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St Andrew Updates Stock and Nixon Fork Advanced Exploration Projects and Other Exploration Programs.


OAKVILLE, Ontario Oakville (2006 population 165,613[2]) is a town on Lake Ontario in southern Ontario, Canada, midway between Toronto (about 31 km or 19 mi away) on its eastern border and Hamilton (about 20 km or 12 mi away) from its western border.  -- St Andrew Goldfields n. 1. A small slender woolly annual (Lasthenia chrysostoma) with very narrow opposite leaves and branches bearing solitary golden-yellow flower heads; it grows from Southwestern Oregon to Baja California and Arizona; - it is often cultivated.  Ltd. (TSX TSX Toronto Stock Exchange (TSE before April, 2002)
TSX Transfer from Stack Pointer to Index
TSX True Space Extension
:SAS (1) (SAS Institute Inc., Cary, NC, www.sas.com) A software company that specializes in data warehousing and decision support software based on the SAS System. Founded in 1976, SAS is one of the world's largest privately held software companies. See SAS System. ) ("St Andrew") is pleased to provide an update of activities at its Stock Gold Complex, Timmins, Ontario This article is about city in Ontario, Canada. For other uses, see Timmins (disambiguation).
Timmins, with a population of 42,997 (2006), is a city in northeastern Ontario, Canada on the Mattagami River. At 2,961.
, and its Nixon Fork, Alaska and Eskay Creek, British Columbia British Columbia, province (2001 pop. 3,907,738), 366,255 sq mi (948,600 sq km), including 6,976 sq mi (18,068 sq km) of water surface, W Canada. Geography
 properties.

Stock Gold Complex

The Clavos Advanced Exploration Program at the Stock Gold Complex is expected to be completed at the end of the fourth quarter of 2005 and the level of the understanding, delineation and evaluation of the Clavos mineralization Mineralization
The process by which the body uses minerals to build bone structure.

Mentioned in: Rickets

mineralization,
n the bioprecipitation of an inorganic substance.
 are such that management believes that the requisite planning and layouts designed to achieve sustainable production can be made to accommodate the structure and nature of the delineated Clavos mineralization.

To date approximately 20,000 tonnes of underground rock have been treated through the Stock Gold Mill, recovering approximately 5,000 ounces of gold.

A total of over 35,000 metres of underground diamond drilling Diamond Drilling is a highly specialized industry used for mineral exploration around the world. Most commonly using wireline and core bits with diamond encrusted matrix. To drill holes to max depths of twelve thousand feet, for the recovery of core used in verifying mineral   have been carried out to define the deposit and to delineate additional resource ounces.

Underground development of over 3,750 metres has been carried out on the 100 metre, 150 metre, 175 metre, 200 metre, 225 metre and 250 metre levels to confirm the continuity and structure of the Clavos mineralization.

The Clavos Decline has been extended a further 275 metres on the incline to a depth of approximately 315 metres below surface. Additional horizontal development has been carried out on the 175 metre, 225 metre and 250 metre levels to provide underground drill access to further delineate the Clavos mineralization at lower elevations.

The 10 kilometre haul road from the Clavos mine to the Stock Gold mill has been completed and is now in daily use to haul rock from Clavos. The overhead power line from the Stock Mine to Clavos is complete and the necessary underground reticulation reticulation /re·tic·u·la·tion/ (re-tik?u-la´shun) the formation or presence of a network.

reticulation

the formation or presence of a network.
 is in place to support the anticipated production levels.

Stock Gold Mill

Satisfactory metallurgical recoveries have been achieved from the underground rock from the Clavos Project (20,000 tonnes). Throughput rates have been in line with designed capacities of 75 tonnes per hour.

Taylor Advanced Exploration Project

The excavation of the box cut for the Taylor Decline and the establishment of the surface infrastructure at the Taylor Advanced Exploration Project have commenced. The decline excavation is planned to commence in the first quarter 2006.

Timmins Exploration Program

Planning is being finalized for a major winter 2006 exploration surface program to test at least 15 targets with over 20,000 metres of surface drilling. During the Spring and Summer of 2005 Geoinformatics Exploration Inc. and St Andrew completed a major upgrade of the St Andrew Timmins 3D geological databases and models, including the integration and input of major data sets collected by the Discover Abitibi Project. These data sets included airborne gravity and magnetics covering the St Andrew exploration areas. A total of 51 exploration targets were delineated and 15 priority targets were chosen for drill testing.

Nixon Fork Mine

In late October, 2005 the Nixon Fork Plan of Operations, Environmental Assessment and draft Solid Waste Disposal Permits, the key permits required for commercial production, were posted for public comment by the State of Alaska and Bureau of Land Management. This public comment period ran for 30 days. St Andrew understands that the regulators are currently evaluating the comments received, resolving any issues raised and finalizing the permit documents. St Andrew anticipates that the regulators will issue in the near future the necessary permits for Nixon Fork to commence operations.

Subject to the receipt of these permits, it is anticipated that Nixon Fork will commence operations in the mid-2006.

During the Summer 2005 Exploration Program several new exploration areas were explored with interesting intersections that will require follow-up in future programs.

An underground winter 2006 diamond drilling program is planned at the Mystery Creek deposit. This program is intended to delineate and confirm additional ore zones that will provide feed for the Nixon Fork operations.

Eskay Creek

A total of 8 targets were tested with 11 diamond drill holes for a total of 2,096 metres of diamond drilling.

Two targets, namely Polo and Harrymel Creek, returned positive evidence of new mineralization within the St Andrew Eskay Creek land position. The Polo target indicated potential massive sulphides (same as the Eskay Creek Mine) and the Harrymel Creek target indicated a copper-zinc-silver skarn skarn

In geology, a metamorphic zone developed in the contact area around igneous rock intrusions when carbonate sedimentary rocks are invaded by and replaced with chemical elements that originate from the igneous rock mass nearby.
.

A follow-up exploration program is planned for next summer 2006.
2005 Eskay Drill Program Drill Hole Coordinates
-----------------------------------------------

--------------------------------------------------------------------
Owner          Hole       Target   Depth     UTM      UTM   Az.  Dip
                                      (m)   East    North
--------------------------------------------------------------------
Heritage   TN-05-01   Tarn North   275.6  414881  6272993  100   -50
--------------------------------------------------------------------
Heritage   TV-05-34           TV   197.7  409450  6265671  180   -50
--------------------------------------------------------------------
Heritage-
 Teuton    BW-05-01   Bonsai West  235.6  403730  6276277  121   -57
--------------------------------------------------------------------
Heritage   KN-05-01   King North   192.6  403265  6274645   90   -75
--------------------------------------------------------------------
Heritage   HC-05-01     Harrymel
                           Creek   191.7  403625  6267990  290   -59
--------------------------------------------------------------------
Heritage   PO-05-01         Polo   236.5  409547  6271491  250   -70
--------------------------------------------------------------------
Heritage    AF05-01        Aftom   182.9  412437  6276231 78.5   -68
--------------------------------------------------------------------
Heritage   PO-05-02         Polo   168.7  409539  6271492  118   -54
--------------------------------------------------------------------
Heritage-
 Teuton     BW05-02  Bonsai West   152.4  403665  6276144  119   -59
--------------------------------------------------------------------
Heritage-
 Teuton     BZ05-01       Bonsai   151.5  404895  6276482  224   -49
--------------------------------------------------------------------
Heritage-
 Teuton     BZ05-02       Bonsai   111.1  404895  6276482  224   -80
--------------------------------------------------------------------



Highlights

Polo Target

Two drill holes tested the Polo target on the east side of the McKay anticline anticline: see fold. , beneath the Bowser Bowser may mean:
  • Bowser, British Columbia, an unincorporated community on Vancouver Island
  • Bowser and Blue
  • Bowser and Blitz from C.O.P.S.
  • Bowser (Nintendo), the main villain in the Mario series of video games.
 basin cover rocks. The first drill hole, PO-05-01, was drilled to the southwest to a depth of 236.53 metres. The drill hole intersected Bowser sediments to a depth of 47 metres, and intercalated in·ter·ca·lat·ed
adj.
Inserted between two others; interposed.



in·terca·late
 pyritic py·rite  
n.
A brass-colored mineral, FeS2, occurring widely and used as an iron ore and in producing sulfur dioxide for sulfuric acid. Also called fool's gold, iron pyrites.
 mudstone mud·stone  
n.
A fine-grained, dark gray sedimentary rock, formed from silt and clay and similar to shale but without laminations.



mudstone  
 and amygdaloidal a·myg·da·loid  
n.
A volcanic rock containing many amygdules.

adj. also a·myg·da·loi·dal
1. Shaped like an almond.

2. Anatomy Of or relating to the amygdala.

3.
  basalt basalt (bəsôlt`, băs`ôlt), fine-grained rock of volcanic origin, dark gray, dark green, brown, reddish, or black in color. Basalt is an igneous rock, i.e., one that has congealed from a molten state.  to 144 metres. Strong pyrite pyrite (pī`rīt) or iron pyrites (pīrī`tēz, pə–, pī`rīts), pale brass-yellow mineral, the bisulfide of iron, FeS2.  stringer and disseminated mineralization hosted by Salmon River Salmon River

River, central Idaho, U.S. It flows northeast past the town of Salmon, where it is joined by the Lemhi River, and then northwest to join the Snake River south of the Idaho-Oregon-Washington border. It is about 420 mi (676 km) long.
 basalt was found at the hole bottom. Massive pyrite was intersected from 164.70 metres to 167 metres.

Although no gold values were intersected, the drill hole demonstrates that massive sulphide exhalite mineralization is found within this Polo target. The lowest part of the mudstone above is anomalous in mercury.

A second drill hole, PO-05-02, was collared from the same setup and drilled to 168.70 metres in an east orientation. The hole intersected mudstone to 45 metres and encountered mafic flows with disseminated pyrite to 58 metres. The remainder of the hole intersected sheared sheared  
adj.
Shaped or finished by shearing, especially cut or trimmed to a uniform length: a sheared fur coat.

Adj. 1.
 mudstone and mafic rocks.

Harrymel Creek

Base metal and silver returns were obtained from a drill hole (HC-05-01) west of Harrymel Creek. Results are as follows:
-------------------------------------------------------------------
BHID      From     To    Width      Cu     Pb     Zn     Ag     Au
            (m)    (m)      (m)   (ppm)  (ppm)  (ppm)  (ppm)  (ppb)
-------------------------------------------------------------------
HC-05-01    47     48        1     294   1945   2205   15.4      1
-------------------------------------------------------------------
HC-05-01    54     56        2      54     32    173   11.9      2
-------------------------------------------------------------------
HC-05-01   118    121        3     541    629   1220    1.9      1
-------------------------------------------------------------------
HC-05-01   132    135        3    1307      6    135    1.2      1
-------------------------------------------------------------------



The silver, lead and zinc anomalous intercepts from 47- 48 metres and from 54 - 56 metres are hosted by graphitic argillite ar·gil·lite  
n.
A metamorphic rock, intermediate between shale and slate, that does not possess true slaty cleavage.



[Latin argilla, argil; see argil + -ite1.
. Base metal anomalous mineralization in HC-05-01 from 118 - 121 metres and from 132 - 135 metres is in a chlorite- diopside diopside

Common silicate mineral in the pyroxene family. Diopside is a calcium and magnesium silicate (CaMgSi2O6) that occurs in metamorphosed siliceous limestones and dolomites, in skarns, and in igneous rocks.
 skarn with 5-10% pyrrhotite pyrrhotite (pĭr`ətīt) or magnetic pyrites, bronze-yellow to bronze-red mineral, a sulfide of iron sometimes containing nickel. It tarnishes easily and is somewhat magnetic. .

The drill hole indicates that skarn mineralization is a possible target west of Harrymel Creek.

A limited surface sampling program was completed to check geophysical anomaly locations and to assess conceptual targets west of the SIBS zone. A sericite Ser´i`cite

n. 1. (Min.) A kind of muscovite occuring in silky scales having a fibrous structure. It is characteristic of sericite schist.
 altered structure 30-40 metres wide was found approximately 600 metres south west of the SIBS area.

A grab sample taken on a magnetic high approximately 1.3 km northwest of the Harrymel hole had copper values of 6940 ppm, silver of 5ppm and gold of 112 ppb.

Teuton Bonsai Joint Venture

Four holes in the program were completed on the Teuton Bonsai JV ground totaling 650.6 metres. The drilling tested the Bonsai West geophysical anomaly with two holes, and the Bonsai prospect with two holes. None of the holes intersected significant gold mineralization.

Qualified Persons

St Andrew's Timmins exploration programs are being carried out under the supervision of St Andrew's Timmins Exploration Manager, Mr. Wayne Reid, P.Geo. Mr. Reid is a qualified person (as defined by National Instrument 43-101) with more than 30 years of experience in the mining industry.

The Heritage exploration programs are being carried out under the supervision of Mr. Gerry Bidwell, P.Geol. and Mr. Warren Bates Bates   , Katherine Lee 1859-1929.

American educator and writer best known for her poem "America the Beautiful," written in 1893 and revised in 1904 and 1911.
, P.Geo. Messrs. Bidwell and Bates are both qualified persons (as defined by National Instrument 43-101).

The Nixon Fork exploration programs are being carried out under the supervision of St Andrew's Alaska Exploration Manager, Mr. William Burnett. Mr. Burnett meets the qualified person requirements (as defined by National Instrument 43-101) with more than 10 years of experience in the mining industry.

Shares Outstanding - 618 million.

St Andrew Goldfields Ltd. (TSX:SAS)
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Geographic Code:1CANA
Date:Dec 12, 2005
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