TEUTON

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TUO TSX.V
TEUTON
resources corporation
Stewart-Eskay Creek Region, Northwestern British
Columbia
Bulk Tonnage Gold-Copper Target
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Eskay Creek Mine
Treaty Creek
Mitchell
Snowfield
Sulphurets
MINERAL BELT
Kerr
MINERAL BELT
TennysonProperty
East Gold
Tennyson Property 9390 acres
in prolific mineral belt
Tide
Scottie Gold
Granduc Mine
Dilworth
Silver Coin
Big Missouri
Premier Mine
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Expenditures in Mineral Belt (2007-2008)
At least 48.3 million to be spent on exploration
in the mineral belt from 2007-2008
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Eskay Creek Mine
Area Play Mineral Potential
Treaty Creek
Kerr-Sulphurets-Mitchell Property (Seabridge)
Kerr-Sulphurets-Mitchell Now Canadas Largest
Gold Deposit
Mitchell
Sulphurets
Kerr
Including measured, indicated and inferred NI
43-101 compliant
TENNYSON
Granduc Mine
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Eskay Creek Mine
Area Play Mineral Potential
Treaty Creek
Snowfield
Snowfield Property (Silver Standard)
Bruceside
Including measured, indicated and inferred NI
43-101 compliant
TENNYSON
Granduc Mine
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TENNYSON

• GRANDUC MINE
• Underground copper producer from 1968-1984
• Recent exploration extended strike of mineralized
  horizons to 4 km
• The Granduc district has the potential to host
  one of the largest Besshi deposits in the world
• Accompanying infrastructure tunnel, access road,
  airstrip
• Southern portion of Tennyson Property is within
  10km of the Granduc Mine

Airstrip
Access Tunnel
Scottie Gold
Granduc Mine
Access Road
British Columbia
Alaska
Premier Mine
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Exploration Tennyson Main Gossan
The Tennyson was discovered in 1984 after
meltback of local glaciers exposed a prominent
gossan (area marked by pervasive red-brown colour
due to oxidation of minerals). The western part
of the present-day property was incorporated in
2006 to include two additional gossans, also
exposed by retreating ice. The property includes
several areas of mineralization, the most
important being the North Porphyry Target (Cu-Au)
and Skarn Zone (Au). Tennyson gossan (Camp Zone
Au, Ag, Pb, Zn) includes volcaniclastic and
sedimentary rocks of the lower part of the
Jurassic Hazelton Group, which show a diversified
pattern of alteration (including propylitic,
argillic and phyllic) associated locally with
strong pyritization.
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Claim Status and Mineral Showings
Gossan
North Porphyry Target
Gossan
Skarn Target
Tennyson Showings

• Cu-Au North Porphyry Target
• High-grade Epithermal Target (Camp Zone)
• Skarn Target
• Two recently exposed gossans west of original
  Tennyson claims

Access Tunnel (to Granduc Mine)
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Geology Stratigraphy
The Tennyson property is located ca. 40 km NNE of
Stewart, BC. The area is underlain by suites of
volcanic and associated sedimentary rocks of the
Mesozoic Stuhini and Hazelton Groups. The layered
rocks are intruded by several plugs of granitoid
to dioritic rocks of Mesozoic and Cenozoic age.
The area hosts several broad zones of
sericite-clay alteration which are accompanied by
bulk tonnage Au-Cu mineralization zones.
Bowser Basin Sediments
Mitchell
Snowfield
Sulphurets
Bruceside
Kerr
TENNYSON
East Gold
10 km
Granduc
Scottie Gold
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Geology Stratigraphy
Geological Mapping Alteration Map (after J.M.
Logan, 1986)
Porphyry Target
Original Tennyson claims are underlain by a
succession of flows, volcaniclastics and
fine-grained sediments which show evidence of a
weak regional metamorphism (greenschist zone).
These rocks are bound eastwards, along a steep
NW-SE trending fault, to unaltered volcanic
breccias and flows. Rocks display variable
alteration including propylitic, argilic and
sericitic, with minor zones of silicification and
localized skarns. Low-grade Au-Cu mineralization
is associated with disseminated pyrite and minor
chalcopyrite while higher-grade Au-Ag
mineralization appears in association with pyrite
bands and veins as well as quartz veins.
TENNYSON
Camp Zone
Skarn Target
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Exploration History

• 1984 Staked for Teuton Resources Corporation
  after discovery of gossan area airborne survey
  discovered sharp magnetic anomaly, reconnaissance
  sampling
• 1985 Reconnaissance program established
  promising areas of gold mineralization
• 1986-1987 Six drill holes high-grade interval
  intersected (1.2 opt Au over 2.1 metres)
• 1988 Rock sampling program and six short drill
  holes by Keylock Resources and Catear Resources
  the best ddh intersection - 0.442 opt Au over 3.1
  m
• 1990 Mapping, sampling, trenching program
  considerable contents of Au, Ag and Cu discovered
  in the Camp Zone area
• 1991 Discovery of the porphyry-type Au-Cu target
  in the northern part of the area
• 1992 Five ddhs drilled by Teuton Resources
  bulk tonnage Au-Cu mineralization intersected in
  the northern part of the Tennyson claims ddh
  TN92-3 0.35 g/t Au and .33 Cu over 99.06 m
  (hole stopped in mineralization)
• 2006 Airborne TEM survey by Aeroquest Ltd.

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ROCK SAMPLES

• 1.678 opt Au 1985 sampling program (Groves,
  1986)
• 2.625 opt Au 1986 sampling program (Logan,
  1986)
• 14.95 opt Ag 1988 program (Keylock/Catear)
• 3.601 opt Au and 3.09 Cu 1990 program
  (Keylock/Catear)

DIAMOND DRILL HOLES

• 1.20 opt Au and 8.29 opt Ag over 2.1 m (ddh
  TN86-4 Camp Zone)
• 0.347 g/t Au and 0.330 Cu over 99.06 m (ddh
  TN92-03 North Porphyry Target)
• 0.09 opt Au and 0.88 opt Ag over 1.5 m (ddh
  TN86-02 Skarn Target) same hole A
  garnet-epidote-magnetite pyrite-chalcopyrite
  skarn was intersected between 99.7 and 109.7 m.
  (J.M. Logan, 1986). Copper was not assayed!

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2006 Airborne TEM Survey
Tennyson and Tenn Claims
Property Boundary
Strongly diversified MAG image reveals the
dominant NNW-SSE structural fabric and responds
to variable alteration patterns. High MAG anomaly
in the south part of the Tennyson claims overlaps
the skarn-type target discovered earlier in
course of ground work. A series of broad
conductors revealed in the NW part of the
Tennyson claims.
Tennyson original claims
Structural grain
LCP
Ground MAG anomaly of the Skarn Target
(coincident with 2006 airborne MAG) was drilled
in 1986 A garnet-epidote-magnetite
pyrite-chalcopyrite skarn was intersected between
99.7 and 109.7 m. (J.M. Logan, 1986) Copper was
not assayed!
MAG Anomaly (Skarn Target)
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1992 Drilling Results

• North Porphyry Au-Cu Zone
• discovered in 1990 zone of porphyry-type
  mineralization unknown extent
• 3 diamond drill holes intersected porphyry style
  gold mineralization from surface to depths up to
  100 m
• ddh TN92-01 0.277 g/t Au and 0.337 Cu over
  92.97 m
• ddh TN92-02 0.375 g/t Au and 0.316 Cu over
  63.09 m
• ddh TN92-03 0.347 g/t Au and 0.330 Cu over
  99.06 m

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Conclusion

• Underexplored multi-target property with
  diversified portfolio of mineral showings
• High potential for bulk tonnage Au-Cu porphyry
  type deposit
• Attractive and convenient location inside
  prominent and recently very active mineral belt

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Contact Us
Website www.teuton.com Investor Relations
Gary Assaly Telephone [phone]
Toll Free 1-800-879-2333 Fax
604-682-3992 Email gary.teuton_at_shawlin
k.ca Mailing Address 207-675 West
Hastings Street Vancouver, BC V6B 1N2