
Yankee Hat Makes High Grade Tungsten Discovery Kidlark Project, Yukon
October 29, 2008
Yankee Hat’s Joint Venture with JOGMEC Yields Significant Results in First Year
Vancouver, BC – October 29th, 2008 – Yankee Hat Minerals Ltd. (“Yankee Hat” or the “Company”) (TSX-V: KHT) is pleased to announce that as a result of the regional joint venture grassroots exploration program with the Japan Oil, Gas and Metals National Corporation (“JOGMEC”) a new property, Kidlark, has been explored. Surface sampling has returned high grade tungsten assay results from this scheelite skarn occurrence.
The Kidlark Property was explored in late July, and company geologists immediately staked 32 claims covering several visually impressive scheelite-bearing garnet skarn tungsten showings. The property, located within the Pelly Mountains, is approximately 90 kilometers northeast of Whitehorse, and 45 km west-northwest of Quiet Lake along the South Canol Highway. It lies less than 20 km northeast of Livingstone, an active placer gold operational area serviced by an active airstrip and winter road access.
Eighteen grab samples were taken from the Kidlark Property and submitted to EcoTech Laboratories in Whitehorse for testing. Assay results for the samples ranged up to 7.68% WO3 and averaged 1.463% WO3 with visual estimations of scheelite content by UV fluorescence correlating well with WO3 % content. The 18 samples were taken from 5 distinct showings over 13 kilometers along a single geological contact.
Table: Grab Sample Results Kidlark Project, Yukon
Sample ID |
W (%) |
WO3 (%) |
Description |
KL-08-AAB-0034
Brand Showing A |
0.382 |
0.482 |
Crumbly and rusty massive sch-py-po rock adjacent to a vuggy siliceous zone. Scheelite is fine to coarse grained, with crystals to 1 cm2 |
KL-08-AAB-0035
Brand Showing B |
3.490 |
4.401 |
Siliceous vuggy zone, adjacent to a banded gt-diop skarn. Moderate scheelite mineralization with py-po. |
KL-08-AAB-0036
Brand Showing C |
0.982 |
1.238 |
Dark green, rusty, vuggy diop skarn – well lamping (under Ultra-Violet light) |
KL-08-AAB-0037
Brand Showing D |
2.940 |
3.708 |
Dark green, rusty, vuggy diop skarn – well lamping (under Ultra-Violet light) |
KL-08-AAB-0038
Brand Showing E |
2.450 |
3.090 |
Dark green, rusty, vuggy diop skarn – well lamping (under Ultra-Violet light) |
KL-08-CGD-0042
Davis Showing |
6.090 |
7.680 |
Rusty skarn zone with massive sch/py/po up to 1m in thickness. Next to rusty metasediments ~5 m in width and talus. |
KL-08-CGD-0043
Davis Showing |
0.054 |
0.068 |
Rusty skarn zone with massive py/po Next to rusty metasediments ~5 m in width and talus. No visible scheelite. |
LVA 0080
Wilson Showing |
<0.001
|
|
Entire showing comprises coarse grained dark red to brown garnet dominated skarn zone approximately 2 m thick with patches of coarse scheelite – no visible scheelite in sample LVA0080. |
LVA 0081
Wilson Showing
|
0.344
|
0.434
|
Entire showing comprises coarse grained dark red to brown garnet dominated skarn zone approximately 2 m thick with patches of coarse scheelite – visible scheelite in sample LVA0081. |
CGD 0060
Near Brand Showing |
0.001
|
0.001
|
Sand sample consisting of dolomitic limestone occurring at granite contact. |
CGD 0061 A
Near Brand Showing |
0.113
|
0.143
|
Rusty garnet epidote skarn zone containing books of medium grained muscovite. Moderate visible scheelite. |
CGD 0061 B
Near Brand Showing |
0.024
|
0.030
|
Rusty garnet epidote skarn zone containing books of medium grained muscovite. No visible scheelite. |
CGD 0062
Arness Showing |
0.072 |
0.091 |
Rusty skarn zone near contact. Visible scheelite seen. |
CGD 0063
Arness Showing |
0.007 |
0.009 |
Rusty skarn zone near contact with quartz flooding. Visible scheelite seen. |
CGD 0064
Davis Showing |
0.675
|
0.851
|
Rusty skarn zone with massive sch/py/po up to 1m in thickness. Next to rusty metasediments ~5 m in width and talus. |
CGD 0065
Near Davis Showing |
1.140 |
1.438 |
Rusty skarn zone with massive sch/py/po up to 1m in thickness. At granite contact. |
CGD 0066
Near Davis Showing |
0.893 |
1.126 |
Rusty skarn zone with massive sch/py/po up to 1m in thickness. At granite contact. |
CGD 0067
Rasmussen Showing |
0.068 |
0.086 |
Garnet skarn with quartz flooding. At granite – limestone contact. |
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Mineral abbreviations: sch=scheelite, po=pyrrhotite, py=pyrite, diop=diopside |
Based on the promising initial exploration results, Yankee Hat has expanded the property by staking an additional 70 claims. This brings the total number of claims to 102, with rough dimensions of 13 kilometers by 2 km and an area of approximately 2,100 hectares. The Company also completed detailed mapping, prospecting, silt and soil sampling, trenching, and ground magnetic work through the month of August and early September. The results of this work are pending and the company will report further once it is received and compiled. Maps and sample photos have been posted on http://yankeehatminerals.com/properties/kidlark
Already at least five distinct mineralized zones (from North to South; Wilson, Rasmussen, Davis, Brand and Arness showings) have been located in outcrop along a 13 kilometer strike length. The known outcrops are variably mineralized, but in general are characterized as garnet-diopside skarn with minor to major pyrrhotite. Tungsten is found thus far as the mineral scheelite. Typically, the mineralized area begins in barren limestone, moving through recrystallized marble, garnet-diopside skarn, a vuggy quartz-pyrite flooded zone, fluid-altered multiphase heterogeneous granite, and unaltered homogeneous granite. Scheelite also occurs within intrusive dykes.
At Kidlark, the Dycer Creek Pluton intrudes into Lower Paleozoic carbonate-bearing continental platform sedimentary sequences of the Cassiar Platform. This geological setting has also given rise to the nearby Risby and Stormy tungsten deposits, as well as to the Northern Dancer tungsten-molybdenite deposit (also known as Logtung) further to the southwest.
The Kidlark discovery was made as a result of Yankee Hat’s generative tungsten exploration program with JOGMEC in southeastern Yukon Territory. The 2008 generative program had a budget of C$920,000 and is funded 60% by JOGMEC and 40% by Yankee Hat. JOGMEC earlier contributed $200,000 to the program that was used primarily for claims and acquisition of an extensive geological data base. Under the joint generative exploration agreement JOGMEC will have the right to acquire a 60% interest in the Kidlark Property, if it is deemed a Designated Property, by funding its pro-rata share of future exploration expenditures. If the property is not selected as a Designated Property, it will be 100% owned by Yankee Hat.
The outlook for the price of tungsten is positive, supported by strong growth in Chinese consumption, and a lack of new primary supply. Given its unique physical attributes, tungsten has many applications in which it is virtually irreplaceable including light bulbs and electrical applications, and as a wear-resistant “super alloy” used in the mining, petroleum, military, construction and metalworking industries.
China currently produces roughly 85% of the world’s tungsten and has recently begun to restrict foreign access to the tungsten it produces. With China hoarding its production for its own growth, the rest of the world is scrambling to find new sources of supply as prices move upwards.
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 Mr. Terence Schorn, P.Geo, Chairman of Yankee Hat, and a qualified person.
Grab samples were submitted to EcoTech Laboratories Ltd. in Whitehorse for conventional dissolution and analysis for a range of major and trace elements, including tungsten. Due to the refractory nature of scheelite (CaWO4) more robust dissolution was carried out to ensure accurate measurement of tungsten in the samples.
ABOUT YANKEE HAT MINERALS:
Yankee Hat Minerals Ltd. is a publicly held resource company that utilizes its management’s expertise in mineral exploration and evaluation, and financial acumen, to identify, acquire, and develop mineral prospects in mining friendly jurisdictions with the potential to host large-scale discoveries. The company strategically focuses on advanced stage projects and commodities that have strong underlying price fundamentals such as tungsten, rare earth elements, copper, and gold.
Investors are invited to visit Yankee Hat's IR Hub at http://www.agoracom.com/ir/yankeehatminerals where they can post questions and receive answers or review questions and answers already posted by other investors. Alternatively, investors are able to e-mail all questions and correspondence to KHT@agoracom.com where they can also request to be added to the investor email list to receive all future press releases and updates in real time.
ON BEHALF OF THE BOARD OF DIRECTORS
“P. Bradley Kitchen”
P. Bradley Kitchen
President, CEO, and Director
For further information, please contact:
Corporate Inquiries:
Nance Massicotte
IR Pro Communications (Vancouver)
Ph: 604.507.3377
Toll Free: 1.866.503.3377
Email: nance@irprocommunications.com
Gus Garisto
Bay Street Connect (Toronto)
Ph: 416.607.6023
Email: gus@baystreetconnect.com
Investor Relations:
AGORACOM Investor Relations
Web: http://www.agoracom.com/IR/YankeeHatMinerals
Email: KHT@agoracom.com
This news release has been prepared by management. The TSX Venture Exchange has not reviewed and does not accept responsibility for the adequacy or accuracy of this news release. This document contains certain forward looking statements which involve known and unknown risks, delays, and uncertainties not under the Company’s control which may cause actual results, performance or achievements of the Company to be materially different from the results, performance or achievements implied by these forward looking statements. We seek safe harbour.
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