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| Share Name | Share Symbol | Market | Type |
|---|---|---|---|
| Alpha Minerals | TSXV:AMW | TSX Venture | Common Stock |
| Price Change | % Change | Share Price | Bid Price | Offer Price | High Price | Low Price | Open Price | Shares Traded | Last Trade | |
|---|---|---|---|---|---|---|---|---|---|---|
| 0.00 | 0.00% | 0 | - |
Hot Features
Premium
Alpha Minerals Inc. (TSX VENTURE:AMW)(FRANKFURT:E2GA), (the "Company" or
"Alpha"), and its 50% Joint Venture partner Fission Uranium Corp are pleased to
announce results for the final ten lake holes of the summer program at their
Patterson Lake South (PLS) property in Canada's Athabasca Basin. All holes
intersected significant mineralization. Of particular note are drill holes
PLS13-109 (99.5m total composite mineralization, including 6.87m total composite
"off-scale") and PLS13-097 (90.0m total composite mineralization, including
6.35m total composite "off-scale") in the R780E zone.
Drilling Highlights include:
-- PLS13-109 (line 750E)
-- 99.5m total composite mineralization (within 105.5m - 334.5m)
including:
-- 6.87m total composite off-scale (greater than 9999 cps)
radioactivity
-- PLS13-097 (line 795E)
-- 90.0m total composite mineralization (within 74.5m - 254.5m)
including:
-- 6.48m total composite off-scale (greater than 9999 cps)
radioactivity
-- PLS13-108 (line 810E)
-- 103.5m total composite mineralization (within 80.5m - 234.5m),
including:
-- 3.25m total composite off-scale (greater than 9999 cps)
radioactivity
-- PLS13-090 and -103 (line 1155E)
-- PLS mineralized strike length extended to 1.23km
It is very significant that none of the mineralized "zones" have been limited by
drilling during the current or earlier programmes, and there is a possibility
that mineralization has continuity between some or all of the "zones". The size
of the mineralizing system discovered at PLS thus far correlates well with
Alpha's regional context of the property.
The following drill holes are reported in this news release: PLS13-104 (R390E
zone); PLS13-106 (R585E zone); PLS13-097, PLS13-101, PLS13-105, PLS13-107,
PLS13-108, and PLS13-109 (R780E zone); and PLS13-090, and PLS13-103 (line 1155E)
all intersected significant mineralization.
R390E Zone
The R390E zone refers to the zone of mineralization currently defined over 255m
of strike length between line 225E (PLS13-093) and line 480E (PLS13-088). One
additional hole was drilled on the R390E zone since the last update (see news
release September 27, 2013). Drill hole PLS13-104 was a vertical collared hole
on line 465E, located 15m grid west of PLS13-088. A 3.6m wide interval of
Devonian sandstone (50.0m - 53.6m) overlies basement pelitic gneiss,
transitioning to semi-pelitic gneiss from 210.4m to the end of hole depth of
309.2m. Several intervals of undifferentiated mylonites are present within the
pelitic sequence, in intervals ranging from 2.1m to 20.6m wide. Radioactive
mineralization occurs in several discrete intervals between 53.5m and 212.0m,
ranging from 0.5m to 17.0m wide for a total composite of 70.0m of
mineralization, including a total composite of 3.02m of off-scale radioactivity
in intervals of 0.15m to 1.48m.
R390E Drill Hole Table
----------------------------------------------------------------------------
(i) Hand-held Scintillometer Results Dev- Base-
On Mineralized Drillcore (greater onian ment Total
than 300 cps / greater than 0.5M Sand- Uncon- Drill-
Collar minimum) stone formity hole
---------------------------------------------------------------------
CPS
Hole Grid From To Width Peak From - Depth Depth
ID Line Az Dip (m) (m) (m) Range To (m) (m) (m)
----------------------------------------------------------------------------
PLS13- less than 300 - 50.0 -
104 465E 26 -88 53.5 56.0 2.5 1700 53.6 53.6 309.2
less than 300 -
58.0 73.0 15.0 3900
86.0 88.5 2.5 430 - 1300
95.5 96.0 0.5 400
less than 300 -
98.0 112.5 14.5 less than 9999
125.5 126.5 1.0 540 - 680
less than 300 -
131.0 141.5 10.5 greater than 9999
less than 300 -
146.5 163.5 17.0 6800
167.5 168.0 0.5 320
202.0 203.5 1.5 550 - 1500
211.5 212.0 0.5 420
----------------------------------------------------------------------------
(i)Scintillometer Instrument: GR-110G
R585E Zone
The R585E zone refers to the zone of mineralization currently defined by only
two drill holes on line 585E. One additional hole was drilled on the R585E zone
since the last update (see news release September 23, 2013). PLS13-106 was a
vertical collared hole on line 585E, located 10m grid north of PLS13-098.
Bedrock was encountered at 53.7m, compared to a depth of 62.4m in PLS13-098.
This represents a significant 8.7m vertical off-set to the top of the basement
between holes. A pelitic gneiss was intersected from 53.7m to 176.2m and a
semipelitic gneiss from 176.2m to 269.6m. A wide sequence of diabase was
intersected from 269.6m to 332.0m. Radioactive mineralization is broad and
relatively moderate to locally strong, occurring in several intervals from 0.5m
to 19.5m for a total composite of 86.5m over a 160.0m section (82.5m to 242.5m).
The difference in intensity of mineralization between drill holes PLS13-098 and
-106 may be related to the significant fault interpreted between the 2 holes.
Further drilling is required to determine the nature and control of
mineralization at the R585E zone.
R585E Drill Hole Table
----------------------------------------------------------------------------
(i) Hand-held Scintillometer Results Dev- Base-
On Mineralized Drillcore (greater onian ment Total
than 300 cps / greater than 0.5M Sand- Uncon- Drill-
Collar minimum) stone formity hole
---------------------------------------------------------------------
CPS
Hole Grid From To Width Peak From - Depth Depth
ID Line Az Dip (m) (m) (m) Range To (m) (m) (m)
----------------------------------------------------------------------------
No
PLS13- Sand-
106 585E170 -85 82.5 83.0 0.5 370 stone 53.7 332.0
less than 300 -
101.0 105.0 4.0 600
114.0 114.5 0.5 720
less than 300 -
118.0 125.5 7.5 1100
128.5 129.0 0.5 870
131.0 131.5 0.5 810
136.0 137.5 1.5 420 - 1700
less than 300 -
151.5 155.0 3.5 1200
less than 300 -
158.0 164.0 6.0 4400
less than 300 -
166.5 184.0 17.5 2500
186.5 188.0 1.5 470 - 2100
less than 300 -
191.5 199.5 8.0 1700
less than 300 -
201.5 214.5 13.0 4500
less than 300 -
218.0 220.5 2.5 950
less than 300 -
223.0 242.5 19.5 1700
----------------------------------------------------------------------------
(i)Scintillometer Instrument: GR-110G
R780E Zone
The R780E zone refers to the zone of mineralization currently defined over 60m
of strike length between line 750E (hole PLS13-109) and line 810E (PLS13-108).
Six additional holes were drilled on the R780E zone since the last update (see
news release September 12, 2013), for a total of 12 holes presently defining the
R780E zone.
Line 750E:
-- Drillhole PLS13-109 was collared as a vertical hole and drilled to a
depth of 401.0m. The collar is located approximately 30m grid west of
PLS13-060. Basement was intersected at 58.3m. A quartzitic gneiss is
present from 58.3m to 103.4m. From 103.4m to 337.6m the lithology is
dominantly pelitic gneiss with multiple intervals of undifferentiated
mylonites (from 1.8m to 9.9m wide) and cataclasites. From 337.6m to the
end of hole depth of 401.0m a semi-pelitic gneiss dominates. Anomalous
radioactivity occurs from 105.5m coincident with the transition from
quartzitic to pelitic gneiss. A total composite of 99.5m of
mineralization within a 229.0m section (105.5m to 334.5m) occurs in
several variably radioactive mineralized intervals ranging in width from
0.5m to 34.0m. A total composite of 6.87m of off-scale radioactivity
occurs in several discrete intervals ranging from 0.12m to 3.28m wide.
Line 765E: Two vertically collared holes were drilled on line 765E
-- Drillhole PLS13-105 was collared as a vertical hole and drilled to a
depth of 419.0m. The collar is located approximately 15m grid west of
PLS13-080. Basement was intersected at 55.0m. A quartzitic gneiss is
present from 55.0m to 109.2m. From 109.2m to 296.6m lithology is
dominantly pelitic gneiss with multiple intervals of undifferentiated
mylonites (from 1.3m to 13.9m wide). From 296.6m to the end of hole
depth of 419.0m a semipelitic gneiss dominates. Anomalous radioactivity
occurs from 106.5m coincident with the transition from quartzitic to
pelitic gneiss. A total composite of 46.5m of mineralization within a
224.0m section (106.5m to 330.5m) occurs in several variably radioactive
mineralized intervals ranging in width from 0.5m to 18.5m. A total
composite of 1.64m of off-scale radioactivity occurs in several discrete
intervals ranging from 0.15m to 1.06m wide.
-- Drillhole PLS13-107 was collared as a vertical hole and drilled to a
depth of 402.0m. The collar is located approximately 15m grid west of
PLS13-060. Basement was intersected at 56.0m. A quartzitic gneiss is
present from 56.0m to 183.8m, which encompasses a pelitic gneiss unit
from 67.8m to 128.6m. From 183.8m to 283.0m lithology is dominantly
pelitic gneiss with a 41.5m wide interval of undifferentiated mylonites
(233.7m to 275.2m). A semipelitic gneiss dominates from 283.0m to the
end of hole depth of 402.0m. Anomalous radioactivity starts at 138.5m
within the quartzitic gneiss. A total composite of 63.5m of
mineralization within a 193.5m section (138.5m to 332.0m) occurs in
several variably radioactive mineralized intervals ranging in width from
0.5m to 24.5m. A total composite of 1.04m of off-scale radioactivity
occurs in several discrete intervals ranging from 0.13m to 0.5m wide.
Line 795E:
-- Drillhole PLS13-097 was collared as a vertical hole and drilled to a
depth of 356.0m. The collar is located approximately 15m grid east of
PLS13-060. Basement was intersected at 55.8m. A quartzitic gneiss with
minor pegmatite and mylonite intervals is present from 55.8m to 183.9m
that encompasses a pelitic gneiss unit from 76.6m to 85.4m. From 183.9m
to the end of hole depth of 356.0m lithology is dominantly pelitic
gneiss with occasional intervals of undifferentiated mylonites (1.1m to
2.4m wide). Anomalous radioactivity begins at 74.5m in proximity to the
contact between the quartzitic gneiss and pelitic gneiss. A total
composite of 82.0m of mineralization within a 180.0m section (74.5m to
254.5m) occurs in several variably radioactive mineralized intervals
ranging in width from 0.5m to 49.5m. A total composite of 6.48m of off-
scale radioactivity occurs in several discrete intervals ranging from
0.1m to 3.63m wide.
Line 810E: Two vertically collared holes were drilled on line 810E
-- Drillhole PLS13-101 was collared as a vertical hole and drilled to a
depth of 350.0m. The collar is located approximately 15m grid east of
PLS13-097. Basement was intersected at 67.4m, which is 11.8m deeper than
the depth of basement intersected in PLS13-097, which may represent an
important structural feature. From 67.4m to 192.6m lithology is pelitic
gneiss with occasional pegmatite injections up to 2.2m thick.
Semipelitic gneiss was intersected from 192.6m to 275.6m, which is
underlain by pelitic gneiss to 334.7m. From 334.7m to the end of hole
depth of 350.0m a semipelitic gneiss dominates. Anomalous radioactivity
starts at 69.5m within a pelitic gneiss, which is an unusually shallow
depth to mineralization for the R780E zone. A total composite of 96.0m
of mineralization within a 230.0m section (69.5m to 299.5m) occurs in
several variably radioactive mineralized intervals ranging in width from
0.5m to 35.0m. A total composite of 0.51m of off-scale radioactivity
occurs in several discrete narrow intervals ranging from 0.10m to 0.17m
wide.
-- Drillhole PLS13-108 was collared as a vertical hole and drilled to a
depth of 392.0m. The collar is located approximately 10m grid north of
PLS13-101. Basement was intersected at 58.3m, which is 9.1m shallower
than the depth of basement intersected in PLS13-101. An alternating
sequence of quartzitic and pelitic gneiss was encountered from 58.3m to
206.1m, which is underlain by semipelitic gneiss to 230.3m. From 230.3m
to 332.4m lithology is dominantly pelitic gneiss with occasional
intervals of undifferentiated mylonites (4.1m to 11.9m wide). From
332.4m to the end of hole depth of 392.0m a semipelitic gneiss
dominates. Anomalous radioactivity begins at 80.5m within the pelitic
gneiss. A total composite of 105.5m of mineralization within a 195.5m
section (80.5m to 276.0m) occurs in several variably radioactive
mineralized intervals ranging in width from 0.5m to 21.5m. A total
composite of 3.25m of off-scale radioactivity occurs in several discrete
intervals ranging from 0.14m to 0.75m wide.
R780E Drill Hole Table
----------------------------------------------------------------------------
(i) Hand-held Scintillometer Results Dev- Base-
On Mineralized Drillcore (greater onian ment Total
than 300 cps / greater than 0.5M Sand- Uncon- Drill-
Collar minimum) stone formity hole
----------------------------------------------------------------------
CPS
Hole Grid From To Width Peak From - Depth Depth
ID Line Az Dip (m) (m) (m) Range To (m) (m) (m)
----------------------------------------------------------------------------
No
PLS13- Sand-
097 795E 351 -86 74.5 75.5 1.0 540 - 770 stone 55.8 356.0
less than 300 -
77.5 81.5 4.0 1500
83.5 84.0 0.5 460
90.5 91.5 1.0 810 - 900
less than 300 -
117.5 167.0 49.5 greater than 9999
less than 300 -
169.0 176.0 7.0 8100
179.5 180.5 1.0 390 - 9700
182.5 188.5 6.0 300 - 850
204.5 206.0 1.5 300 - 850
220.0 222.0 2.0 320 - 8400
340 - greater than
228.5 234.5 6.0 9999
less than 300 -
241.0 243.0 2.0 560
254.0 254.5 0.5 820
----------------------------------------------------------------------------
No
PLS13- Sand-
101 810E 23 -87 69.5 70.5 1.0 460 - 520 stone 67.4 350.0
less than 300 -
78.0 84.0 6.0 3100
94.5 96.0 1.5 350 - 710
less than 300 -
103.0 138.0 35.0 9200
less than 300 -
141.5 159.5 18.0 5700
less than 300 -
163.0 174.5 11.5 9900
less than 300 -
179.0 196.0 17.0 greater than 9999
550 - greater than
226.0 227.0 1.0 9999
230.0 230.5 0.5 1100
251.0 251.5 0.5 470
290.5 292.0 1.5 640 - 1300
less than 300 -
297.0 299.5 2.5 550
----------------------------------------------------------------------------
No
PLS13- less than 300 - Sand-
105 765E 70 -87 106.5 110.0 3.5 3200 stone 55.0 419.0
less than 300 -
113.0 131.5 18.5 greater than 9999
less than 300 -
145.5 151.5 6.0 2000
less than 300 -
189.0 192.5 3.5 greater than 9999
850 - greater than
195.0 197.5 2.5 9999
203.5 205.0 1.5 460 - 2000
210.5 211.5 1.0 1300 - 5000
245.0 246.0 1.0 960 - 1200
249.0 249.5 0.5 1100
252.5 253.5 1.0 380 - 860
263.5 264.5 1.0 730 - 3000
282.0 283.0 1.0 440 - 640
320.5 321.0 0.5 350
less than 300 -
325.5 330.5 5.0 580
----------------------------------------------------------------------------
No
PLS13- less than 300 - Sand-
107 765E 49 -89 138.5 163.0 24.5 8400 stone 56.0 402.0
less than 300 -
166.0 167.5 1.5 510
less than 300 -
171.5 175.0 3.5 greater than 9999
178.5 179.5 1.0 930 - 9200
less than 300 -
192.5 199.0 6.5 7200
203.5 204.0 0.5 1000
207.0 207.5 0.5 1200
221.0 221.5 0.5 410
less than 300 -
251.5 265.0 13.5 6400
less than 300 -
267.5 274.5 7.0 8000
289.0 290.0 1.0 1300 - 1800
less than 300 -
306.5 309.5 3 980
331.5 332.0 0.5 330
----------------------------------------------------------------------------
No
PLS13- Sand-
108 810E 271 -83 80.5 82.0 1.5 360 - 570 stone 58.3 392.0
88.0 88.5 0.5 380
less than 300 -
91.0 112.5 21.5 1200
less than 300 -
115.5 130.0 14.5 1600
less than 300 -
132.5 149.0 16.5 2400
less than 300 -
152.0 172.0 20.0 greater than 9999
less than 300 -
174.5 195.5 21.0 greater than 9999
201.0 202.0 1.0 860 - 1700
217.0 217.5 0.5 460
less than 300 -
228.0 234.5 6.5 greater than 9999
256.5 257.5 0.5 370
268.0 269.0 1.0 1600 - 6300
275.5 276.0 0.5 1600
----------------------------------------------------------------------------
No
PLS13- less than 300 - Sand-
109 750E 309 -89 105.5 116.0 10.5 greater than 9999 stone 56.0 401.0
less than 300 -
136.0 170.0 34.0 greater than 9999
173.5 174.0 0.5 760
less than 300 -
177.5 182.0 4.5 4000
186.0 186.5 0.5 350
less than 300 -
191.5 193.5 2.0 5900
less than 300 -
197.0 212.0 15.0 greater than 9999
251.0 251.5 0.5 530
266.5 267.5 1.0 400 - 490
less than 300 -
274.5 292.0 17.5 4000
294.5 296.5 2.0 370 - 440
less than 300 -
300.0 309.5 9.5 5200
332.5 334.5 2.0 320 - 720
----------------------------------------------------------------------------
(i)Scintillometer Instrument: GR-110G
Line 1155E
Line 1155E is located approximately 195m grid east of the R945E zone. Drilling
of two holes (PLS13-090 and 103) was a follow-up test of a subtle radon in water
anomaly identified during the Phase 2 EIC radon in water and sediment survey
completed during April 2013, by RadonEx Exploration Management of St. Lazare,
Quebec. This anomaly lies along an ENE trend, in proximity to the PL-3B EM
conductor and on trend with the five PLS mineralized zones (R00E, R390E, R585E,
R780E, and R945E) that remain open in all directions. Drilling on line 1155E
extends the mineralization at PLS to a 1.23km strike length. Although neither
drill hole encountered strong mineralization, both encountered significant
widths of anomalous radioactivity in a geologic setting similar to the
high-grade zones to the west. The very large mineralizing system at PLS remains
open to the east, which reinforces that further drilling is required from the
ice surface available during the 2014 drill to evaluate line 1155E.
Line 1155E: Two vertically collared holes were drilled on line 1155E
-- Drillhole PLS13-090 was collared as a vertical hole and drilled to a
depth of 323.0m. Basement was intersected at 62.0m. A quartzitic gneiss
is present from 62.0m to 96.7m. From 96.7m to 314.3m the lithology is
comprised of alternating sequences of pelitic, quartzitic, and
semipelitic units. A diabase unit was encountered from 314.3m to the end
of hole depth of 323.0m. A weak radioactive mineralized interval is
present over a continuous 12.5m interval from 189.5m to 202.0m within a
semipelitic gneiss, with a range of less than 300 to 1600 cps.
-- Drillhole PLS13-103 was collared as a vertical hole and drilled to a
depth of 427.0m. The collar was located 10m south of PLS13-090.
Quartzitic gneiss was encountered from 62.4m to 111.7m, which was
underlain by alternating pelitic gneiss, mylonite, and semipelitic
gneiss units to 304.6m. From 304.6m to the end of hole depth of 427.0m a
semipelitic gneiss dominates. A total composite of 15.5m of
mineralization within a 34.5m section (175.0m to 209.5m) occurs in
several weakly radioactive mineralized intervals ranging in width from
1.0m to 6.5m. A deeper and narrow 1.0m weakly radioactive interval was
intersected at 365.5m.
Line 1155E Drill Hole Table
----------------------------------------------------------------------------
(i) Hand-held Scintillometer Results Dev- Base-
On Mineralized Drillcore (greater onian ment Total
than 300 cps / greater than 0.5M Sand- Uncon- Drill-
Hole Location minimum) stone formity hole
-------------------------------------------------
CPS
Hole Grid From To Width Peak From - Depth Depth
ID Line Az Dip (m) (m) (m) Range To (m) (m) (m)
----------------------------------------------------------------------------
No
PLS13- less than 300 - Sand-
090 1155E 180 -89 189.5 202.0 12.5 1600 stone 62.0 323.0
----------------------------------------------------------------------------
No
PLS13- Sand-
103 1155E 347 -88 175.0 177.5 2.5 360 - 550 stone 62.4 427.0
less than 300 -
188.0 193.5 5.5 770
less than 300 -
197.5 204.0 6.5 560
208.5 209.5 1.0 420 - 570
365.5 366.5 1.0 320
----------------------------------------------------------------------------
(i)Scintillometer Instrument: GR-110G
A $9.2M, 14,700m drill program and ground geophysics surveys continues at PLS.
Barge-based lake drilling is now complete. The program's remaining holes will be
land-based.
Natural gamma radiation in drill core that is reported in this news release was
measured in counts per second (cps) using a hand held Exploranium GR-110G total
count gamma-ray scintillometer. The reader is cautioned that scintillometer
readings, like the down hole gamma probe readings, are not directly or uniformly
related to uranium grades of the rock sample measured, and should be used only
as a preliminary indication of the presence of radioactive materials. The degree
of radioactivity within the mineralized intervals is highly variable and
associated with visible pitchblende mineralization. All intersections are
down-hole, core interval measurements and true thickness is yet to be
determined.
Radiometric surveys are planned for all holes using a Mount Sopris 2GHF-1000
Triple Gamma probe, which allows for more accurate measurements in high grade
mineralized zones.
Split core samples from the mineralized section of core will be taken
continuously through the mineralized intervals and submitted to SRC
Geoanalytical Laboratories (an SCC ISO/IEC 17025: 2005 Accredited Facility) of
Saskatoon for analysis, which includes U and fire assay for gold. All samples
sent for analysis will include a 63 element ICP-OES, uranium by ICP-MS and
boron. Assay results will be released when received.
For additional comments about the Summer 2013 Program, please watch a corporate
video at the Alpha Minerals website:
http://www.alphaminerals.ca/corporate-videos/
Patterson Lake South Property
The 31,000 hectare (76,000 acres) PLS project is a 50%/50% Joint Venture held by
Alpha Minerals Inc (AMW) and Fission Uranium (FCU). The Joint Venture property
is 100% owned with no underlying royalties or vendor payments. For the present
work, the exploration is still being operated as a Joint Venture under the
direction of the Joint Venture Management Committee with Fission Uranium acting
as the operator.
The property is accessible by road with primary access from all-weather Highway
955, which runs 74km north to the former Cluff Lake mine, (greater than 60M lbs
of U3O8 produced from multiple open pit and underground mines), and passes
through the claims covering the UEX-Areva Shea Creek discoveries located 58km to
the north, currently under active exploration and development.
The technical information in this news release has been prepared in accordance
with the Canadian regulatory requirements set out in National Instrument 43- 101
and reviewed on behalf of Alpha Minerals Inc, by Garrett Ainsworth, P.Geo., Vice
President Exploration, a qualified person.
On behalf of the Board of Directors of Alpha Minerals Inc.
"Ben Ainsworth"
--------------------------------------------------
PEng BC/SK, President, CEO and Director
Please refer to the Alpha Minerals Inc. website (www.alphaminerals.ca) for the
video and further updated information.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that
term is defined in the policies of the TSX Venture Exchange) accepts
responsibility for the adequacy or accuracy of this release.
This press release contains "forward-looking information" that is based on
Alpha's current expectations, estimates, forecasts and projections. This
forward-looking information includes, among other things, statements with
respect to Alpha's development plans. The words "will", "anticipated", "plans"
or other similar words and phrases are intended to identify forward-looking
information.
Forward-looking information is subject to known and unknown risks, uncertainties
and other factors that may cause Alpha's actual results, level of activity,
performance or achievements to be materially different from those expressed or
implied by such forward-looking information. Such factors include, but are not
limited to: uncertainties related exploration and development; the ability to
raise sufficient capital to fund exploration and development; changes in
economic conditions or financial markets; increases in input costs; litigation,
legislative, environmental and other judicial, regulatory, political and
competitive developments; technological or operational difficulties or inability
to obtain permits encountered in connection with exploration activities; and
labour relations matters. This list is not exhaustive of the factors that may
affect our forward-looking information. These and other factors should be
considered carefully and readers should not place undue reliance on such
forward-looking information. Alpha disclaims any intention or obligation to
update or revise forward-looking information, whether as a result of new
information, future events or otherwise.
FOR FURTHER INFORMATION PLEASE CONTACT:
For corporate communications please contact:
Robert (Bob) Meister
Alpha Minerals Inc.
(604) 629-0293
(604) 684-9365 (FAX)
Toll Free: 1-866-629-0293
Email: info@alphaminerals.ca
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