TIDMLND
RNS Number : 6178L
Landore Resources Limited
14 January 2021
This announcement contains inside information as defined in
Article 7 of the Market Abuse Regulation No 596/2014
LANDORE RESOURCES LIMITED
(AIM Ticker: LND.L)
SOIL SAMPLING ESTABLISHES
SIGNIFICANT ANOMOLOUS GOLD ALONG STRIKE FROM
THE BAM GOLD PROJECT
JUNIOR LAKE PROPERTY
London, United Kingdom, ---14th January 2021 - Landore Resources
Limited (AIM: LND) ("Landore Resources" or "the Company") is
pleased to report on the results of the 2020 soil sampling program
carried out along strike to the east and west of its BAM Gold
Project ('BAM Gold'), Junior Lake Property, Ontario, Canada.
Highlights:
-- In 2020 Landore completed a new soil-till sampling campaign
covering 2.0 kilometres along strike to the east of BAM Gold. The
2020 campaign successfully established the presence of widespread
anomalous gold and indicated multiple gold trends. The area covered
recorded the highest soil-till assay results to date in both of the
2019/20 soil till campaigns completed on the Junior Lake property
and supports extending the resource drilling from BAM Gold.
-- In addition, an infill soil-till sampling programme was
completed over the 2.1 kilometres strike length to the immediate
west of BAM Gold, with the results confirming the prospectivity of
this area and its potential to contain extensions of BAM Gold.
Drilling has commenced in this area and has intersected similar
geological lithology and mineralisation to BAM Gold.
Commenting on this report, Chief Executive Officer of Landore
Resources, Bill Humphries, said:
"The highly successful soil sampling programmes, completed in
2020 and in 2019, has established the presence of widespread
anomalous gold and multiple gold trends along strike to the east
and west of BAM Gold for a total length of 8 kilometres. These
programmes have identified numerous new drill targets which have
the potential of being advanced into additional resources to
continue the rapid growth of the BAM Gold Project.
Drilling Update:
The drilling programme for 2020-21 at the BAM Gold Deposit is
progressing as planned with a total of 6,518 metres of HQ diamond
core, comprising 30 drill holes, completed to date. All drill holes
have successfully intersected prospective mineralised zones
associated with the BAM Gold Deposit. The drill core has been
logged, processed and sent to ALS Minerals of Thunder Bay for
analysis to date. Assay results are pending and will be reported
once received and collated. The drilling programme is expected to
complete in April 2021.
2020 SOIL SAMPLING PROGRAMME, JUNIOR LAKE PROPERTY
Landore Resources' geological team completed an extensive
exploration campaign during the summer of 2020 which included the
establishment of a cut grid and soil sampling, westwards along
strike for 2.1 kilometres and eastwards along strike for 2
kilometres from the existing BAM Gold Project, successfully
establishing the presence of widespread anomalous gold and multiple
gold trends.
A full report on the 2020 soil sampling programme has been
prepared by the Company (the "2020 Report"), with the key
information from the 2020 Report summarised below. The 2020 Report
containing maps and charts titled '2020 Soil Sampling Programme,
Junior Lake property' and dated January 11 2020 can be viewed on
Landore's website www.landore.com
"Summary
The Junior Lake property is located approximately 230 kilometres
north-northeast of Thunder Bay, ON. The property contains three
NI43-101 compliant mineral resources, two of which are
predominately nickel (B4-7 and VW) and one which is gold (BAM
Gold).
During the summer of 2020 soil sampling was conducted on the
Junior Lake property aimed at infilling and extending the 2019 soil
sampling program (see soil report dated 30 November 2019). A total
of 1013 samples, inclusive of QAQC samples were collected. Soil
sampling consisted of collection of the B horizon at a nominal
spacing of 25m. Numerous areas were unable to be sampled due to
swampy conditions or signs of disturbance from past forestry
operations.
Soil data has indicated exploration targets prospective for
further significant gold mineralization to the east and west of the
currently-defined BAM Gold deposit. Numerous anomalous gold trends
were noted, of which four priority areas are:
1. Continuation of the BAM Gold trend an additional 1.5 km to
the west of which follow up drilling along a portion has had
encouraging results,
2. Anomalous gold values associated with iron formation between
Juno Lake and Boras Lake that are open to the west, towards the
known Lamaune Gold occurrence,
3. Anomalous gold values continuing west towards Juno Lake along
the projected metasedimentary sequence of the BAM gold and the
possibility of a southwest splay from this trend passing just south
of Juno Lake, and
4. The gold trend east of the BAM Gold Deposit has been extended
for a further 2.0km. Gold anomalies continue eastward beyond the
surveyed grid.
The soil sampling program was deemed a successful, low cost tool
for gold exploration and should be expanded to cover the width of
the property.
Introduction
The sampled portions of the grid spanned three separate
areas:
1) The Eastern section of the existing Felix Lake soils grid
from 700W to 2000W. Infilling to obtain coverage at 100 metre
centres along strike (1.3km x 1.7km wide).
2) Extending the existing Junior lake soils grid to the west
from 400E to 600W at 100 metre centres (1km X 1.7km wide).
3) Completing a new soils grid to the East of the BAM Gold
deposit from 3000E to 5000E at 100 metre centres (2km x 1.2km)
A total of 1,013 samples, including 121 reference samples, were
analyzed.
Samples were collected from the B horizon at a nominal distance
of 25m using a Dutch auger. Samples had their location recorded
using a handheld GPS as well as the grid reference. Each sample
also had the depth it was taken and description of colour and
composition noted.
The area was extensively logged 20 years ago. As a result, areas
with obviously disturbed soil, with thick organics or A horizons
>2m, the limit of the soil auger, or conversely no developed
soil profile, were not sampled.
Property Description and Location
The Junior Lake property is located 230km north-northeast of
Thunder Bay, ON and 75km east-northeast of the village of
Armstrong, Ontario. The property is accessible by heading east
along gravel logging roads from the village of Armstrong.
The property consists of 1,158 mineral claims and six mining
leases.
Regional Geology
The Junior Lake property is located within the Caribou Lake -
O'Sullivan greenstone belt of the East Wabigoon Subprovince of the
Superior Province. The greenstone belt ranges from 3.5 - 15 km in
width, north-south, and extends for 80 - 100 km, east-west
(MacDonald, 2006). To the south it is bordered by the Robinson Lake
Batholith of the Lamaune Batholitic Complex and to the north by a
roughly east-west trending fault zone. Northeast of the property
the belt is intruded by the tonalitic to quartz dioritic Summit
Lake Batholith. Nipigon diabase sills and cross-cutting dykes
intrude the western portion of the greenstone belt.
Regional deformation is west to west-northwest trending and
sub-vertical to steeply north dipping foliation and small scale
folding. Metamorphism is generally greenshist, increasing to
amphibolite near the contact of the batholiths.
BAM Gold Deposit
From 2015 to 2020 Landore has explored for gold on the property
conducting multiple drill programs as well as ground geophysics,
soil sampling and geological mapping.
The Junior Lake property is host to the BAM Gold deposit
reporting 31,083,000 tonnes (t) at 1.02 grams/tonne (g/t) for
1,015,000 ounces of gold including 21,930,000t at 1.06g/t for
747,000 ounces gold in the Indicated category (7 January 2020
Mineral Resource Estimate, National Instrument 43-101 ("NI 43-101")
compliant).
2020 Soil Sampling
The sampled portions of the grid spanned three separate
areas:
1) The Eastern section of the existing Felix Lake soils grid
from 700W to 2000W. Infilling to obtain coverage at 100 metre
centres along strike (1.3km x 1.7km wide).
2) Extending the existing Junior lake soils grid to the west
from 400E to 600W at 100 metre centres (1km X 1.7km wide).
3) Completing a new soils grid to the East of the BAM Gold
deposit from 3000E to 5000E at 100 metre centres (2km x 1.2km)
A total of 1,013 samples, including 121 reference samples, were
analyzed.
Samples were collected every 25m using a 4 cm Dutch auger and
placed in clean, brown paper bags specifically designed for this
type of material. Samples had their depth of collection noted as
well as a general description of the sample itself (see Appendix
II). In areas of poor soil development composite samples, when
possible, were taken using multiple holes. Once collected, samples
were dried in camp before shipment to the laboratory.
Duplicate samples were taken (4% of samples) and silica blanks
were inserted (4% of samples). Replicate samples were taken at
thirteen separate locations. The replicate samples consisted of
three or four samples taken on an approximately 1 m x 1 m grid,
where possible.
A total of 1,013 soil samples were submitted to ALS Global Ltd.
of Vancouver for analysis. The samples were analyzed for low level
gold in soils and sediments. The analytical package used was
'Prep-41, Au Me-ST 43' which involves drying at <60(o) C and
sieving to -180 micron followed by aqua regia digestion and ICP-MS
finish for analysis of gold and 42 other elements. The samples
submitted consisted of 893 individual soils, 49 duplicate soils, 24
replicate samples and 48 silica blanks.
QAQC
The duplicate samples taken correspond well. The majority of
elements have 70-90% within +/-20% of the duplicate values, that
increases to >90% of the values when the range is expanded to
+/-30%. The outliers may in part be attributed to the sample sites.
Numerous locations had thin B horizons which resulted in composite
samples being taken. It is likely this contributed to the variation
in duplicates.
The replicate samples were taken at eight separate locations and
consist of three to four samples on an approximate one meter by one
meter square. Of the replicant samples, four of the sites had one
sample of the replicant set with values greater than double the
remaining samples while the other samples were within 20%. Three of
the replicant sets had one sample >20% of the other samples. One
set of replicant samples was within 20% for all samples. The
variability may be a result of a different medium being sampled as
often the sample description is different on the outlier
sample.
After review and consideration, the combined 2019-2020 data set
was used for interpretive purposes.
Soil Sampling Results
To remove anomalous samples, they were screened based on their
description. Samples described as organic rich, black or grey in
colour or clay were considered suspect and may not be
representative of the B horizon. The remaining samples were used
for the calculation of the background value of each element. The
background value is the average of the lower 25% quartile, listed
in Table 2.
Table 1: Select elements' calculated background values.
Element Au Ag As Cu Ni
Background Value 0.261 ppb 0.013 ppm 1.06 ppm 3.78 ppm 5.29 ppm
---------- ---------- --------- --------- ---------
The response ratios (RR) were calculated for all elements by
taking the background value and dividing it into the analytical
value. This was also done for the suspect samples. RRs are rounded
and values of >=5 considered anomalous.
A correlation matrix was also generated for the samples taken.
Gold (Au) showed only a very weak correlation with bismuth, and
chromium. As a result, it was determined that use of the
correlation matrix was not helpful at this time.
An examination of the gold RR showed there were 103 samples with
anomalous values (RR>=5). Of these samples 40 had values of
10-30 while 13 had RR >30. In order to help prioritize them a
criterion of Au+As+Cu RR>5 was used. This criterion was
previously established in 2019 as a signature of the gold
mineralization of the BAM deposit. Seventeen samples were
determined to have the same signature as the BAM deposit. Maps
showing the anomalous sites for Au, As, Ag, Cu, Au+As+Cu are in
Appendix I. As well a map illustrating the trend of the gold within
the soil samples is in Appendix I.
In order to assist in correlating anomalies across lines, the
regional fabric of the area was used. Within the area there is a
general fabric that strikes 105-115(o) , this is highlighted by
completed geophysics (VLF, MaxMin). The geophysics highlights
formation sulphide zones within the area and is used as both marker
horizons and to illustrate the fabric within an area. It is
important to note that there are cross cutting structures within
the area. These structures may play an important role in the gold
mineralization, acting both as pathways and aiding in concentrating
the auriferous fluids. As such they will require additional
investigation and follow-up in the future.
To determine significant anomalies several elements with
RR>=5 were examined, in particular Au, Ag, As, and Cu, with
these elements often being closely associated with gold deposits.
Criterion developed in 2019 established the combination of Au+As+Cu
as being characteristic of the BAM deposit. Using this criteria,
locations with coincident Au+As+Cu, and to a lesser extent Ag,
anomalies were considered to have the same characteristics as the
BAM occurrence and examined in detail. Seventeen sites were found
with coincident Au+As+Cu anomalies, as well as thirteen additional
sites with Au RR>30 of which selected locations are listed in
Table 2.
Table 2: Samples containing anomalous Au+As+Cu and select
samples with anomalous Au. Location and RR values given. A) Felix
Lake Grid. B) Junior Lake Grid. C) Junior Lake East Grid.
A) Felix Lake Grid
Sample Line Station Response Ratio Notes
Au As Cu Ag
---- ---- ---- ---
Samples are along trend with additional Au and Au and Cu
anomalies from the 2019 survey. Trend
is traceable for 800m and may extend for an additional 700m to
A0059943 L1800W 100S 6 66 27 1 the west.
-------- -------- ---- ---- ---- --- ---------------------------------------------------------------
Y068896 L1200W 150S 52 1 4 3
-------- -------- ---- ---- ---- --- ---------------------------------------------------------------
Y068899 L1200W 250S 42 2 1 1
-------- -------- ---- ---- ---- --- ---------------------------------------------------------------
High Au value within previously defined 800m trend of poor
Y068925 L1400W 275S 51 1 10 2 sample coverage.
-------- -------- ---- ---- ---- --- ---------------------------------------------------------------
Samples within swampy region, trend can be correlated to W or
SSW. Trend 800m in length and
can be linked to existing BAM Au mineralization and 2019 soil
A0059722 L400W 375N 8 5 16 4 samples.
-------- -------- ---- ---- ---- --- ---------------------------------------------------------------
A0059706 L300W 450N 32 3 5 2
-------- -------- ---- ---- ---- --- ---------------------------------------------------------------
A0059698 L200W 475N 14 18 7 3
-------- -------- ---- ---- ---- --- ---------------------------------------------------------------
B) Junior Lake Grid
Sample Line Station Response Ratio Notes
Au As Cu Ag
----- ---- --- ---
Locations are part of a large zone of anomalous Cu, As and Au
values surrounding an E-W swampy
area south of the BAM Gold trend. Samples may represent a
A0059413 L000 N300 7 14 9 3 separate, sub-parallel shear.
------- --------- ----- ---- --- --- ---------------------------------------------------------------
A0059415 L000 N350 142 20 2 1
------- --------- ----- ---- --- --- ---------------------------------------------------------------
A0059416 L000 N375 8 16 10 2
------- --------- ----- ---- --- ---
A0059395 L100E N375 6 18 32 6
------- --------- ----- ---- --- ---
A0059397 L100E N450 12 21 12 1
------- --------- ----- ---- --- ---
A0059353 L300E N325 5 60 10 5
------- --------- ----- ---- --- ---
A0059354 L300E N525 5 10 9 2
------- --------- ----- ---- --- ---
A0059460 L400E N400 7 28 14 4
------- --------- ----- ---- --- --- ---------------------------------------------------------------
Locations abo ve and north of the BAM Gold metasedimentary
sequence. Connects to anomalous
A0059471 L500E N600 9 140 96 7 As and Au to the E and to the BAM occurrence.
------- --------- ----- ---- --- --- ---------------------------------------------------------------
A0059473 L500E N650 53 25 7 2
------- --------- ----- ---- --- --- ---------------------------------------------------------------
C) Junior Lake East
Sample Line Station Response Ratio Notes
Au As Cu Ag
---- ---- ---- ---
Samples define a corridor 100-200m wide and approximately 1.9km
E-W. corridor is along strike
from the known BAM Au mineralization. Centered within the
corridor are exploration drill holes
with gold mineralization as well as surface samples with
anomalous Au values. Trend is a continuation
Y069222 L3200E 175S 101 16 32 16 of anomalous values found in 2019.
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Y069224 L3200E 225S 41 3 3 3
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Y069165 L3400E 187.5S 18 12 9 2
-------- -------- ---- ---- ---- ---
Y068831 L3500E 175S 218 8 5 3
-------- -------- ---- ---- ---- ---
Y068829 L3500E 200S 79 1 1 1
-------- -------- ---- ---- ---- ---
Y068991 L4000E 300S 7 5 9 3
-------- -------- ---- ---- ---- ---
Y068995 L4000E 400S 8 17 10 3
-------- -------- ---- ---- ---- ---
Y067660 L4300E 450S 15 24 12 5
-------- -------- ---- ---- ---- ---
Y067743 L4600E 400S 23 303 137 5
-------- -------- ---- ---- ---- ---
Y067799 L4800E 450S 22 7 5 5
-------- -------- ---- ---- ---- ---
Y067757 L5000E 375S 506 1 2 1
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Samples located south of the BAM Au trend and can be loosely
correlated together. They may
represent small offshoots or ballooning of the BAM
Y069247 L3100E 250S 56 5 4 4 mineralization.
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Y067667 L4300E 625S 43 3 1 2
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Samples are located north of the BAM Au trend. Numerous
additional samples with elevated As,
Cu or Ag occur. Northern most samples along surveyed lines show
a weak E-W correlation and
Y068846 L3600E L025N 33 2 2 4 may represent an additional Au trend.
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Y068973 L3700E 100S 28 14 9 2
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Y067703 L4500E 100N 6 58 7 2
-------- -------- ---- ---- ---- ---
Y067702 L4500E 075N 16 32 9 13
-------- -------- ---- ---- ---- ---
Y067818 L4700E 200S 10 28 18 5
-------- -------- ---- ---- ---- ---
Y067757 L5000E 375S 506 1 2 1
-------- -------- ---- ---- ---- --- ----------------------------------------------------------------
Interpretation
Gold appears to respond well to the sampling programs conducted
in both 2019 and 2020. It is possible to link together anomaly
trends across 100s of meters. It is important to not just rely on
the intensity of the RR but to also use a multi-element
classification. This is highlighted when the BAM occurrence is
examined where multiple gram surface samples generate an Au RR of
5-6 in the immediate samples. This criterion is not meant to
exclude single element Au anomalies.
Through use of the soil data the BAM Gold trend was extended
1.1km to the west. Some exploratory diamond drilling has been
conducted on a portion of this extension during fall 2020 and
indicates the gold mineralization continues. Additional anomalies
continue for 1.5km and indicate that the trend may not only
continue but indicates the presence of possible parallel, untested
trends.
To the east of the BAM Gold Deposit the trend has been extended
for a further 2.0km. A portion of this area has already been
sparsely drilled with encouraging results. Two parallel areas of
interest, to the north and south, indicate the possible presence of
addition gold horizons. These horizons may correlate to some of the
anomalous trends to the west of the BAM Gold mineralization,
indicating a possible second and third, untested mineralized
horizon to the north and south of the BAM Gold deposit.
Conclusions and Recommendations
The 2020 soil sampling program was successful in generating
several anomalies of interest as well as expanding on
previously-generated anomalies. Exploration targets to the east and
west of the currently-defined BAM Gold deposit are prospective for
further significant gold mineralization. Gold is shown to respond
well to the low-cost survey which has strong potential for future
exploration.
Recommendations:
- Survey lines should be conducted in areas of interest and to
expand on observed trends. These lines can be done quickly via GPS
and do not require a cut line. Initial line spacing of 200m is
acceptable with the line spacing being reduced to 100m spaced lines
with samples every 25m in areas being infilled. The length of the
infill line should extend a minimum of 100m above and below the
interpreted anomaly.
- Intensive prospecting to be conducted along anomalous gold
trends. Previous work has indicated that unassuming, weakly sheared
surface samples can return significant gold values. Sampling of all
outcrops, where they occur, needs to be conducted in high priority
areas. Ideally samples perpendicular to the trend should be spaced
10m while sampling along the strike of the anomaly <50m.
- Property scale exploration to be done using 500m spaced lines
across areas of interest both east and west.
- Test lines should be done over the Lamaune Gold occurrence to
determine its characteristics and once characterized, additional
iron formations on the project sampled.
From the soil sampling program there are four areas identified
as priority targets:
1. Gold anomaly trend west of Juno Lake, adjacent to the
interpreted BAM Gold metasedimentary sequence. The presence of
anomalous gold values along this trend gives additional strength to
the continuation of gold mineralization along this horizon. The
possibility of a southwest auriferous splay occurring and passing
just south of Juno Lake needs to be evaluated.
2. Follow up on the multiple anomalous trends between Juno Lake
and Boras Lake associated with the iron formations. Unfortunately,
terrain may prove to be a problem as much of the area has thick
overburden. Identification of a fingerprint for the Lamaune Gold
occurrence to the west may assist in narrowing down the
targets.
3. Extend surveyed lines to the north and south of the BAM Gold
deposit to test for possible parallel trends. Evidence of possible
multiple mineralized shears can be interpreted from the soil
sampling.
4. The eastern extension of the Junior Lake grid contains
numerous anomalies including the highest Au RR's (506, 218 and 101)
of the survey. Work in the area includes five exploration diamond
drill holes conducted in 2018. These exploration diamond drill
holes intersected elevated gold values. The 2020 sampling shows a
continuous soil anomaly along the interpreted BAM Gold
mineralization as well as possible additional anomalies to the
north and south. Recommendations in the area consist of:
a. Drilling along the defined trend.
b. Detailed prospecting along the possible anomalous trends to the north and south.
c. Extension of the soil sampling grid to the east to follow along the anomalous values and guide exploration."
End of Extracts
Drilling Update-BAM Gold.
The drilling programme on the BAM Gold Deposit, consisting of
14,000 metres of HQ diamond core, commenced on schedule in October
2020 and is aimed at further infilling and extending the defined
resource of 1,015,000 ounces of gold and to test the depth
potential of the previously delineated mineralisation. The drilling
programme is expected to complete in April 2021.
To date, 30 drill holes have been completed for a total of 6,518
metres, with:
1) 9 holes for 1,425 metres drilled to the immediate west of BAM
Gold extending the existing mineralisation for a further 500
metres. Drilling has intersected similar geological lithology to
BAM Gold.
2) 16 holes for 3,464 metres drilled beneath the west defined
pit shell to test for possible depth extension. All holes
intersected typical BAM Gold lithology and mineralisation,
including some with visible gold. Results are pending.
3) 5 holes for 1,629 metres drilled beneath the deepest part of
the east defined pit shell to test for potential underground mining
potential. All holes intersected typical BAM Gold lithology and
mineralisation, including some with visible gold. Results are
pending.
Considerable delays in receiving assay results are being
experienced in the exploration industry world-wide due to the
significant increase in drilling activity brought upon by the
increase in metal prices, particularly gold. Consequently, ALS
Minerals, one of the leading laboratories, has advised that a
period of 7-8 weeks, from delivery of samples to the laboratory, is
currently required for completion of full analysis.
Drilling will recommence during the next week and is scheduled
to complete in April.
Planning:
At the conclusion of the 2020/21 drilling campaign an updated
Mineral Resource Estimate ("MRE") and Preliminary Economic
Assessment ("PEA") will be prepared on the BAM Gold Deposit.
BAM GOLD DEPOSIT:
The BAM Gold Deposit extends for 3,700 metres from 400E to 4100E
and remains open down dip and along strike to the east and the
west. The BAM Gold Deposit is located approximately mid-way along a
highly prospective Archean greenstone belt which traverses the
Junior Lake Property from east to west for approximately 31
kilometres. The favora ble greenstone belt ranges from 0.5 to 1.5
kilometres wide and hosts multiple known gold occurrences including
the Lamaune Gold Prospect .
Mineral Resource Estimate:
The current MRE for the BAM Gold Deposit (details of which were
notified on 7(th) January 2020) reported: 31,083,000 tonnes (t) at
1.02 grams/tonne (g/t) for 1,015,000 ounces of gold including
21,930,000t at 1.06g/t for 747,000 ounces gold in the Indicated
category.
BAM Gold Resource and PEA:
A Technical Report and PEA of the BAM Gold Project was released
on 20(th) February 2019. The PEA is in compliance with the
requirements of the Canadian National Instruments 43-101 Standards
of Disclosure for Mineral Projects ("NI 43-101").
The Junior Lake Property:
The Junior Lake Property, 100% owned by Landore Resources,
together with the contiguous Lamaune Iron property (90.2% owned)
(jointly the "Junior Lake Property"), consisting of 30,507
hectares, is located in the province of Ontario, Canada,
approximately 235 kilometres north-northeast of Thunder Bay and is
host to: The BAM Gold Deposit; the B4-7
Nickel-Copper-Cobalt-Platinum-Palladium-Gold Deposit; the VW
Nickel-Copper-Cobalt Deposit; Lamaune Gold Prospect and numerous
other precious and base metal occurrences.
Covid-19
The Company is following Government Covid-19 guidelines in its
operations in Canada.
Michele Tuomi, (P.Geo., BSc. Geology), Director/VP Exploration
of Landore Resources Canada Inc. and a Qualified Person as defined
in the Canadian National Instrument 43-101 and the AIM Rules for
Companies, has reviewed and verified all scientific or technical
mining disclosure contained in this announcement.
- ENDS -
About Landore Resources
Landore Resources is an exploration company that seeks to grow
shareholder value through the acquisition, exploration and
development of precious and base metal projects in eastern Canada.
The Company is primarily focused on the development of the Junior
Lake Project. Landore Resources has mineral rights to 5 properties
in eastern Canada. The Company is headquartered in Guernsey, with
an exploration office located in Thunder Bay, Ontario, Canada.
For more information, please contact:
Landore Resources Limited
Bill Humphries, Chief Executive Tel: 07734 681262
Officer
Glenn Featherby, Finance Director Tel: 07730 420318
Cenkos Securities (Nominated Advisor
and Broker)
Derrick Lee / Peter Lynch Tel: 0131 220 9100
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