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Last C$0.10 CAD
Change Today 0.00 / 0.00%
Volume 75.5K
As of 2:04 PM 07/27/15 All times are local (Market data is delayed by at least 15 minutes).

kivalliq energy corp (KIV) Snapshot

Open
C$0.10
Previous Close
C$0.10
Day High
C$0.10
Day Low
C$0.09
52 Week High
09/5/14 - C$0.23
52 Week Low
07/20/15 - C$0.09
Market Cap
20.6M
Average Volume 10 Days
73.8K
EPS TTM
C$-0.0080
Shares Outstanding
216.8M
EX-Date
--
P/E TM
--
Dividend
--
Dividend Yield
--
Current Stock Chart for KIVALLIQ ENERGY CORP (KIV)

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kivalliq energy corp (KIV) Details

Kivalliq Energy Corporation, an exploration stage company, focuses on the acquisition, exploration, and development of resource properties. The company explores for uranium deposits. Its flagship property includes the Angilak Property covering 275,469 acres located in Nunavut Territory, Canada. The company was incorporated in 2008 and is headquartered in Vancouver, Canada.

Founded in 2008

kivalliq energy corp (KIV) Top Compensated Officers

Chief Executive Officer and Director
Total Annual Compensation: C$174.7K
President
Total Annual Compensation: C$165.0K
Chief Financial Officer
Total Annual Compensation: C$70.5K
Chief Operating Officer
Total Annual Compensation: C$180.0K
Compensation as of Fiscal Year 2014.

kivalliq energy corp (KIV) Key Developments

Kivalliq Energy Corporation Commences 2015 Exploration Program at Angilak Property

Kivalliq Energy Corporation commenced exploration at the company's Angilak Property in Nunavut Territory, Canada. The focus of the program will be drill testing the high priority Dipole target and advancing multiple uranium targets in the Dipole-RIB Trend through geochemical surveying. The first phase of a CAD 1.5 million 2015 exploration program has commenced at Kivalliq's 100% owned, 105,280 hectare (260,154 acre) Angilak Property. Staff and supplies were mobilized to the existing Nutaaq camp in late June. Kivalliq plans to drill up to 1,000 metres in six holes at Dipole in July, using one of three diamond drill rigs already on site. Ground geochemical surveying will run concurrently with the drill program, following-up on high priority targets identified during the 2014 season at Dipole and RIB. The Dipole-RIB Trend is located approximately 25 kilometres southwest of Lac 50, in a northeast trending belt of Archean metavolcanic rock interpreted to be equivalent to Lac 50 resource host rocks. Based on corroborative geophysical and geochemical exploration, Dipole and RIB are excellent analogues to the Lac 50 deposit. The RIB target, located four kilometres south of Dipole, was identified by Noranda Exploration Ltd. in 1976 as a one kilometre long basement conductor on the western margin of the Angikuni Basin unconformity. During 1977-78, 14 of 25 diamond drill holes intersected uranium mineralization at shallow depths (less than 35 metres), with the two best intercepts being 0.19% U3O8 over 9.3 metres (including 0.52% U3O8 over 2.6 metres) and 1.61% U3O8 over 0.7 metres. Exploration by Kivalliq in 2014 confirmed the RIB conductor using airborne Versatile Time Domain Electromagnetic (VTEM) geophysics. EL soil samples also outlined a corresponding 3.6 kilometre long uranium geochemical trend, demonstrating that historic work tested only a portion of the RIB target. Due to geological similarities with both Dipole and Lac 50, the RIB target warrants further infill geochemical work in 2015.

Kivalliq Energy Corp. Announces Summer Program at Hatchet Lake Advances Priority Target Areas

Kivalliq Energy Corp. announced the completion of the summer exploration program at Kivalliq’s 100% owned Hatchet Lake Property in the Athabasca Region of Saskatchewan. Kivalliq conducted its first exploration program at the 13,711 hectare (33,881 acre) Hatchet Lake Property between June 1 and June 23. The focus was on multiple unconformity-related basement targets based on results from over $750,000 in previous exploration performed by Hathor Exploration Limited (Hathor) and Rio Tinto Canada Uranium Corporation (Rio Tinto). Kivalliq’s 2015 summer program, budgeted at CAD 500,000, was comprised of prospecting, mapping, ground magnetometer /very low frequency (VLF) electromagnetic (EM) geophysical surveys, and biogeochemical (vegetation-black spruce) /soil geochemical surveys. The program was designed to verify airborne geophysical signatures and confirm uranium anomalism in priority areas.

Roughrider Exploration Limited and Kivalliq Energy Corporation Announces Results from the Ground Magnetometer and Very Low Frequency Electromagnetic Geophysical and Biogeochemical Sampling Surveys at the Jurgen 1 and Jurgen 2 Targets

Roughrider Exploration Limited and Kivalliq Energy Corporation announced the results from the ground magnetometer and very low frequency (VLF) electromagnetic (EM) geophysical and biogeochemical sampling surveys completed March 30, 2015 at the Jurgen 1 and Jurgen 2 targets. The Jurgen 1 and Jurgen 2 uranium target areas are located in the western portion of the Genesis property on Wellbelove Bay of Wollaston Lake, eastern Athabasca, approximately 60 kilometres along the Wollaston-Mudjatik lithostructural corridor from Cameco Corporation's Eagle Point uranium mine. The Jurgen 1 and Jurgen 2 ground geophysical and biogeochemical grids for the Genesis 2015 winter exploration program were designed to follow-up and tighten spacing on anomalous 2014 soil geochemical results coincident with northeast trending airborne EM geophysical conductors. In the Athabasca region, EM conductors often represent graphitic horizons in pelitic rocks that are a common host for uranium mineralization. Breaks in the general EM and magnetic trends in conjunction with elevated geochemistry may indicate structural disturbances that can be important to uranium mineralization emplacement. Ground magnetic and VLF-EM surveys were performed on two grids over the Jurgen 1 and Jurgen 2 areas during March. Approximately 70 line kilometres of ground geophysics covered geochemically anomalous areas coincident with priority airborne EM conductors. Grid lines were spaced 50 and 100 metres apart, with readings taken at 12.5 and 20 metre intervals. A total of 594 biogeochemical samples (black spruce twigs) were collected on the same survey grids at 25 to 50 metre intervals. Jurgen 1 remains a compelling target demonstrating good spatial correlation between: 1) the high uranium results from the 2015 biogeochemical program; 2) the high uranium results from the 2014 enzyme leach soil sampling program; and 3) the main Jurgen 1 EM conductive trend. At Jurgen 1, eight of 249 samples returned values above the 98th percentile for uranium and twenty-one samples returned values above the 95th percentile. The three high uranium values from the 2015 program were from samples coincident with the main Jurgen 1 conductor; 1.35ppm U, 1.64ppm U and 1.75ppm U. At Jurgen 2, eight of 296 biogeochemical samples returned values above the 95th percentile for uranium. The high uranium value on the Jurgen 2 grid was 1.26ppm U. Biogeochemistry results at the Jurgen 1 and Jurgen 2 grid areas also show anomalous associated metals (Pb, Ni, Cu, Mo, Ag) although their distributions are not conclusive. Anomalous Ni and Pb values accompany anomalous U values in places, and in the case of Ni at Jurgen 1, appear to flank the south contact of the main Jurgen 1 EM conductor. At Jurgen 2, the VLF-EM survey suggests a possible structural feature that disrupts the EM conductors mapped. Biogeochemical results for uranium at Jurgen 2 show a more subtle correlation to both the 2014 enzyme leach soil sample results and the airborne EM conductors targeted, but seem to extend to the Jurgen 1 conductor that passes through the south portion of the grid. At the Sava Lake prospect, approximately 25 kilometres east of Jurgen 2, anomalies in uranium and pathfinder elements were identified in reconnaissance level biogeochemical sampling; however, based on sampling completed to date, the anomalies at Sava Lake lack the cohesion to warrant immediate follow-up. Geophysical data review was provided by in3D Geophysics Ltd. and SJ Geophysics Ltd. The VLF-EM survey instrumentation was on board the GEM GSM-19 magnetometer units and collected data from transmission stations at Jim Creek (Seattle), Washington transmitting at 24.8 kHz and Cutler, Maine transmitting at 24.0 kHz.

 

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