Kivalliq Energy Corporation ("Kivalliq") (TSX VENTURE:KIV) today announced
results from five diamond drill holes at the Nine Iron Trend. The Nine Iron
Trend (a portion of which was formerly referred to as the "BIF Zone") is located
approximately 10 kilometres southeast of the Lac Cinquante Uranium Deposit and
five kilometres southwest of Kivalliq's Nutaaq camp. Nine Iron is one of six
mineralized zones discovered this year within the 340,268 acre Angilak Property
in Nunavut, Canada.


Key Point Summary



--  The Nine Iron Trend is outlined by a distinct, nine kilometre long
    magnetic geophysical anomaly extending below the contact or 
    "unconformity" with the Angikuni Basin 
--  Drilling in 2012 at the east end of Nine Iron Trend intersected
    anomalous uranium in five holes over a strike length of 100 metres, and
    to a vertical depth of 154 metres 
--  Significant uranium mineralization was intersected in three of five
    diamond drill holes: 
    --  0.45% U3O8 over core interval of 0.9 metres in hole 12-BIF-001 
    --  0.28% U3O8 over core interval of 1.3 metres in hole 12-BIF-002 
    --  0.24% U3O8 over core interval of 2.1 metres in hole 12-BIF-003 
--  Prospecting samples taken in 2011 along three kilometres of the Nine
    Iron Trend returned high grade uranium assays 
--  87,438 acres in 38 new strategic claims staked in 2012 increase Angilak
    Property to 340,268 total acres 



"The Nine Iron Trend is located five kilometres from any previously known
mineralization and is a completely new target area within the Angilak Property.
This trend combines significant uranium in drill core with highly mineralized
surface samples, along a sizable geophysical signature that strikes beneath the
Angikuni Basin unconformity," stated Kivalliq's President Jeff Ward. "We
consider Nine Iron to be more evidence of the District Scale potential of the
Angilak Property, and a high priority unconformity-related target for 2013."


Nine Iron Trend

The Nine Iron Trend was initially recognized during the 2011 prospecting program
while investigating historic reports of mineralized showings in the area.
Discontinuous high-grade U-Cu-Mo-Ag mineralization was identified in samples
taken from multiple veins (1 to 3 cm wide) occurring in outcrop and sub-crop
over three kilometres of strike length. Assay results from prospecting include
13 of 25 grab samples exceeding 1% U3O8 and 5 samples with over 15% U3O8 (see
news release dated January 12, 2012 - formerly BIF Zone). These results prompted
ground geophysical surveying and geological mapping which revealed a
southwest-trending magnetic anomaly that coincided with both prospecting results
and a 10 kilometre by one kilometre belt of Archean aged metasedimentary rocks.
The magnetic trend and host rocks sit on the southeastern flank of the Yathkyed
Greenstone Belt and trend westward below an unconformable contact with the
Proterozoic age Angikuni Basin.


Based on the 2011 ground geophysics and mapping, a number of targets were tested
by reverse circulation exploratory drilling (RC) and subsequent diamond drilling
in 2012. In total, 841 metres in five core holes were drilled from three sites
at the northeast end of the Nine Iron Trend. Holes were spaced 50 metres apart
along 100 metres of strike length, and drilled to the north at azimuths of 330
degrees and inclinations ranging from -45 degrees to -65 degrees. Uranium
mineralization was intersected in all five holes at vertical depths between 17
and 154 metres. Weighted assay results from down hole core intervals in five
diamond drill holes at Nine Iron are presented in the table below:




---------------------------------------------------------------------------
     2012 Nine Iron Trend Diamond Drill Hole Weighted Assay Results(i)     
---------------------------------------------------------------------------
              From    To Interval(ii)   U3O8    Cu    Mo    Ag             
DDH            (m)   (m)      (m)        (%)   (%)   (%) (g/t)  Description
---------------------------------------------------------------------------
12-BIF-001    23.9  24.3      0.4       0.13  0.01  0.08   3.7  Nine Iron  
---------------------------------------------------------------------------
12-BIF-001    33.4  34.3      0.9       0.45  0.01  0.01   0.9  Nine Iron  
---------------------------------------------------------------------------
12-BIF-001    41.4  41.7      0.3       0.13  0.01  0.05   2.4  Nine Iron  
---------------------------------------------------------------------------
12-BIF-001    44.6  45.6      1.0       0.31  0.01  0.01   1.8  Nine Iron  
---------------------------------------------------------------------------
12-BIF-001    59.4  62.1      2.7       0.08  0.01  0.01   1.4  Nine Iron  
---------------------------------------------------------------------------
12-BIF-001    97.5  97.8      0.3       0.28  0.02  0.02   4.0  Nine Iron  
---------------------------------------------------------------------------
12-BIF-002    21.6  22.5      0.9       0.19  0.01  0.08   3.4  Nine Iron  
---------------------------------------------------------------------------
12-BIF-002    30.9  32.2      1.3       0.28  0.01  0.01   0.6  Nine Iron  
---------------------------------------------------------------------------
12-BIF-002    43.0  43.3      0.3       0.09  0.01  0.04   4.1  Nine Iron  
---------------------------------------------------------------------------
12-BIF-002    62.1  62.4      0.3       0.10  0.00  0.18   1.6  Nine Iron  
---------------------------------------------------------------------------
12-BIF-002    83.4  84.1      0.7       0.22  0.02  0.03   3.8  Nine Iron  
---------------------------------------------------------------------------
12-BIF-003   109.8 111.9      2.1       0.24  0.01  0.02   3.6  Nine Iron  
---------------------------------------------------------------------------
12-BIF-003   197.7 198.7      1.0       0.04  0.02  0.00   0.1  Nine Iron  
---------------------------------------------------------------------------
12-BIF-003   212.5 212.8      0.3       0.13  0.04  0.02   3.7  Nine Iron  
---------------------------------------------------------------------------
12-BIF-004    36.5  36.9      0.4       0.10  0.01  0.00   1.2  Nine Iron  
---------------------------------------------------------------------------
12-BIF-004    38.8  39.3      0.5       0.40  0.05  0.00   4.0  Nine Iron  
---------------------------------------------------------------------------
12-BIF-004    40.7  41.0      0.3       0.10  0.02  0.01   0.8  Nine Iron  
---------------------------------------------------------------------------
12-BIF-004    93.2  93.6      0.4       0.40  0.08  0.03   7.3  Nine Iron  
---------------------------------------------------------------------------
12-BIF-004   104.7 105.3      0.6       0.29  0.01  0.05   7.0  Nine Iron  
---------------------------------------------------------------------------
12-BIF-005   105.3 105.6      0.3       0.26  0.03  0.00   4.0  Nine Iron  
---------------------------------------------------------------------------
12-BIF-005   147.5 148.1      0.6       0.07  0.01  0.11  10.2  Nine Iron  
---------------------------------------------------------------------------
(i) All samples are subjected to ICP1 Analysis by Saskatchewan Research     
Council Geoanalytical Laboratories "SRC" in Saskatoon, Canada. ICP1 results 
greater than 1,000 ppm U are subjected to SRC U3O8 Assay; ICP1 results for  
Cu, Mo and Ag are reported by SRC in parts per million (ppm). 1 ppm = 1gm/t,
10,000 ppm = 1%; Intervals include ICP U analysis in ppm converted to U3O8%.
Conversion to U3O8% = ppm x 0.0001179.                                      
(ii) Down-hole core interval. True widths cannot be estimated at this time  



To view cross sections, assays and drill plan maps from the 2012 exploration
program, please visit: http://www.corebox.net/properties/angilak/ or
www.kivalliqenergy.com/projects/angilak/program_images/


Nine Iron Geology

Uranium mineralization along the Nine Iron Trend is structurally controlled,
occurring in narrow, discontinuous high-grade breccia veins, low-grade fracture
fillings associated with hematite alteration, and at contacts between
metasedimentary layers in the hanging wall of banded iron formation (BIF).
Emplacement of mineralization is strongly controlled by rock-layer competency
contrasts, such as sediment contacts, or the margins of semi conformable
granitic and trachytic dykes. The metasedimentary package is composed largely of
sandy pelite and tuffaceous turbidites, and contains a 20-30 metre--thick
horizon dominated by quartz-magnetite banded iron formation, the unit
responsible for the Nine Iron magnetic response.


Staking

Throughout the 2012 exploration season, an additional 38 claims totaling 87,438
acres were staked to protect several strategic areas near the Angilak Property
boundaries. Of these, a block of 23 claims were staked south of the Lac 50
Trend, covering the western half of the Nine Iron magnetic trend, where it
extends below the Angikuni Basin unconformity. Upon final approval of new claims
by the Nunavut Mining Recorder, the Angilak Property will total 340,268 acres.


QA/QC

Half-spilt NQ core samples from Angilak Property drill holes having anomalous
radioactivity levels above 200 cps were sent to the Saskatchewan Research
Council Geoanalytical Laboratories ("SRC") for analysis. All samples were
analyzed for U3O8 and a multi-element suite. The SRC facility operates in
accordance with ISO/IEC 17025:2005 (CAN-P-4E), General Requirements for the
Competence of Mineral Testing and Calibration laboratories and is accredited by
the Standards Council of Canada. The samples are first analyzed by SRC's ICP-OES
multi-element Uranium exploration ICP1 method. The method analyzes for
multi-elements including Ag, Mo, Cu, Pb, Zn and a suite of rare earth elements.
ICP results U greater than 1,000 parts per million (ppm) are analyzed using
SRC's ISO/IEC 17025:2005-accredited U3O8 Assay method. Laboratory quality
control (QC) includes a repeat analysis on every 20th sample. Repeat samples had
good reproducibility. Kivalliq's quality assurance and quality control
procedures include the systematic insertion of blanks and standards into the
drill core sample string. All QA/QC results were within expectations.


Jeff Ward, P.Geo. and President of Kivalliq is a Qualified Person as defined
under National Instrument 43-101 and has reviewed and approved the scientific
and technical information contained in this news release.


About Kivalliq Energy Corporation

Kivalliq Energy Corporation (TSX VENTURE:KIV) is a Vancouver-based uranium
exploration company holding Canada's highest grade uranium deposit outside of
Saskatchewan's Athabasca Basin. The Company's flagship project, the 340,268 acre
Angilak Property in Nunavut Territory, is host to the Lac Cinquante Deposit with
a NI 43-101 Inferred Resource of 1,779,000 tonnes grading 0.69% U3O8, totaling
27.13 million pounds U3O8. Kivalliq's comprehensive exploration programs
continue to advance the Lac Cinquante Deposit and demonstrate the "District
Scale" potential of the Angilak Property.


Kivalliq's team of northern exploration specialists have forged strong
relationships with sophisticated resource sector investors and project partner
Nunavut Tunngavik Inc. ("NTI") in order to advance the Angilak Property.
Kivalliq was the first company to sign a comprehensive agreement to explore for
uranium on Inuit Owned Lands in Nunavut Territory, Canada and is committed to
building shareholder value while adhering to high levels of environmental and
safety standards and proactive local community engagement.


On behalf of the Board of Directors

James R. Paterson, CEO

Kivalliq Energy Corporation

Kivalliq Energy Corporation is a member of the Aurora Mineral Resource Group of
companies.


Certain disclosures in this release, including the growth and value of the
Angilak Property, constitute forward-looking statements that are subject to
numerous risks, uncertainties and other factors relating to Kivalliq's
operations as a mineral exploration company that may cause future results to
differ materially from those expressed or implied in such forward-looking
statements, including risks as to market price of Kivalliq's securities and the
market for securities of resource exploration companies in general; commodity
prices and, in particular, the price of uranium and the completion of Kivalliq's
plans and projects. Readers are cautioned not to place undue reliance on
forward-looking statements. Other than as required by applicable securities
legislation, Kivalliq expressly disclaims any intention or obligation to update
or revise any forward-looking statements whether as a result of new information,
future events, or otherwise.




FOR FURTHER INFORMATION PLEASE CONTACT: 
Kivalliq Energy Corporation
James R. Paterson
CEO
604.646.4527 or Toll Free: 1.888.331.2269
info@kivalliqenergy.com
www.kivalliqenergy.com and www.auroraresource.com
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