Fission, the Operator, Reports Remaining Assays on R00E, R390E and R780E Zones at PLS
KELOWNA, BRITISH COLUMBIA--http://www.juniorminingnetwork.com/junior-miner-news/news-releases/631-tsx-venture/fcu/13843-fission-the-operator-reports-remaining-assays-on-r00e-r390e-and-r780e-zones-at-pls.html
Assay Highlights include:
Zone R00E
(Marketwired - June 5, 2013) - http://www.juniorminingnetwork.com/junior-miner-news/news-releases/631-tsx-venture/fcu/13843-fission-the-operator-reports-remaining-assays-on-r00e-r390e-and-r780e-zones-at-pls.html
FISSION URANIUM CORP.
(the "Company" or "Fission") (TSX VENTURE:FCU)(FRANKFURT:2FU), the
operator, and its 50% Joint Venture partner Alpha Minerals Inc., are
pleased to report assay results from the remaining seventeen drill holes
from the winter program at its Patterson Lake South (PLS) Property. The
new results show continuous areas of broad uranium mineralization at
shallow depth in all three PLS zones. Of particular note is hole
PLS13-066 which returned an interval of 63.5m at 1.15% U3O8, including
2m at 9.51%.
These assays are the final results from the
winter 2013 exploration program which saw a drill strike rate of 82% in
the discovery of two new mineralized uranium zones (R390E, R780E), and
significant growth of the R00E zone.
Ross McElroy, President, COO, and Chief Geologist for Fission, commented,
"The
Winter program at PLS represents one of the most impressive uranium
exploration programs I've ever seen or been a part of. With some huge
intersections and high grades these results are a great end to the
Winter program and a promising prelude to the Summer exploration
program."
Assay Highlights include:
Zone R00E
- Hole PLS13-067 (line 045E) intersected:
- 6.0m (61.5m-67.5m) of 4.80% U3O8 including:
- Hole PLS13-061 (line 360E) intersected:
- 23.5m (110.0m-133.5m) of 1.39% U3O8, including:
- 6.0m (126.0m-132.0m) of 4.34% U3O8
- Hole PLS13-066 (Line 420E) intersected:
- 63.5m (82.5m-145.5m) of 1.15% U3O8, including:
- 2.0m (133.0m-135.0m) of 9.51% U3O8
- Hole PLS13-060 (Line 780E) intersected:
- 7.0m (144.0m-1151m) of 1.22% U3O8, including:
Assays
reported for four vertical collared holes in this news release
represent close spaced delineation drilling on lines 045E and 060E of
the R00E zone. Interpretation thus far shows mineralization to be
primarily focused in a footwall steeply south dipping package of E-NE
trending pelitic gneiss, sandwiched between a semi-pelitic rock to the
north and a quartz-feldspar gneiss to the south.
Delineation drilling
has also shown mineralization to cross lithological boundaries into the
footwall and hanging wall adjacent the pelitic gneiss. This lithologic
package appears to be parallel along strike to the ~073° oriented
basement EM conductor identified from airborne and ground geophysics
surveys.
As was the case with previous drill results
from the R00E zone, the main mineralized horizon appears to be
structurally controlled and generally flat lying within the pelitic (+/-
graphite) unit, with the upper level of the mineralized zone occurring
at or near the top of the Archean basement rocks, either within or
immediately below a thin veneer or Devonian sandstone (see
cross-sections lines 045E and 060E.
Mineralization has been traced
northward extending into the semi-pelitic package on sections L025W,
040W and 060W) and remains untested on the other sections.
| Table 1: R00E Zone - Composited Mineralized Intervals (Down-hole measurements) | ||||||
| Zone | Hole ID | Grid Line | From (m) | To (m) | Interval (m) | U3O8 (wt%) |
| R00E | PLS13-065 | 060E | 51.00 | 53.50 | 2.50 | 0.12 |
| | PLS13-067 | 045E | 50.50 | 52.00 | 1.50 | 0.09 |
| | | | 61.50 | 67.50 | 6.00 | 4.63 |
| | | | 63.50 | 67.50 | 4.00 | 6.86 |
| | | | 110.00 | 110.50 | 0.50 | 0.05 |
| | PLS13-069 | 045E | 52.00 | 53.50 | 1.50 | 0.36 |
| | | | 100.50 | 101.50 | 1.00 | 0.06 |
| | PLS13-071 | 045E | No significant mineralization | |||
| Composite Parameters | ||||||
| | 1. | Minimum Thickness: 0.50m |
| | 2. | Grade Cut-Off: 0.05 U3O8 (wt%) |
| | 3. | Maximum Internal Dilution: 2.00m |
R390E Zone
Assays
reported for eight vertical collared holes in this news release
(PLS13-044, 046, 061, 062, 064, 066, 068 and 070) represent close spaced
delineation drilling on lines 360E, 375E, 390 E, 405E and 420E of the
R390E Zone. As is the case with the R00E zone, R390E mineralization is
spatially located proximal to the north of the PL-3B basement EM
conductor and situated within a well-defined resistivity low corridor.
Drillhole interpretation thus far defines the area of highest grade
mineralization to be associated with a steeply south dipping pelitic
(+/- graphitic) lithology sandwiched between a semipelitic gneiss to the
north and a quartz-feldspar gneiss to the south, where the
mineralization is focused primarily near the contact between the pelitic
gneiss and quartz-feldspar gneiss.
Holes drilled on sections 390E have
encountered weak mineralization in the footwall semipelitic rocks to the
north (PLS13-068 and 070) and the hanging wall quartzitic gneiss to the
south (PLS13-46). This lithologic package appears to be parallel along
strike with that of the R00E Zone.
Most significant are
the results of holes PLS13-061 (located 15m grid west of hole PLS13-053)
and PLS13-066 (located 15m grid east of hole PLS13-066). Hole 061 (line
360E) shows the uranium to be concentrated within two zones: a) an
upper 21.0m wide interval (77.0m - 88.0m) that averages 0.26% U3O8 and a
higher grade lower 23.5m wide interval (110.0m - 133.5m) that averages
1.39% U3O8. Hole PLS13-066 (line 420E) shows the uranium to be
concentrated in 1 continuous 63.5m interval (82.0m - 145.5m) that
averages 1.15% U3O8 and includes several high-grade sub-intervals from
2.0m to 6.0m wide.
| Table 2: R00E Zone - Composited Mineralized Intervals (Down-hole measurements) | ||||||
| Zone | Hole ID | Grid Line | From (m) | To (m) | Interval (m) | U3O8 (wt%) |
| R390E | PLS13-044 | 390E | 56.00 | 73.00 | 17.00 | 0.24 |
| | | | 60.00 | 61.00 | 1.00 | 1.24 |
| | | | 77.00 | 83.00 | 6.00 | 0.32 |
| | | | 86.00 | 89.50 | 3.50 | 0.38 |
| | | | 96.50 | 103.50 | 7.00 | 0.46 |
| | | | 101.00 | 102.50 | 1.50 | 1.36 |
| | PLS13-046 | 390E | 96.50 | 98.00 | 1.50 | 0.13 |
| | | | 127.50 | 129.00 | 1.50 | 0.04 |
| | | | 206.50 | 207.50 | 1.00 | 0.15 |
| | | | 239.00 | 240.00 | 1.00 | 0.14 |
| | | | 243.50 | 244.00 | 0.50 | 0.16 |
| | PLS13-061 | 360E | 77.00 | 98.00 | 21.00 | 0.26 |
| | | | 92.50 | 97.50 | 5.00 | 0.75 |
| | | | 102.50 | 103.50 | 1.00 | 0.25 |
| | | | 110.00 | 133.50 | 23.50 | 1.39 |
| | | | 126.00 | 132.00 | 6.00 | 4.34 |
| | | | 137.50 | 140.00 | 2.50 | 1.17 |
| | PLS13-062 | 375E | 51.00 | 55.00 | 4.00 | 0.36 |
| | | | 86.00 | 98.50 | 12.50 | 0.19 |
| | PLS13-064 | 405E | 83.50 | 84.50 | 1.00 | 0.29 |
| | | | 90.50 | 91.50 | 1.00 | 0.11 |
| | | | 95.00 | 96.00 | 1.00 | 0.06 |
| | | | 110.50 | 121.00 | 10.50 | 0.08 |
| | | | 125.50 | 136.00 | 10.50 | 0.43 |
| | | | 130.00 | 132.00 | 2.00 | 1.37 |
| | PLS13-066 | 420E | 82.00 | 145.50 | 63.50 | 1.15 |
| | | | 88.00 | 90.50 | 2.50 | 4.50 |
| | | | 101.00 | 107.50 | 6.50 | 2.60 |
| | | | 122.00 | 124.00 | 2.00 | 2.14 |
| | | | 133.00 | 135.00 | 2.00 | 9.51 |
| | PLS13-068 | 390E | 96.00 | 111.00 | 15.00 | 0.26 |
| | | | 116.00 | 117.00 | 1.00 | 0.10 |
| | PLS13-070 | 390E | 85.50 | 89.00 | 3.50 | 0.13 |
| Composite Parameters | ||||||
| 1. | Minimum Thickness: 0.50m | |
| 2. | Grade Cut-Off: 0.05 U3O8 (wt%) | |
| 3. | Maximum Internal Dilution: 2.00m |
R780E Zone
Assays
reported for three vertical collared holes in this news release
(PLS13-048, 055 and 060) represent close spaced delineation drilling on
line 780E. The R780E zone discovery was the result of follow-up by
drilling of a radon in water anomaly identified during the January -
February 2013 survey conducted by RadonEx Exploration Management. The
radon anomaly is on trend to the E-NE from the R00E and R390E zones, and
is situated close to the east end of the PL-3B EM conductor and
associated resistivity low corridor that is inferred to be terminated by
a cross cutting structure.
Similar to the R00E and
R390E Zones, interpretation of mineralization in R780E, shows that
mineralization is primarily focused within the graphitic pelitic rock,
but in all three holes, mineralization continues across the footwall
semipelite contact. The most northerly hole, PLS13-048 intersected
mineralization entirely within the footwall semipelitic rocks.
The
best developed mineralized zones were returned from hole PLS13-060,
which had a total of 11 discontinuous intervals from 0.5m - 15.5m wide
within 124.5m (133.5m - 258.0m). The strongest interval of
mineralization was from a 7.0m interval (144.0m - 151.0m) that averaged
1.22% U3O8, including a higher grade 2.5m wide core (146.5m - 149.0m) at
3.0% U3O8.
| Table 3: R00E Zone - Composited Mineralized Intervals (Down-hole measurements) | ||||||
| Zone | Hole ID | Grid Line | From (m) | To (m) | Interval (m) | U3O8 (wt%) |
| R780E | PLS13-048 | 780E | 155.00 | 164.50 | 9.50 | 0.08 |
| | | | 167.00 | 173.50 | 6.50 | 0.18 |
| | | | 176.00 | 177.00 | 1.00 | 0.07 |
| | PLS13-055 | 780E | 109.50 | 114.00 | 4.50 | 0.40 |
| | | | 117.00 | 118.00 | 1.00 | 0.15 |
| | | | 141.50 | 145.50 | 4.00 | 0.40 |
| | | | 166.00 | 176.00 | 10.00 | 0.57 |
| | | | 173.50 | 176.00 | 2.50 | 1.87 |
| | | | 192.00 | 192.50 | 0.50 | 0.39 |
| | PLS13-060 | 780E | 133.50 | 141.00 | 7.50 | 0.18 |
| | | | 144.00 | 151.00 | 7.00 | 1.22 |
| | | | 146.50 | 149.00 | 2.50 | 3.00 |
| | | | 154.00 | 156.50 | 2.50 | 0.13 |
| | | | 159.50 | 175.00 | 15.50 | 0.20 |
| | | | 183.00 | 189.50 | 6.50 | 0.39 |
| | | | 193.50 | 196.50 | 3.00 | 0.14 |
| | | | 203.50 | 209.00 | 5.50 | 0.36 |
| | | | 212.00 | 216.50 | 4.50 | 0.36 |
| | | | 221.00 | 226.50 | 5.50 | 0.11 |
| | | | 247.50 | 248.00 | 0.50 | 0.20 |
| | | | 257.50 | 258.00 | 0.50 | 0.38 |
| Composite Parameters | ||||||
| 1. | Minimum Thickness: 0.50m | ||
| 2. | Grade Cut-Off: 0.05 U3O8 (wt%) | ||
| 3. | Maximum Internal Dilution: 2.00m |
Regional Tests
Two drill holes tested regional targets further along trend and on a parallel conductor to the north.
Line 2190E - PLS13-057
was targeted as a follow-up test to hole PLS13-040 (see news release
March 11, 2013), which was targeted on an EM conductor and coincident
intense resistivity low located ~2.2km to the east of the R00E Zone.
Hole 040 was interpreted to be analogous to the northern semipelitic
unit which bounds mineralization further to the west in R780E. Hole 057
was drilled to test further to the south where it was interpreted to be
in the pelitic corridor. However no pelite was encountered in hole 057
and no associated mineralization. Overall uranium values are low,
ranging from <2ppm to 5ppm.
Line 990E - PLS13-063
was targeted based on a limited radon anomaly coincident with one of
the central EM conductors and a resistivity low. Basement rock was
encountered at 54.5m. A favorable sequence of alternating pelitic and
semi-pelitic gneiss was intersected from 54.5m - 163.7m (end of hole). A
Diabase unit was intersected from 128.7m - 132.4m. Overall uranium
values are low, ranging from <2ppm to 13 ppm.
Composited U3O8 mineralized intervals are summarized in Table 4 below.
| Table 4: R00E Zone - Composited Mineralized Intervals (Down-hole measurements) | ||||||
| Zone | Hole ID |
Grid
Line
| From (m) | To (m) | Interval (m) | U3O8 (wt%) |
| Regional | PLS13-057 | 2190E | No signficant mineralization | |||
| | PLS13-063 | 990E | No signficant mineralization | |||
| Composite Parameters | ||||||
| 1. | Minimum Thickness: 0.50m | ||
| 2. | Grade Cut-Off: 0.05 U3O8 (wt%) | ||
| 3. | Maximum Internal Dilution: 2.00m |
Composited
U3O8 mineralized intervals are summarized in Tables 1-4. Samples from
the drill core are split in half on site. Most samples are standardized
at 0.5m down-hole intervals. One-half of the split sample is sent to the
laboratory for analysis and the other half remains on site for
reference. All intersections are down-hole, core interval measurements
and true thickness are yet to be determined.
Split core
samples were submitted to SRC Geoanalytical Laboratories (an SCC ISO/IEC
17025: 2005 Accredited Facility) of Saskatoon for assay analysis, which
includes a 63 element ICP-OES, uranium by fluorimetry (partial
digestion), and boron. Samples within mineralized intervals and any
samples which return >500ppm U, are assayed for weight % U3O8, as well as fire assayed for gold. Further assay results will be released when received.
Patterson Lake South Property
The
31,039 hectare PLS project is a 50%/50% Joint Venture held by Fission
Uranium Corp. and Alpha Minerals Inc (AMW). Fission Uranium Corp is the
Operator. PLS is accessible by road with primary access from all-weather
Highway 955, which runs north to the former Cluff Lake mine, (>60M
lbs of U3O8 produced), and passes through the nearby UEX-Areva Shea
Creek discoveries located 50km to the north, currently under active
exploration and development. Updated maps and assay tables can be found
on Fission Uranium Corp's website at http://www.fissionuranium.com/projects/patterson-lake-south-sk/.
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 the company by Ross
McElroy, P.Geol., President and COO for Fission Uranium Corp., a
qualified person.
FISSION URANIUM CORP.
is a Canadian-based resource company specializing in the strategic
acquisition, exploration and development of uranium properties and is
headquartered in Kelowna, British Columbia. Fission Uranium Corp's
Common Shares are listed on the TSX Venture Exchange under the symbol
"FCU".
This press release contains "forward-looking
information" that is based on Fission's current expectations, estimates,
forecasts and projections. This forward-looking information includes,
among other things, statements with respect to Fission'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 Fission'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. Fission disclaims
any intention or obligation to update or revise forward-looking
information, whether as a result of new information, future events or
otherwise.
ON BEHALF OF THE BOARD
Ross McElroy, President & COO
Neither
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.
Rich Matthews
Investor Relations
877-868-8140
ir@fissionuranium.com
www.fissionuranium.com
Fission Acquires 100% of 15,373 ha Uranium Property With High Grade Showings on Surface Over 3% U3O8
KELOWNA, BRITISH COLUMBIA--http://www.juniorminingnetwork.com/junior-miner-news/news-releases/631-tsx-venture/fcu/13701-fission-acquires-100-of-15-373-ha-uranium-property-with-high-grade-showings-on-surface-over-3-u3o8.html
(Marketwired - June 3, 2013) - FISSION URANIUM CORP. ("Fission" or "the Company") (TSX VENTURE:FCU)(FRANKFURT:2FU)
is pleased to announce the addition of three new properties, staked by
Fission's technical team, in the northwest and northeast Athabasca Basin
regions, Canada.
The newly acquired properties are referred to as
Beaver River, Thompson Lake and Manitou Falls respectively. The new
acquisitions are part of Fission's objective to stake ground where
Uranium mineralization is highly prospective and shallow, as is the case
with its recent high grade discoveries at PLS and Patterson Lake (PLN)
properties.
Beaver River and Thompson Lakes properties
are located in the Beaverlodge district. Between 1953 and 1982 this area
produced 25,142 tons of Uranium from 16 operating mines (Saskatchewan
Industry and Resources Misc Report 2003-7). The Manitou Falls property
is located within the eastern Athabasca Basin, where it overlies the
Mudjatic domain basement rocks.
Ross McElroy, President, COO, and Chief Geologist for Fission, commented,
"While
our primary focus remains expanding the PLS discovery, there are still
many underexplored areas of the Athabasca Basin and we consider these
new properties to be highly prospective additions to our growing
portfolio."
Highlights
Beaver River:
Six claims totalling 15,373 ha located on the north-central edge of the
Basin. The property includes most of the known electro-magnetic (EM)
conductors in the area and a number of uranium showings including
surface outcrop sample assays of 3.66%, 3.37%, and 2.93% U3O8. The
Company considers this property to be highly prospective and aims to
begin ground exploration work this summer in order to identify drill
targets for a winter drill program.
Thompson Lake:
Single claim of 1,188 ha is located approximately 15km west of Uranium
City and is situated geologically approximately 10km north of the
north-central area of the Athabasca Basin, approximately 5km west of the
historic Lorado mine, where 89 tons of uranium were produced. The
historic Gulch uranium deposit, reported at 310,000 tons of possible
reserves at 0.09% U3O8 (SK ECON, Saskatchewan Mining Deposit Database)
lies 2.5km to the south-west on strike of the property 15km from Uranium
City. Previous exploration has identified numerous uranium showings
including outcrop grab sample assays at this property include 2.23% and
0.11% U3O8.
Manitou Falls:
Single claim
of 2,941 ha located on the northeastern side of the Athabasca Basin.
The eastern side of the Athabasca Basin is significant as it is home to
all of Canada's current production of uranium. The property benefits
from a large amount of historical data from surveys and ground
prospecting work that has identified six radiometric anomalies and
multiple conductors.
Updated maps can be found on the Company's website at http://www.fissionuranium.com.
About Fission Uranium Corp.
Fission
Uranium Corp. is a Canadian-based resource company specializing in the
strategic acquisition, exploration and development of uranium properties
and is headquartered in Kelowna, British Columbia. Common Shares are
listed on the TSX Venture Exchange under the symbol "FCU".
ON BEHALF OF THE BOARD
Ross McElroy, President & COO
Cautionary Statement:
Certain
information contained in this press release constitutes
"forward-looking information", within the meaning of Canadian
legislation. Generally, these forward-looking statements can be
identified by the use of forward-looking terminology such as "plans",
"expects" or "does not expect", "is expected", "budget", "scheduled",
"estimates", "forecasts", "intends", "anticipates" or "does not
anticipate", or "believes", or variations of such words and phrases or
state that certain actions, events or results "may", "could", "would",
"might" or "will be taken", "occur", "be achieved" or "has the potential
to".
Forward-looking statements contained in this press release may
include statements regarding potential spin-out and listing of Fission
Uranium and the future operating or financial performance of Fission and
Fission Uranium which involve known and unknown risks and uncertainties
which may not prove to be accurate.
Actual results and outcomes may
differ materially from what is expressed or forecasted in these
forward-looking statements. Such statements are qualified in their
entirety by the inherent risks and uncertainties surrounding future
expectations. Among those factors which could cause actual results to
differ materially are the following: market conditions and other risk
factors listed from time to time in our reports filed with Canadian
securities regulators on SEDAR at www.sedar.com.
The forward-looking statements included in this press release are made
as of the date of this press release and the Company and Fission Uranium
disclaim any intention or obligation to update or revise any
forward-looking statements, whether as a result of new information,
future events or otherwise, except as expressly required by applicable
securities legislation.
Neither
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.
Rich Matthews
Investor Relations
877-868-8140
ir@fissionurnaium.com
www.fissionuranium.com...
Fission Uranium: Summer Program to Follow-Up Surface Uranium Boulders at North Shore, AB
KELOWNA, BRITISH COLUMBIA--http://www.juniorminingnetwork.com/junior-miner-news/news-releases/631-tsx-venture/fcu/14343-fission-uranium-summer-program-to-follow-up-surface-uranium-boulders-at-north-shore-ab.html
(Marketwired - June 17, 2013) - FISSION URANIUM CORP.
(TSX VENTURE:FCU) (FRANKFURT:2FU) (the "Company" or "Fission), is
pleased to report an update on its exploration program plan for the
highly prospective North Shore project, located in the northwest area of
the Athabasca Basin in Alberta.
The decision to advance exploration
plans is a result of the completion of the Alberta Government's Lower
Athabasca Regional Plan (LARP). The North Shore project now consists of
17 Metallic and Industrial Mineral Permits ("MAIM") totaling
approximately 55,160 ha.
Since December 2010, Fission has been granted a
work assessment deferral, pending the results of the LARP Conservation
Areas decision. Exploration plans are being advanced for the summer 2013
period, to include a high resolution airborne radiometric survey and
followed up by ground prospecting, geophysics, and radon surveys in high
priority areas.
Property Highlights include:
- Identification of several anomalous uranium showings in boulders and outcrop, including sandstone boulders grading up to 1.39% U3O8
- Located on the NW edge of the Athabasca Basin, with targets expected to be at shallow depth
Ross McElroy, President, COO, and Chief Geologist for Fission, commented,
"The
completion of the LARP will allow us to advance our exploration at the
North Shore project. The North Shore fits with Fission's strategy of
exploring high priority shallow exploration targets within and around
the world premiere Athabasca Basin uranium district. While our primary
focus remains expanding the PLS discovery, there are still many
underexplored areas of the Athabasca Basin and we consider this property
to be an important land package in our growing portfolio."
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 the company by Ross
McElroy, P.Geol. President and COO for Fission Uranium Corp., a
qualified person.
FISSION URANIUM CORP.
is a Canadian based resource company specializing in the strategic
acquisition, exploration and development of uranium properties and is
headquartered in Kelowna, British Columbia. Fission Uranium Corp's
Common Shares are listed on the TSX Venture Exchange under the symbol
"FCU".
This press release contains "forward-looking
information" that is based on Fission's current expectations, estimates,
forecasts and projections. This forward-looking information includes,
among other things, statements with respect to Fission'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 Fission'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. Fission disclaims
any intention or obligation to update or revise forward-looking
information, whether as a result of new information, future events or
otherwise.
ON BEHALF OF THE BOARD
Ross McElroy, President & COO
Rich Matthews
Investor Relations
TF: 877-868-8140
ir@fissionuranium.com
www.fissionuranium.com
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