FJORDLAND EXPLORATION INC.

News Releases:

July 29, 2010
Gold Fields Commences 5000 m Drilling Program on Southeast Zone, Woodjam South, British Columbia (more...)

July 27, 2010
Woodjam North: Drilling at Deerhorn Zone Yields 115.9 m Grading 0.287g/t Gold and 0.321% Copper. Initial Drilling at Spellbound Area Provides Encouraging Results (more...)

July 7, 2010
Fjordland Provides Update on Sampling Programs on Six Copper-Gold-Molybdenum Prospects in North-Central BC (more...)

July 6, 2010
Gold Fields Completes Due Diligence on Woodjam South Property, BC (more...)

June 2, 2010
Fjordland Expands Tak Gold-Copper Property Portfolio (more...)

May 26, 2010
Gold Fields Granted Option on Woodjam South Property, BC (more...)

Market Coverage:

July 2010 - Northern Miner
Fjordland, Cariboo shift Woodjam (read more...)

July 2010 - Resource World
Woodjam Gold-Copper Project Looking Good (read more...)

March 2010 - Midas Newsletter
Fjordland's Discoveries Attract Major Miners (read more...)

February 2010 - Lawrence Roulston
Fjordland Exploration (read more...)

June 2009 - AME BC
Intersections - Digging deeper for high quality products (read more...)

August 2009 - Dow Jones Newswires
CANADA VENTURE: Fjordland A Diversified Copper-Gold Play (read more...)

January 2009 - Research Capital
Fjordland makes Research Capital's "Drillers Dozen" to highlight some of the best new discoveries of the past 3 years (read more...)

ST Property

Location

Compilation

The ST property lies approximately 35 kilometres south of Prince George. The property consists of 6 mineral claims with a total area of 2,878 hectares.

The southern 75% of the property is underlain mainly by Proterozoic to Paleozoic-aged sedimentary rocks of the Snowshoe Group. The northernmost portion of the property is underlain by Triassic-aged Takla Group fine clastic sedimentary rocks. The sedimentary packages are intruded by Cretaceous-aged granitic intrusives of the Naver Pluton.

In 2007, an airborne magnetic survey was completed over the northern portion of the property testing the contact zone between the Naver Pluton and sedimentary rocks of the Takla and Snowshoe Groups anomalies.

In 2008, a combined Induced Polarization (IP) chargeability and resistivity survey was completed on 2 lines testing an anomalous magnetic high from the airborne survey. IP delineated 4 high chargeability anomalies.

Follow-up prospecting and MMI sample collection was completed across chargeability anomalies delineated along both lines.

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