalies on the southern portion of the
project and the newly acquired highly prospective Tacora concession.
As
of the date of this prospectus, the Company has completed approximately 1,500
meters of the program with no significant results received to date.
Mineral Resources
There
have been no known Mineral Resource estimates completed on the Huilacollo
Property.
Adjacent Properties
The
most significant nearby property of interest is the Pucamarca Gold-Silver Mine
owned by Minsur S.A., which is located 15 km southeast of the Huilacollo
Property up against the Peru-Chile border in Tacna Province, Southern Peru. The
Pucamarca Mine was put into production in 2012 with its first gold produced in
early 2013. The initial mineable mineral resource for the project upon start-up
was listed at 34.24 million tonnes with an average grade of 0.72 g/t Au and 6.72
g/t Ag for a total of 793,000 troy ounces of gold and 7.7 million troy ounces of
silver (BNAmericas report dated August 28, 2009). No details for the resource
are reported.
A
little more distant is the Santa Rosa and Cerro Tucari mines of Aruntani S.A.C.
located approximately 100 km to the northwest of the Huilacollo Property. The
mineralization at these two mines was discovered in 1997 and 2000, respectively,
with commencement of production in 2002 and 2004, respectively. The two mines
are still in production and were producing in the early years at roughly 100,000
ounces per annum for Santa Rosa and 200,000 ounces per annum for Cerro Tucari.
Recommendations and Conclusions
Based
upon widespread visible alteration across the Huilacollo Project including
silicification, hematization and advanced argillic alteration in combination
with the recent results of exploration by Corisur including, soil/talus
sampling, trenching and ground IP surveys, an aggressive exploration over all
areas and targets displaying significant alteration. Exploration should consist
of lithological alteration mapping, drone photo and elevation surveys,
continued soil/talus sampling, additional trenching along with ground
geophysical surveys including ground magnetic surveys and additional infill and
extended IP surveys. The ground work should be followed up with drilling at each
of the five target areas. The Phase 1 exploration fieldwork budget (exclusive of
drilling) is estimated at US$1.65 million, as detailed below.
Additional
geological mapping that leads to a new integrated lithological, structural and
alteration interpretation of the historical drilling and well mapped surface
geology in the northern half of the Huilacollo Property area. A
northeast-southwest structural trend is well recognized in the field and in the
ground geophysics and is likely an important control on high grade precious
metal mineralization.
The
proposed exploration plan for the Huilacollo Property includes ground IP and
magnetic surveys to cover the whole project area including the newly acquired
Tacora area. The aim should be to complete, extend and infill the previous
surveys completed in 2006 for Alturas and 2016 for Corisur. To date, the ground
IP surveys have mapped precious metal mineralization spatially related to silica
alteration, which is characterized by high resistivity and low chargeability. Additional surveying should be conducted
to extend previous lines and infill areas of only reconnaissance level
surveying. Final products should include inversion modeling and pseudo 3D
modelling in conjunction with other targeting criteria.
26
It
is recommended that the remainder of the Huilacollo Property be surveyed with
additional and complete soil and/or talus sampling surveys to identify new
geochemical trends and flesh out the already known trends. The Tacora area
requires at least a first pass reconnaissance survey. Soil and talus geochemical
sampling should be followed up with strategically located trenches in the areas
with strong geochemical anomalies. An initial 1,500 m trenching program is
proposed for Phase 1 exploration.
An
aggressive drilling program should be conducted using diamond core drilling.
Phase 1 drilling should be focussed at existing drill ready targets with about
10,000 m at Andamarca and Andamarca Norte with a goal of expanding the known
precious metal mineralization at both targets. The estimated cost to conduct the
Phase 1 drilling is US$4.5 million, as detailed below. The Phase 1 drilling is
not dependent on any further exploration results. A Phase 2 program of
exploration drilling that consists of 25,000 m of core and reverse circulation
drilling should be planned that will be a combination of resource definition and
exploration should be planned and budgeted. This Phase 2 drilling program will
depend partially upon the results of the Phase 1 ground exploration and drilling
program.
The
recommended exploration and budget for Phase 1 is detailed in Table 8 below:
TABLE 8 - PHASE 1 RECOMMENDED EXPLORATION AND BUDGET
Phase 1 Andamarca Drilling
|
|
Cost/m
|
|
|
Target Area (Type)
|
(approx.)
|
Quantity (m)
|
Cost
|
Andamarca (Core)
|
$450/m
|
5,000
|
$2,250,000
|
Andamarca Norte
(core)
|
$450/m
|
5,000
|
$2,250,000
|
|
Drilling
Subtotal
|
10,000
|
$4,500,000
|
|
Phase 1 Property Wide Activities
|
Activity Type
|
|
|
Cost
|
Geological Mapping
& Consulting
|
|
|
$50,000
|
Drone Orthophoto
& DEM Survey
|
|
|
$100,000
|
Magnetic Surveying
|
|
|
$75,000
|
IP Surveying
|
|
|
$200,000
|
Trenching &
Trench Sampling
|
|
|
$200,000
|
Geochemical Soil -
Talus Sampling
|
|
|
$200,000
|
Metallurgical Test
Work
|
|
|
$25,000
|
Resource Modeling
Studies
|
|
|
$100,000
|
Bonding /
Environmental
|
|
|
$100,000
|
Earthwork /
Reclamation
|
|
|
$50,000
|
Database Management
|
|
|
$18,000
|
Property Maintenance
& Payments
|
|
|
$532,000
|
|
Property Wide Activities Subtotal
|
$1,650,000
|
27
|
|
|
|
|
|
|
Contingency (10%)
|
$615,000
|
|
Grand Total
|
$6,765,000
|
The
Phase 2 exploration program, being contingent on positive results from the Phase
1 program, should include further drilling at the two primary target areas,
Andamarca and Andamarca Norte, as well as first pass drilling at the Cerro
Huilacollo, Cerro Colorado, Cerro Osroche targets and on the Tacora and Tacora
Sur concessions.
The
recommended exploration and budget for Phase 2 is detailed in Table 9 below:
TABLE 9 - PHASE 2 RECOMMENDED EXPLORATION AND BUDGET
Phase 2 Andamarca Drilling
|
|
Cost/m
|
|
|
Target Area (Type)
|
(approx.)
|
Quantity (m)
|
Cost
|
Andamarca (Core)
|
$450/m
|
5,000
|
$2,250,000
|
Andamarca Norte (core)
|
$450/m
|
5,000
|
$2,250,000
|
Tacora/Cerro Huilacollo,
|
|
|
|
|
$450/m
|
10,000
|
$4,500,000
|
Cerro
Colorado/Cerro Soroche
|
|
|
|
|
|
|
|
|
Drilling Subtotal
|
20,000
|
$9,000,000
|
Phase 1 Property Wide Activities
|
|
Activity Type
|
Cost
|
Geological Mapping
& Consulting
|
$100,000
|
Trenching &
Trench Sampling
|
$200,000
|
Geochemical Soil -
Talus Sampling
|
$200,000
|
Metallurgical Test
Work
|
$50,000
|
Resource Modeling
Studies
|
$200,000
|
Bonding /
Environmental
|
$100,000
|
Earthwork /
Reclamation
|
$100,000
|
Database Management
|
$18,000
|
Property Maintenance
& Payments
|
$532,000
|
Property Wide Activities Subtotal
|
$1,500,000
|
|
|
Contingency
(10%)
|
$1,050,000
|
Grand Total
|
$11,550,000
|