rpt on additional heavy mineral sampling black river - Geology Ontario

31C14SW2006 2 .20926 GRIMSTHORPE
010
t?
N.T.S. 31C/11
REPORT ON
ADDITIONAL HEAVY MINERAL SAMPLING
ON THE BLACK RIVER PROPERTY
GRIMSTHORPE TOWNSHIP, ONTARIO
Prepared By: Robert J. Dillman
8901 Reily Drive
Mount Brydges, Ontario
Feb. 18,2001

I. INTRODUCTION
Scope
Location and Access
Claim Logistics and Ownership
Survey Dates and Personnel
Physiography
Previous Work
Regional Geology
Property Geology and Mineralization
Gold Mineralization
Regional Kimberlite Occurrences
II. SURVEY PROCEDURE AND RESULTS
Analytical Procedure
'Kimberlite' Indicator Minerals
Results of Survey
Gold
Pyrite
'Kimberlite' Indicator Minerals
Chromite
Garnet
Chrome Clinopyroxene
Chrome Amphibole
Tourmaline
Zircon
Discussion of Results
Gold
'Kimberlite' Indicator Minerals
INDEX
III. CONCLUSIONS AND RECOMMENDATIONS
REFERENCES
AUTHORS CERTIFICATE
APPENDIX
Microprobe Results
Compilation Map
Page
1
111
1
6
6
7
7
10
11
11
11
11
14
14
14
14
14
18
18
18
18
23
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u
K
H
to
O
o
Ol
to
to
o
to to
n
5)
io id "0
n
O
H
O
0
FIGURES
Figure 1.
Figure 2.
Figure 3.
Figure 4.
Figure 5.
Figure 6.
Figure 7.
Figure 8.
Figure 9.
Figure 10.
Figure 11.
Figure 12.
TABLES
Table 1.
Table 2.
Table 3.
Location Map
Location Map
Claim Map
Regional Geology
Property Geology
Regional Kimberlite Occurrences
Chromite Plot
Chromite Plot
Eclogite Garnet Plot
Eclogite Garnet Plot
Eclogite Garnet Plot
Chrome Diopside Plot
Claim Logistics
Procedure of Heavy Mineral Processing
Heavy Mineral Sample Results
2
3
4
8
9
12
16
17
18
29
20
22
5
13
15

REPORT ON
ADDITIONAL HEAVY MINERAL SAMPLING
BLACK RIVER PROPERTY
GRIMSTHORPE TOWNSHIP, ONTARIO
l. INTRODUCTION
Scope
This report summarizes a follow-up program of heavy mineral prospecting for
kimberlite indicator minerals, diamond and gold on the Black River Property in Grimsthorpe
Township, Ontario. The program was generated in response to the detection of 'zinc-rich'
chromite grains in two heavy mineral concentrates collected on the property during the initial
1999-2000 heavy mineral survey. Similar Zn-chromite are an important indicator mineral of
diamond-bearing lamprophyre in the Wawa region of Ontario.
Results of this survey are compiled on a 1:2,500 scale map included with this report.
Location and Access
The Black River Property is situated in the central region of Grimsthorpe Township in
the Southern Ontario Mining Division (Figure 1.).
There is good road access to the property (Figure 2). Starting at the town of Gilmour,
located on Highway 62 north on Madoc, access can be made by traveling northeast on the
paved Wadsworth Lake Road for a distance of 4.7 kilometres to the intersection with the
Scootamatta Lake Access Road. Traveling south, the intersection of the Lingham Lake
Access Road is located 1.2 kilometres past the hydro transmission line. The Lingham Lake
Road crosses the property 1.3 kilometres south of the intersection.
The property is covered by 1:50,000 scale topographic map 31C/11.
Claim Logistics and Ownership
The Black River Property encompasses six units by three contiguous unpatented
mining claims (Figure 3). Table 1 summarizes the property.
The four claims comprising the Black River Property are equally owned by Robert
Dillman of Mount Brydges, Ontario and Jim Chard of Cordova Mines, Ontario.
Survey Dates and Personnel
Heavy mineral samples were collected on the Black River Property between
November 20, 2000 and November 21, 2000. Seven samples were collected on the property
during this time. Three additional samples were collected outside the property boundary.
Page 1 of 24

O 100 200 300 400km
i i i i i
FIGUKK
PROPERTY LOCATION

4
LAKE
ONTARIO
3* Mflt* FIGURE 1
LOCATION MAP

BLACK RIVER PROPERTY
GRIMSTHORPE TWP., ONTARIO
PLAN No. M97

TABLE 1.
CLAIM LOGISTICS
BLACK RIVER PROPERTY
GRIMSTHORPE TWP., ONTARIO
CLAIM
No.
1076804
LOCATION
Lot's 21 A 22, Concession XVI South 1A
No. of
UNITS
2 units
Recording
DATES
March 8, 1996
1076805
Lot's 19 A 20, Concession XV North 1A
2 units
March 8, 1996
1076806
Lot 18, Concession XV
2 units
March 8, 1996
6 units
Total Area: 120 hectares
Claim Ownership:
R. Dillman
8901 Reily Drive
Mount Brydges, Ontario
J. Chard
RR#1
Havelock, Ontario

Initial concentration of the eight samples was preformed between November 23, 2000
and November 24, 2000 by Jim Chard at his facilities in Marmora, Ontario. Removal of the
magnetic minerals and refinement of each heavy mineral concentrate was preformed by the
author at Mount Brydges, Ontario between December 1, 2000 and December 2, 2000.
Petrologic examination by the author was accomplished between December 3, 2000 to
January 17, 2001. 33 hours were devoted towards searching 245 grams of heavy mineral
concentrate for kimberlite indicator minerals and related minerals.
Physiography
The Black River Property is crosscut by a chain of interconnecting north-northwest
trending streams and ponds, the largest of which is the Black River. Drainage of the Black
River and feeder streams is variable, ranging poor to good as it is controlled by elevation
changes and some damming by beavers.
The property is characterized by moderate topography with up to 15 0Xo bedrock
exposure. Maximum relief is approximately 25 metres. Greatest elevation changes occur
east of the Black River where a significant outcrop ridge runs parallel to the river. West of
the river, regions are characterized by gently rolling ridges also orientated parallel to the
river.
Most of the property is covered by mixed hardwood forest. Maple, birch and poplar
are the dominant tree types, with minor balsam, fir, hemlock, cedar and isolated stands of
white pine.
Overburden consists primarily of ground moraine deposits of unconsolidated till
material occurring as a thin to moderate cover over most of the property. Till was deposited
in the Pleistocene by an ice sheet moving essentially north to south during an event
associated with the Wisconsin Glaciation. These deposits are primarily gravelly to sandy
loam with numerous locally derived pebbles and boulders. Glacial outwash deposits have
accumulated north of the property. These deposits consist of well-sorted fine to coarse
sandy deposits and coarse sand to cobble deposits showing excellent bedding. Recent
deposits of coarse material have accumulated along the Black River flood plain.
Previous Work
Grimsthorpe Township was mapped by V. B. Meen of the Ontario Department of
Mines in the 1940's (Meen, 1942). The area was mapped by R. M. Easton of the Ontario
Geological Survey in 1990 (Easton and Ford, 1990). Prior to 1991, there is no record of any
mineral exploration in this area of Grimsthorpe Township.
In 1991, R. Dillman prospected and staked claims along the Black River to cover
several gold discoveries. Following staking, geological and geophysical surveys consisting
of magnetometer and VLF-electromagnetic surveys were preformed over portions of the
property.
Page 6 of 24

In 1992, after a property examination by Homestake Minerals, several claims were
staked extending the property towards the north along the Black River. Soil sampling,
trenching and additional geological and geophysical surveys were preformed throughout the
year. Increased attention lead to additional gold discoveries by several exploration
companies and local prospectors and prompted the staking of claims adjoining the northwest
corner of the Black River Property.
In 1993, additional trenching and soil sampling was preformed by Dillman on the
property. Trenching was also preformed in 1996.
In the fall of 1999, four claims forming the south extension of the property were
abandoned. This was a result of changes to land-use policies and the formation of the
Lingham Lake Conservation area which buffered part of the claim block.
In the fall 2000, Dillman and Chard collected ten heavy mineral concentrates from the
property, the survey resulted in the detection of Zn-chromite similar to those found in the
Wawa region. Chrome clinopyroxene and Ca-Mg almandine garnet were also identified by
the survey. Prospecting during the program lead to the discovery of gold with arsenopyrite
in sugary quartz boulders lodged in the bank of the Black River. At present, no follow-up
work has been conducted to establish the extent of gold mineralization.
Regional Geology
The property is situated in the Madoc-Bancroft region of the Grenville Structural
Province of the Precambrian Shield. Rock units belong to the Mid-Sedimentary Belt of the
Elzevir Terrain subdivision of the Grenville Province. The regional geology is summarized in
Figure 4.
The property is underlain by Proterozoic aged metasedimentary and mafic
metavolcanic rocks. The supracrustal rocks are locally intruded by mafic to felsic dykes, sills
and large batholiths. The northwest trending greenstone unit is bounded on the east by the
Elzevir Granite Batholith and to the west, by the Lingham Lake Complex, a large circular
differentiated plutonic mass which evolved from a magma gradually changing in composition
from mafic to felsite.
Property Geology and Mineralization
The geology of the property is summarized in Figure 5. The geology is characterized
by large massive fine-grained basaltic flows and schistose metasedimentary units which
generally strike in a northwest direction and dip moderately towards the southwest.
Metasedimentary rocks occur as units between 1-75 metres thick consisting of
interbedded fine-grained argillaceous, graphite and greywacke schist and rare coarsergrained
quartz pebble conglomerate. Finer-grained units commonly contain variable
amounts of pyrite, pyrrhotite and magnetite resulting in a rusty appearance on outcrop
surfaces. Preservation of original bedding has been observed in some units although the top
Page 7 of 24

QILMOUR GOLD MINE 6
Black R/
Property
7 LIMESTONE
Au Gold
6 GRANITE
Pb Lead
5 GABBRO
Ni Mckei
C*
4 MARBLE
3 METASEDIMENTARY SCHISTS
2 FELSITE TUFF
l MAFIC MET A VOLCANIC FLOWS
MRSZ
f —— f —— f
O l 2 km
Moim River Shear Zone
GEOLOGY
TUDOR-MADOC REGION

. t
GEOLOGY
(LACK RIVER PROERTY '^
Grimsthorpe Twp., Ontario
Mafic Dyke
Felsic Dyke
Gabbro
Metasedimentary
Schists
l Metavokanic Flows
Q.V. Quartz Vein
Gold Occurrence
r . Glacial Striation
W Chromite

of the units has not been determined. Metasedimentary units typically outcrop in recessive
areas such as along northwest trending lineaments and are most abundant on the property
along the Black River and in areas west of the river. Contacts with basaltic flows are
sometimes sheared and commonly contain areas of quartz veining, some of which contain
arsenopyrite and gold.
Fine-grained northwest trending felsic dykes and fine-grained east-west trending
mafic dykes have intruded the metavolcanic-metasedimentary contact along the river and in
rock units west of the river. The dykes range between 1-2 metres wide. The felsic dykes are
medium-grained and grey in color. Fine planar black mica and augend quartz 'eyes' occur
throughout the felsic dykes. Mafic dykes are aphanitic, black in color, blocky and well-jointed.
It is believed the mafic dykes are older than the felsic dykes.
A small, coarse-grained gabbro body has intruded the mafic-metasedimentary contact
in the vicinity of the river in the north area of the property. Although the contacts are not
exposed, the gabbro appears to be roughly circular in shape, measuring approximately 50
metres in diameter. A similar gabbroic sill occurs at the metavolcanic-metasedimentary
contact east of the river in the southeast region of the property.
No large fault structures are recognized on the property although pronounced
lineaments suggest faulting has occurred. At least two directions of lineaments are present,
of which, the most dominant are orientated northwest and coincide with the strike of rock
units on the property. Cross-cutting lineaments evident by interconnected swamps orientated
east-west suggest the presence of younger faulting. Evidence in the rocks of the existence
of younger fault structures are apparent by a well-defined set of joints having an E-W
orientation which cross-cut and off-set features such as: bedding plains, contacts and
schistosity
Local zones of shearing occur in metasedimentary rocks at the metavolcanic contact
following the river and marginal to several northwest trending felsic dykes. Some
recrystallization and chloritization of the metasedimentary rock is associated with the shear.
Zones of Fe-Mg carbonate alteration are rare but pervasive in outcrops marginal to the
gabbroic sill at the metavolcanic-metasedimentary contact in the southeast corner of the
property.
Gold Mineralization
Previous prospecting and geological traverses lead to the discovery of eight areas of
significant gold mineralization close to the metavolcanic-metasedimentary contact following
the Black River (Figure 5). The mineralization is part of a series of similar gold showings
which occur along the contact over a distance of 5 kilometres (Dillman, 1991).
Two styles of gold mineralization occur on the property. The most prolific gold
mineralization is found in narrow arsenopyrite-bearing quartz veins in sheared and
mineralized metasedimentary rock. The quartz is granular textured and ranges from white to
'smokey-blue' in color. Assays of this mineralization have ranged 1.0 to 4.5 grams per tonne
over widths of 0.5 metres and 56.8 g/t in selected samples.
Page 10 of 24

The second style of gold mineralization is associated with the gabbro sill in the
southeast corner of the property. At the Gopher Showing in lot 18, concession XV, gold has
been detected in pyrite and carbonated chlorite schist developed along the margins of a 1
metre wide quartz vein. The vein has developed in a tension fracture in a gabbroic sill
situated at the metavolcanic-metasedimentary contact. The vein extends perpendicular into
the gabbro for an unknown distance. Assays of samples taken on the margins of the vein
have ranged as high as 9.2 and 21.9 g/t over widths of 0.15 to 0.4 metres.
Kimberlite Occurrences
There are no known kimberlite occurrences on the property however, within the region
kimberlite does occur (Figure 6). The closest known bedrock occurrence of kimberlite
includes: dykes at Picton, Varty Lake, and in city of Ottawa. Several pieces of kimberlite
were found in the waste pile of the Addington Gold Mine located near Flinton. The pieces are
believed to have come from an unreported kimberlite found in the mine.
Rumors of diamonds in glacial drift have been reported from several areas within the
region. The most famous is the Peterborough diamond reported to have been found along
the old CN rail line between Marmora and Peterborough.
II. SURVEY PROCEDURE AND RESULTS
ANALYTICAL PROCEDURE
During the survey, seven heavy mineral samples were collected from the property.
Maps showing sample locations, microprobe results and certificates of grain analyses are
appended to this report.
Kimberlite Indicator Minerals
Heavy mineral concentrates were processed in two stages. Each step is presented in
Table 2.
In the field, gravel was screened through a 5.0 mm screen and approximately 10 kg of
material was collected for further concentration. Additional screening divided the 10 kg of
material into 2.0 mm and 1.0 mm size fractions. Heavy minerals in the 1.0 mm fraction were
concentrated by Jim Chard using a spiral separator. Magnetic minerals in concentrates from
the spiral concentrator were removed using a magnetic tray and stored for future reference.
The remaining 'non-magnetic' concentrate for each sample was refined to a specific gravity
of 3.0 by Robert Dillman using a density liquid: Lithium Metatungstate.
Heavy mineral concentrates were examined by the author using a binocular
microscope and 20x magnification.
Page 10 of 24

@ G iimour
Rumoreti Diamond Fin
Peterborough Diamond
Peterborough
Property
Kimberlite found in
Addington Gold Mine
Matty Lake
Kimberlite Dyke
TORONTO
x
LAKE
OUT A H 1C
Picton
Kimberlite Dyke
KIMBERLITE AND DIAMONDS
IN SOUTHEASTERN ONTARIO

TABLE 2.
STEPS TO PRODUCE
HEAVY MINERAL CONCENTRATE
10 Kg Gravel -5.0 mm size
l
^^ screen ing.
+2.0 mm concentrate yX
+1.0 mm concentrate -1.0 mm fraction
Microscope Examination
and Mineral Selection
spire! concentrator
-1.0 mm concentrate
Microprobe Analyses
and Interpretation
Removal of Magnetic Minerals
Density Liqiud: Lithium Metatungstate
specific gravity: +3.0
Microscope Examination
and Mineral Selection
Microprobe Analyses
and Interpretation
page li.

RESULTS OF THE SURVEY
Gold
Survey results and sample locations are summarized in Table 3.
A signal gold grain was recovered from sample GRIM-11. The sample was collected
in the Black River in claim 1076804, lot 20, concession XVI.
The gold grain is approximately 0.35 mm in diameter and roughly disk-shaped with
rusty pits on the surface. The morphology is best described as reshaped (Avril, 1999)
suggesting potentially significant migration from source has occurred.
Additional minerals in the concentrate which may have some association with local
gold mineralization include: pyrite, pyrite + quartz composite grains, fragments of euhedral
brown tourmaline crystals.
Pyrite
Traces of pyrite are present in all the samples found on the property. Pyrite is a
common constituent in the metasedimentary units crossing the property. Samples GRIM-11
and G-5 have above background quantities of pyrite suggesting samples were collected
close to bedrock sources.
In sample GRIM-11, some pyrite occurs in composite with quartz. Similar composite
mineralization was found in two samples collected up-stream from the GRIM-11 sample site.
Euhedral crystals of pyrite are present in sample G-5. A sample previously collected
along the same creek up-stream from the G-5 sample site did not have any pyrite indicating
a potential source close to the G-5 sample site. The location of the G-5 site is in the vicinity
to the gold occurrence known as the Gopher Showing.
'KIMBERLITE' INDICATOR MINERALS
Chromite
Sixteen grains of chromite were identified in samples G-3, G-4 and GRIMS-10. Based
on the amount of zinc and magnesium, microprobe analyses preformed on chromite grains
suggest two populations exist. The most dominate, zinc-bearing chromite, averages 1.99 -
4.1607o ZnO. Mg-chromite do not have ZnO, average >^0.0% MgO and have greater amounts
of chrome. Mg-chromite was only found in sample G-4.
The majority of chromite grains found in the three samples are well-preserved
octahedral shaped crystals. Well-preserved euhedral crystal are most prevalent in sample
G-4. The grain-shape preservation suggests an immediate source in the area.
Page 14 of 24

TABLE 3.
RESULTS OF HEAVY MINERAL SAMPLING
Sample
Number
Lot 4
Concession
Claim
Number
U.T.M
Coordinates
E N
Grid
Coordinate
Sample
Type
Sample
Weight
kg (-5.0 mm)
Microprobe
Results
(1.0-0.14 mm grain size)
Comments
G-1
20 XVI l
S.y2
Off
property
303680 4968100
Stream
Gravel
12.5
-
abundant clear green
amphibole. Black River
G-2
18 XV
s.y2
1076806
305125 4966600
24+90N,
0+80E
Stream
Gravel
13.7
1 Ca-Mg-almandine
G-3
18 XV
N.y2
1076805
304625 4967090
31+65N,
2+40E
Stream
Gravel
7.4
2 Zn-chromite,
1 with Cr-amphibole
inclusions.
1 Sub-chrome augite
poor sample site.
Clear zircons and
fragments of tourmaline
crystals in concentrate.
G-4
18 XV
N.y2
1076806
304980 4966695
25+65N,
0+70E
Stream
Gravel
11.7
11 Zn-chromite
2 Mg-chromite
25 m upstream from
GRIM-10. Octahedral
crystals of chromite.
G-5
18 XV
s.y2
1076806
305460 4966520
23+55N,
2+10E
Stream
Gravel
9..2
-
abundant euhedral
cubes of pyrite.
G-6
18 XV
N.y2
1076806
305000 4967405
27+OON,
H-60E
Stream
Gravel
10.2
~
G-7
20 XVI
s.y2
1076804
304195 4967405
35+90N,
3+25W
Stream
Gravel
10.8
-
GRIM-11
20 XVI
s.y2
1076804
304280 4967075
24+35N,
0+95E
Stream
Gravel
11.6
1 gold grain
abundant pyrite 8, qtz
pyrite composites,
tourmaline
G-8
20 XVII
s.y2
Off
property
304775 4967985
Glacial
Till
12.2
~
carbonated-rusty grains,
some pyrite.
G-9
19 XVII
S.Y2
Off
property
304945 4967980
Glacial
Till
10.9
-
abundant pyrite.
GRIM-10
18 XV
N.%
1076806
304990 4966690
25+40N,
0+80E
Stream
Gravel
1 Zn-chromite (-0.5
mm concentrate)
additional probe work on
-0.5 mm concentrate.

Feb-03-200! 02:?7pm From-Rl BARNETT GEOLOSICAL +5196521475 T-443 P.010/028 F-173
CHROMITE - R. DILLMAN
GRIMSTHORPE (Feb. 7, 2001)
70
60
d60
W
O40
"o o
O
l ' i ' i r i ' r
Diamond Inclusion
10
j '- ' l l --t-- l _l -l- -l l i t l
4 6 8 10 12 14 16 18 20
Wt ** MgO
RLB

9000
70.00
Cr2O3 60.00
GRIM-7
GRIM-10
G-3
40.00
30.00
20.00
0.00 2-00 10.00
4.00 6.00 8.00
12.00
Ti02
PLOT OF Cr2O3 VS TiO2 (after Fipke, 1995)
CHROMITE COMPOSITIONS OF
BLACK RIVER PROPERTY VS
WAWA DIAMOND-LAMPROPHYRE DIKES
(modified from SAGE, 2000)

Garnet
Spherical or pellet-shaped grains of pink and orange garnet are present in most of the
heavy mineral concentrates collected on the property and surrounding region. Previous
microprobe analyses has indicated some of the pellet-shaped garnets are calcium-rich
pyrope-almandine compositions equivalent to 'G5 1 garnets (Dawson, 1975) and potential
eclogitic garnet. Previous sampling identified 11 G5 garnet, averaging 1-5 grains in most of
the samples collected across the property.
During this survey, only one G5 garnet was identified after 33 garnet analyses. The
grain occurs in sample G-4. The grain is orange in colour, pellet-shaped and approximately
0.5 mm in diameter.
Chrome Clinopyroxene
18 bright-green minerals were selected from the concentrates as potential chrome
clinopyroxene. Most of the microprobe analyses determined the majority of 'green' minerals
in the concentrates to be amphibole and epidote (in much lesser quantities). 6 clinopyroxene
minerals were identified in the grains submitted for analyses. The composition of the
clinopyroxene range between augite to diopside, most with only minor amounts of chrome. A
single grain of sub-chromium augite was identified in sample G-3. The grain contains Q.66%
Cr2O3 and Q.91% Na2O and potentially plots on the low end of the trend displayed by
mantle-derived chrome diopside found in kimberlite. The composition coincides with a similar
sub-chrome augite grain in a till sample collected in the southwest corner of the property
during the previous sampling program.
Chrome Amphibole
Microprobe analyses found samples G-3 and G-4 to contain Zn-chromite with
inclusions of chrome-rich amphibole. The amphiboles are unique in composition, containing
in access of 1.307o Cr2O3, the chemistry possibly corresponds to chrome-rich actinolite or
hornblende.
Tourmaline
Two forms of tourmaline occur in the heavy mineral concentrates. Samples G-3 and
GRIM-11 contain fragments of euhedral crystals of brown tourmaline. This type of tourmaline
has been observed with quartz stringers in a small circular gabbroic intrusion crossed by the
river in lot 20, concession XVI.
Small pellet-shaped grains of dark brown or black tourmaline were identified in
samples: GRIM-10, G-2, G-3 and G-4. Pellet-shaped tourmaline is abundant in samples
GRIM-10 and G-4. The grains are very similar in appearance to pellet-shaped chromite and
were selected for microprobe analyses on this basis.
Page 18 of 24

Fab-03-2001 02:25pm Frcm-RL BARNETT GEOLOGICAL +519652U75 T-443 P.OOi F-178
GARNET - R. DILLMAN
GRIMSTHORPE (Feb. 7, 2001)
RUB
wt % CaO

FBO-C9-200! 02:26pm From-RL BARNETT GEOLOGICAL +5196S21475 T-443 P.005/029 F-178
CLINOPYROXENE ~ R. DILLMAN
GRIMSTHORPE (Fob. 7, 2001)
6.0
5.0
6
4.0
3.0
2.0
1.0
0.0
0.0 1.0 2.0 3.0 4.0 5.0 6.0
Wt **
o
RLB

Zircon
Clear-colourless, anhedral to subhedral crystals of zircon are noticeably present in
samples GRIM-10, G-3 and G-4. The zircons fluoresce yellow when tested by a sodium
(black) light. Zircon is reported from the majority of diatremes found world-wide (Fipke, C.E.).
Diatreme zircon tends to be pellet-shaped and purple or orange in colour.
DISCUSSION OF RESULTS
Gold
The shape of the gold grain found in sample GRIM-11 is similar to the shapes of gold
grains which have traveled some distance from source. Some potential exists the grain is
from a local source since several gold occurrences are located west of the river in the vicinity
to the GRIM-11 sample site. The gold occurrences are situated in metasedimentary units
which are also cut by the river. The gold grain potentially represents additional
mineralization along the metasedimentary horizon up-stream from the GRIM-11 sample site.
'Kimberlite' Indicator Minerals
The minerals described in this report are not by definition 'true' kimberlite indicator
minerals, however some over-lap does exist of certain trends and mineral plots. Of greatest
interest are the Zn-chromites found on the property since these grains have very unique
chemistries and are similar to Zn-chromite occurring in the diamond-bearing lamprophyre of
the Wawa region of Ontario. It is also interesting that based on Cr2O3-TiO2 plots, at least
one of these grains falls within the field exclusive to kimberlite and lamproite.
The well-preserved crystal shapes of the majority of chromite grains suggest sources
are close to the sample sites. It is probable that the Zn-chromites all come from the same
source. This can also be concluded from the chromite with inclusions of chrome-rich
amphibole detected at two different sample sites. The distribution of chromite on the property
points towards a potential source situated in the north half of lot 19, concession XV or XVI.
The sub-chrome augite found on the property are similar in composition to
clinopyroxene from basic intrusions such as peridotite. Chrome-augite of this composition
are found in the Montreal area and occur as megacrystic grains in many of the Montregion
type intrusions associated with the Ottawa-Bonnechere Graben structure. Similar
clinopyroxene are found in heavy mineral concentrates collected close to carbonatites in the
Kapuskasing region of the Kapuskasing Structural Zone. In sample G-4, at least one Craugite
was found with chromite suggesting there is an association at the source of the
minerals.
It is debatable if the G5 pyrope-almandine garnets are potential indicator minerals
since the grains are wide-spread, occurring in many of the heavy mineral concentrates
collected on the property. It is unfortunate a microprobe is needed to differentiate between
Page 23 of 24

potential indicator G5 garnets and garnets of a metamorphic origin. This problem also exists
with tourmaline and zircon.
IV. CONCLUSION AND RECOMMENDATIONS
The detection of one single gold grain may or may not be considered as a significant
anomaly. In terms of exploration, the grain is the first grain detected by heavy mineral
sampling. The location of the grain coincides with a metasedimentary unit which hosts most
of the gold occurrences on the property. The grain could be evidence of the potential of the
unit to host high-grade gold mineralization in its native form (something which is important in
the current depressed gold market). Additional prospecting and surficial exploration is
warranted on this basis.
The chrome-rich mineral assemblage found in several of the heavy mineral
concentrates are very unique and show a close overlap with assemblages from diamondbearing
lamprophyre in the Wawa region. Additional heavy mineral sampling and
prospecting are required to prove this. A ground magnetometer survey is warranted to aid in
defining potential source of the minerals.
A budget to complete the necessary surveys includes:
Prospecting 8* Heavy Mineral Sampling
S5500
Magnetometer Survey 10,000
Rock Analyses 1000
Heavy Mineral Concentrating: 10 samples 1700
Microprobe Analyses 1000
Reports 8. Maps 1500
Food, lodging S transportation 4500
Total S25,200
Respectfully submitted,
Robert J. Dillman
Geologist
B.Sc.
February 18, 2001
Page 24 of 24

REFERENCES
Christie, B.J., 1992. Report on Prospecting, Geological
Mapping, and Soil Sampling, Di liman Black River
Property, Grimsthorpe Township, Southern Ontario
Mining Division, Ontario. Unpublished internal
report for Homestake Canada Ltd.
Dawson, J.B., and Stephens, W.E. 1975. Statistcal Classification
of Garnets From Kimberlite and Associated Xenoliths,
Journal of Geology, vol.83, pp. 589-607
Diliman, R.J., 2000. Report on Rock and Heavy Mineral Sampling
on the Black River Property, Grimsthorpe Township,
Ontario. Assessment report.
Dillman, R.J., 1992. Report on Electromagnetic (VLF) and
Magnetic Surveys, Black River Property,
Grimsthorpe Township, Southern Ontario Mining
Division, Ontario. Report for the Ontario
Prospectors Assistance Program, file no. OP92-235
Dillman, R.J., 1991. Report on Prospecting, Grimsthorpe
Township, Hastings County, Ontario. Report for
the Ontario Prospectors Assistance Program, file
no. OP91-535
Easton, R.M., and Ford, F., 1990. Geology of the Grimsthorpe
Area. In Summary of Field Work and Other
Activities 1990, Ontario Geological Survey,
Miscellaneous Paper 151, p. 99-110.
Fipke, C.E., 1995. Significance of Chromite, Ilmenite,
G5 Mg-Almandine Garnet, Zircon and Tourmaline
in Heavy Mineral Detection of Diamond Bearing
Lamproite. In: Proceedings of the Fifth
Inernational Kimberlite Conference, Diamonds:
Characterization, Genesis and Exploration,
pages 366- 381.
Meen, V.B., 1942. Geology of the Grimsthorpe-Barrie Area;
Ontario Department of Mines, Vol. 51, pt. 4, p.
1-50 (with Map 51d: published 1944).
Moore, J.M., 1982. Stratigraphy and Tectonics of the
Grenville Orogen in Eastern Ontario; Abstract
Volume, 1982 Grenville Workshop, Friends of the
Grenville.
Geological Survey of Canada 1981, Aeromagnetic Map 97G,
Grimsthorpe Township, Mazinaw Lake Sheet.
Sage, R.P., 2000. "Sandor" Diamond Occurrence, O.G.S. Report

CERTIFICATE
I, ROBERT JAMES DILLMAN, do hereby certify as follows:
[L]
I am a Mining Exploration Geologist and that I reside and carty on business
at 8901 Reily Drive, in the town of Mount Brydges, Ontario.
[2.] I am a Graduate of the University of Western Ontario, and hold a
Bachelor of Science Degree and majored in Geology.
[3.] I have been practicing my profession as a Geologist since 1 992.
[4.] I am a Licenced Prospector in Ontario and have been actively engaged as a
Professional Prospector since 1 978.
[5.] My report, dated February 18, 2001, titled: "REPORT ON ADDITIONAL
HEAVY MINERAL SAMPLING ON THE BLACK RIVER
PROPERTY GRIMSTHORPE TOWNSHIP, ONTARIO" is based on
information collected by myself between November 20, 2000 and February
18, 2001. Any other information which has been gathered from additional
sources has been cited in this report.
[6.] The information given in this report is as accurate as to the best of my
knowledge and I have not stated false information for personal gain.
[7.] I authorize the use of this report or any part of if proper credit is given to
the original author.
[8.] I have 50 0A interest in the property.
[9.] I am a member of the Geological Association of Canada.
ROBERT JAMES DILLMAN, B.Sc.
GEOLOGIST
Dated at Mount Brydges, Ontario
This 18 th day of February, 2001

fab-03-ZGOl a2:25pm From-Ri BARNET" GEOLOGICAL 45136521475 T-443 P.C02 P-IT8
GARNET - R. DILLMAN
GRIMSTHORPE - G-2 (Feb. 7, 2001)
234
wt %
CaO
o
RLB

ab-OS-2501 02:26pm Frcm-RL. BARNETT SECtOS l CAI +51B652U75 T-443 P 003
ECLOGITIC GARNET - R. DILLMAN
GRIMSTHORPE - G-2 (Fob. 7, 2001)
O
CM
CO
Z
#
*
0.18-
0.16"
0.14-
0.12
0.10-
0.06
0.06
0.04-
0.02-
0.00
C) 2 4 6 8 10 12 14 1
wt
CaO
RLB

02:26pm From-R t BARNETT GEOLOGICAL T-443 P.004/D29 F-179
o
p
4-
z.oo
1,40
1.20-
1,80-
1.60-
1.00-
0.80-
0.60
0.40-
0.20"
rt /*Nrt
ECLOGITIC GARNET
GRIMSTHORPE - G-2
O
R. DILLMAN
(Feb. 7, 2001)
10 12 14 16
wt
CaO
RLB

feb-Oa-2001 02:29pm Froiti-Ri BARNETT GEOLOGICAL +5I86521475 T-443 P.OID/329 F-173
ECL-PYROPC, R, OlLLHftN, GRIHSTHORPE, February 9, 2001, R,L.8.
SI02
TIC2
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C2G3
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CAC
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SI
Al
ftl
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i
39,05
.04
23.12
.08
25.70
9.65
2,12
.00
100.35
5.943
.060 i
4.084
.005
.010
J. 26V
.076
7.1S9
J4S
t
.000
t
4
*
l
(f
*
t
.000 9 ,977
24,900
F/N
*
1, 529
F/frt 605
; SWIPLi; G-2 GM1N

02:26pm From-R. BARNET GEOLOSICAl •f519S52l475 1-443 P 008/329 F-173
CLINOPYROXENE - R. DILLMAN
GRIMSTHORPE - G-2 (Feb. 7, 2001)
6.0
5.0
O* 4.0
**
o
3.0
* 2'0
1.0
0.0
0.0 1.0 2.0 9.0 4.0 5.0 6.0
wt **
o
RLB

"BC-G3-200! 02:27pm Ftcm-R. BARNETT CSEOIOSICAL +5IS6521475 T-443 P,007/329 F-IT3
CLINOPYROXENE -
GRIMSTHORPE - G-3
6.0
i——i——i
R. OILLMAN
(Feb. 7, 2001)
5.0
O 4.0 O*
#
1,0
0.0
0.0 1.0 2.0 9.0 4.0 5.0 6.0
w t ** Na tO
o
RLB

: ea-03-200i From-Rt BARNET" T-443 P.DOB/029 F-:?8
CLINOPYROXENE
GRIMSTHORPE - G-4
6.0
R. DIULMAN
(Feb. 7, 2001)
ow
6
5.0
4,0
3.0
2.0
1.0
0.0
0,0 1,0 2.0 3.0 4.0 6.0 6.0
wt
Na 2O
RLB

-eb-Co-ZCOl Ci:27pm From-Rl SAffNET" SEOlOulCAl +5I3652U75 T-443 P 009/329 F-i"6
CLINOPYROXENE - R. DILLMAN
GRIMSTHORPE - G~11 (Ftb. 7, 2001)
LO
5.0
O 4.0
M
O
3.0
2.0
1.0
0.0
0.0 1.0 2.0 3.0 4.0 5.0 6.0
wt
Na 2O
RLB

Fsb-03-200! 02:29pm Frcm-R. BARNETT SEOLOulCAL +513652M75 T-443 P.OIT/329 F-173
1
SIG2 54.70
TI02 .03
fl2D3 .64
020,' .00
FEO 2.38
H80 16.40
UNO
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CAO
K20
25.42
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NA20 .22
S'JP, 99.83
31 1.995
A l .005 2
RI .023
U . 001
en .000
ft .073
MG ,892
HN .001
Cfl .993
Nft .016
X .000 1
0 6.000
f If
F/Ftt
j
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t
it
t
t
t
f
t
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t
082
076
2
54. 12
02
81
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4, 37
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12
23. 80
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99. 72
1.994
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.135
.819
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6.000
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t
t
tz
*
2,011
t
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CLINOPYROXENE,
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14
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24. .60
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t
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R. 01LLMAK, SRIMSTKORPE, F*bruary 9, 2001, R,L,3,
4
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8, 67
12. 17
14
24. 37
02
43
99. 77
1.994
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6.000
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t
i
t
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\ SAMPLE S-2
2 SAMPLE 6-3
3 SAflPLE 6-4
a SAMPLE G-4
5 SftHPtE G-ll
li SfiNPLE G-ll
SKA IN
GRAIN
GRAIN
SBAIH
GRAIN
GRAIN
21
13
43
44
13
16

•'sb-03-20C1 02:27pm rrora-Ri. BARNETT 3EOL03ICAL +51965JU75 T-443 P.OIi/328 F-'79
CHROMITE - R. DILLMAN
GRIMSTHORPE - G-3 (Feb. 7, 2001)
70
60
o! 0
~~i ^ T "~
Diamond hidueion
#30
10
O 2 4 6 8 10 12 14 16 18 20
Wt 9b
MgO
o
RLB

"Bb-03-2001 02:28pm From-R;. BARNETT GEOLOGICAL +S13652U75 '1-443 P.01J/329 F-178
70
60
o! 0
6*0
CHROMITE - R. DILLMAN
GRIMSTHORPE - G-4 (Feb. 7, 2001)
i i i i ~r
Diemond inclusion Fi*id
#30
1O
2 4 6 8 10 12 14 16 18 20
wt ** MgO
o
RLB

Fab-C?!-2GCn 02:28pm Frcm-R, BARNETT 5EOL03!CAL +5I3B521475 l ~44i P .013/329 F-i?3
CHROMITE - R. DILLMAN
GRIMSTHORPE - GRIM 10 (Feb. 7, 2001)
70
60
o!0
6*0
l ' l
Diamond irciuelon
#30
*-*
3*20
10
.J____l l .j...... I.- ....i--..-L...... i l f l i l i l
4 6 8 10 12 14 16 18 20
wt *K MgO

"*b-03-200! 02-3CI|OT frcm-Rl BARNETT S T-443 P. 01 il/328 M 79
CHSOH1TE, 8. DIliltoN, GRJHSTHPfW, Fiomry 9, 2 )01, R,L.8
1
3102 .09
UK . 74
AX03 J i. 44
C203 42,54
FEC 35,86
m . 73
HSC .40
if HO J. 31
NIC .18
SUM 109,29
2
,00
.20
13.57
49.48
31.77
.51
4,17
.44
.C8
100.22
3
.11
.23
16,12
42.00
37.16
.78
.60
2.44
.oy
99.53
4
.08
.11
;4.4fc
42. li
37.53
.78
.46
3.13
.09
99.09
5
.07
.49
11,93
46,33
35.9.5
.90
.47
1.99
.11
100.22
b
.03
1 85
14.79
42.79
37.53
.57
.61
2.25
.08
100.50
.08
1.32
H. 77
41.82
37.87
.66
.56
2.20
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99.41
a
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2.0;
19,52
37,27
36.40
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3.36
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100. U
SI .025 *
11 ,15b *
At 5,409 *
Of: 9.391 *
fi 8 .J73 *
Mtl .173 *
MS .166 *
I'A . 682 *
N; .040 24.416
C 32.000 *
F7M 51.33?
f/m .981
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.041 *
4.339 *
10,738 *
7.29.3 *
.119 *
1.706 *
.039 *
.CIS 24.392
32,000 *
4.344
.313
,C.51 *
.049 *
5.561 *
9.J71 *
8.770 *
.186 *
.252 *
.508 *
.020 24,550
32.800 *
35,48?
.973
.023 *
.024 *
4,901 *
9.536 *
9,100 *
.190 *
.197 *
.665 *
021 24.706
32.000 *
4?, 106
.979
.020 *
.105 *
4.004 *
10. 882 *
8.'j58 s
.21? *
.200 *
.410 *
.025 24.429
32.000 *
43.961
.978
.008 '
.390 *
4,882 *
9.476 *
8.791 *
.135 *
,25S *
.465 *
.018 24.420
32.000 *
35.051
.972
.023 *
.282 *
4.944 *
9.392 *
8.996 *
.159 *
.237 *
.461 *
.030 24.524
32.000 t
38.612
.975
.014
.427
6.312
8.086
8.353
.123
.339
.631
t
t
*
*
t
4
.1
.024 24 .356
32.000 t
24. m
' 961
t
1 SAMPLE li-3 QWIli li
2 SflWE G-3 GRAIN
3 SfiWE G-4 GRAIN
4 SftNHi G-4 CRAIH
1 SAKPIE G-4 GRAIN
16, 1NCI CR-ANPH
4
S
6, INCI CR-fiHPH
6 SftMPU G-4 GRfilN 7
l SftRPlE S-4 CRA1H 9
8 SAMPLE G-4 GftAIH 10

Fdb-05-ZOOi 02:30pm From-RL BARNETT SEOLOSICAL •1-5)36521475 T-443 P.020/029 F-1T6
CHROMIC, S. DIUMAK, GRIMSTHflRPE, February 9, 2001, R.L.8.
9
SI 02 .O/1
TI02
. n
AiiC3 14,69
C2C3 4J,0?
FEO 37.68
HNC .63
MGC .52
ZNl 2.49
H10 .i!
SUtt 99.47
10
.04
.84
14.54
42.77
33.59
.60
,49
2. 62
.06
100.56
11
.04
^.67
12,3'.
45,00
J6.01
.60
.51
2. IS
.10
100,44
12
.07
.31
14.65
51.67
21.74
.34
10.94
.00
.16
99.88
13
.10
.23
19.81
42.42
3?. 60
.63
.89
3.59
.16
100.45
14
.05
.47
16.17
41.56
36.99
.61
.75
3.22
.20
100. Q2
15
.02
1.10
14.81
50.59
22.22
.30
It,l4
.00
.19
100.37
16
.07
.21
19.85
40.05
33.26
.81
.70
4.16
.07
99,18
S! ,020
.Oil *
TI .045
.178 *
Al 4,934 4 .840 *
CR 9.707 9 ,552 *
FE 8.982 9 .117 *
MN ,J52 * ,144 *
110 .221 * .206 *
IH .524 * .549 *
Ni .025 24.611 ,OS4 24.611
0 42.000 * 32
F/N U.345
F/FM .976
.000 *
44.663
.978
.017 '
.176 *
4.086 *
9.997 *
e. 462 *
.143 *
.214 *
.446 *
.023 24.163
32.000 *
40.285
.976
.018 *
.061 *
4.502 *
10.654 *
4.742 *
.075 *
4.2SJ *
.000 *
.034 24.339
32,000 *
:.U3
.531
.027 *
.047 *
6.341 *
9.110 *
7.406 t
.145 *
,J60 *
.72!) *
.039 24.196
32.000 *
20,954
.954
.014 *
.099 *
5.353 *
9.240 *
8.699 *
.145 *
.314 *
,669 *
.045 24.584
32.000 *
28,li4
.966
,005 *
.214 *
4.525 *
10.366 *
4.616 *
.066 *
4.303 *
.000 *
.040 24.333
32.000 *
1.134
.531
.019 *
.044 *
6,468 *
8.756 *
7.651 *
.190 *
.289 *
.849 *
.016 24.321
32,000 *
2?. 317
,965
9 SAMPLE G-4 GRAIN 12
10 SflilPLE G-4 GRAIN 14,
li SAMPLE S-4 GRAIN IS
12 SAMPLE G-4 GRAIN 17
15 SAHPLE G-4 GRAIN 18
14 SAHPli S-4 GRAIN 23
15 SAMPLE G-4 GRAIN 26
16 SAMPLE GRIH'IO GRAIN
INCL CR-ftHPN
17

fnb-08-2001 OZ:2Spm From-Ri BARNETT SEOtCSICAL +51866ZHT5 T-443 P.018/029 F-176
CR-AHPHI80LE, R. DUIMWI, SHIHSrHOSPf, February 9, 2001, R.L.6.
SI02
TI02
f(203
C20i
FEfi
(ISO
UNO
CAC
K2C
NA20
SUN
1
50,11
.14
6.46
1.72
3.56
20..60
.00
12,54
.07
1,70
97,12
2
45.50
Jo
:i,u
1.32
14.74
10.84
.09
11.61
,29
1.41
97.77
51
AL
Al
Tl
Cfi
fi
MG
MK
Cft
K
HA
0
7.067 *
.933 8.000
.174 *
.015
,m
'
*
.420 *
4,330 *
.000 5.131
1.898 *
.01J *
.465 2.375
23.000 *
FE 6.32
Cft 28.55
MG 65.14
F/H .097
F/FH .088
6.700 *
1.300 8.000
.715 *
.040 *
.154 *
1.815 *
2.3?9 *
.011 5,114
1.8J2 *
.054 *
.403 2.289
23.000 *
30.12
iO,40
39.48
.768
.434
1 SfiMfU G-3 fiRfllN 16, INCL Id CHRDM
2 SAMPLE G-4 GRAIN 6, INCL IN

c eb-03-2CO) 92:28pm -R^ BARNET" 3E0103ICAL T-443 P.OU/029 F-'TS
Mr. R. Dillmn, February 9, 2001
R. j. Diliman Geological Services,
8901 Rally Drive,
RK 5, Mount Brydges,
NOL 1WO
Pft/Fax 1-519-264-9278
R. L. Barnett Geological Consulting Inc.,
9684 Longwoods Road,
RR 32, London, Ontario.
N6P 1P2
Ph. 1-519-652-1498
Fax 1-519-652-1475
Dear Robert,
The identity of "non-indicator" minerals in the Grimstboxrpe
samples of February 7, 2001, for which analyse* were not
provided, is:
GRIM 10
0-2
groins 1,2,4,11,13-16,18,23,24,31-35 - simple ilmenite
grains 3,5,7,12,19,21,26,36,39 - tourmaline
grains 6,40 - Pfe-qpat
grain 8 - Mn-ilmenite
grains 9,27,37 - Ti-magnetite
grains 22,28,29,38,48 - amphibole
grain 20 - staurolite
grain 10 - magnetite
grain 25 - Fe-spinel
grain 30,46 - rutile
grains 41,45 - grossular-almandine 00
grain 42 - diopside
grain 43 groaaulax-andradite as
grain 44 - Ma-alnondine
grain 47 - sphene
grains 1,2,4,5,6,9,10,11,25 - tourmaline
grains 3,18 - anphitoole
grains 7,13 - almandine
grain 8 ~ airqple ilmenite
grains 12,16 - spessartine-almandine aa
grains 14,3.7 - grossular'almandine aa
grain 20 - K-spar
grain 22 - quartz
grain 23,24 ~ Fe-cpx
G-3 grains 1,2,4
grains 3,14
grain s
grain 6
grains 7,8
grains 9,11
grain* 10,12
tourmaline
almandine
simple ilmenite
Fe-qpx
epidote
spesaartine-aljiKuidine aa
grossular-almandine ss

OZ:ZBpm Frcm-Ru BARNET" 5EOLC3ICAL +513652UT6 "-443 f . 015/3:9 F-;73
G-4 grains 1,2,3,11,13,16,20,21,22 - tourmaline
grains 8,27-32,37,39 - groesular-alroandine ss
grains 33-36,36 - spfeaaartine-alitiandine aa
grains 40,41,42 - epidote
grain 24 - single ilmenite * Cl~sunphibole
O-5 grain l - rutile
grain 2 - tourmaXine
grains 3,5,6,7 - aiirple ilmenite
grain 8 - groosular-aUroandine as
grain 4 - Ti-magnetite
3-11 grains 1-5,8,9,10 - groooular-almandine aa
grains 6,7,12 - apeaaartine-almandine sa
grain 11 - groaaular-andradite aa
grains 14,15 - Fe-cpx
grain 17 ~ sphene
Sincerely,
R. L, Barnett

Ontario
and Mines
Mining Act, Subsection 65(2) and 66(3), R.S.0.1990
Declaration of Assessment Work
Performed on Mining Land
Transaction Number (office use)
. 00008
Assessment Files Research Imaging
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31C14SW2006 2 .20926 GRIMSTHORPE
Instructions: - f-or worK perrormea on ^rown Lanus oeiure recording a claim, use form 0240.
- Please type or print in ink.
On o
* **t \j ^
Name
ROBERT J. DILLMAN
Client Number 125989
Address
8901 REILY DRIVE
Telephone Number
(519)264-9278
MOUNT BRYDGES, ONTARIO NOL 1WO
Name
Address
Fax Number
Client Number
Telephone Number
Fax Number
(519)264-9278
2. Type of work performed: Check K) and report on only ONE of the following groups for this declaration.
rj' Geotechnical: prospecting, surveys, n Physical: drilling stripping,
" assays and work under section 18 (regs) " trpnrhinn ann accnHatori s
trenching and associated assays
D
Rehabilitation
Work Type
HEAVY MINERAL SURVEY
Office Use
Commodity
Oates Work From 20 NOVEMBER 2000 TO 17 JANUARY 2001
Performed Day | Month | Year Day | Month | Year
J
Total S Value of ^ ^
Work Claimed H OH o .
NTS Reference
Global Positioning System Data (if available)
Township/Area GRIMSTHORPE TOWNSHIP
MorG-PlanNumber M97
Htoci v di^
MAR 0 \ 2001
Mining Division Q /\ (T\
Resident Geologist —-—
GEOSCIENCE ASSESSMENT
J. OFFICE

LxJO/90. 0666g
Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;
- provide proper notice to surface rights holders before starting work;
- complete and attach a Statement of Costs, form 0212;
- provide a map showing contiguous mining lands that are linked for assigning work;
- include two copies of your technical report.
3. Pereon or companies who prepared the technical report (Attach a list if necessary)
Name
ROBERT J. D l LIMAN
Telephone Number
(519) 264-9278
Address 8901 REILY DRIVE , MOUNT BRYDGES, ONTARIO
Name
Address
Name
Address
NOL 1WO
Fax Number (519) 264-9278
Telephone Number
Fax Number
Telephone Number
Fax Number
4. Certification by Recorded Holder or Agent
l, ROBERT J. DILLMAN , do hereby certify that l have personal knowledge of the facts set forth in
(Print Name)
this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its
completion and, to the best of my knowledge, the annexed report is true.
s\
Signature of Recorded Holder or Agent jf}/)
U/^^^
Agent's Address 8901 REILY DRIVE, MOUNT feRVpGES, ONTARIO l
t^Ok luOQ
^Oleltprone Number (519) 264-9278
Date FEBRUARY 18, 2001
Fax Number (519) 264-9278
0241 (03/97)
RECEIVED
MAR U t :";
GEOSCIENCF ASSESSMENT
OfflCE______

Ontario
Ministry of
Norttiem Development
and Mines
Statement of Costs
for Assessment Credit
Transaction Number (office use)
UJQ/9Q.
Personal information collected on this form is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining
This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provin
Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.
Work Type
Units of work
Depending on the type of work, list the number of hours/ lays
worked, metres of drilling, kilometres of grid line, numbei
rf
samples, etc.
Cost Per Unit
of work
Total Cost
SAMPLE COLLECTION
2 DAYS
3225 PER DAY
3450
HEAVY MINERAL CONCENTRATING
7 SAMPLES
3165 PER SAMPLE * GST
31236
PETROLOGY
256 GRAMS
33 PER GRAM +GST
3822
REPORT
MICROPROBE ANALYSES
3 DAYS
5.5 HOURS
3275 +GST
3100 PER HOUR * GST
3883
3589
Associated Costs (e.g. supplies, mobilization and demobilization).
SAMPLE SHIPMENT
319
Transportation Costs
TRUCK
290 KM
30.35 PER KM
3102
Food and Lodging Costs
Total Value of Assessment Work
34,098
2. 2
RECEIVED
MAR u i;::;
GEOSCIENCF ASSESSMENT
j__ OFFiC?
r-.-- . .. ,,-T,,-,- -u,---—
.,_y.^,."... ^asmft^^m^^t^am
M -
IT-

Calculations of Filing Discounts:
1. Work filed within two years of performance is claimed at 1000Xo of the above Total Value of Assessment Work.
2. If work is filed after two years and up to five years after performance, it can only be claimed at 500Xo of the Total
Value of Assessment Work. If this situation applies to your claims, use the calculation below:
TOTAL VALUE OF ASSESSMENT WORK x 0.50 = Total S value of worked claimed.
Note:
- Work older than 5 years is not eligible for credit.
- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a
request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the
Minister may reject all or part of the assessment work submitted.
Certification verifying costs:
l, ROBERT J. DILLMAN. ,, do hereby certify, that the amounts shown are as accurate as may reasonably
(please print full name)
be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying
Declaration of Work form as RECORDED HOLDER l am authorized to make this certification.
(recorded holder, agent, or state company position with signing authority)
0212 (03/97)
Date
FEB. 18, 2001
RECEIVED
MAR O 1 2001
GEOSCIENCE ASSESSMENT
_____OFFICE

Ontario
ROBERT J. DILLMAN 125989
GRIMSTHORPE TWP. M-97
Ministry of
Northern Development
and Mines
Schedule for Declaration of
Assessment Work on Mining Land
Transaction Number (office use)
Mining Claim Number. Or if
work was done on other eligible
mining land, show in this column
the location number indicated
on the claim map.
Number of Claim
Units. For other
mining land, list
hectares.
Value of work
performed on this
claim or other
mining land.
Value of work
applied to this
claim.
Value of work
assigned to other
mining claims.
Bank. Value of work
to be distributed
at a future date.
1076804
2
1171
800
214
157
1076805
2
586
800
1076806
2
2341
800
1541
Column Totals
K098 32,400 3214 31,698
0290 (02/96)
RECEIVED
MAR o i --j
SEOSCIENCF ASSESSMENT
______OFFICE

Ministry of
Ministers du
Northern Development
Developpement du Nord
and Mines et des Mines Ontario
Geoscience Assessment Office
933 Ramsey Lake Road
April 3, 2001
6th Floor
Sudbury, Ontario
ROBERT JAMES DILLMAN
P3E 6B5
8901 REILY DRIVE
R R #5 Telephone: (888) 415-9845
MT BRYDGES, Ontario Fax: (877)670-1555
NOL-1WO
Visit our website at:
www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm
Dear Sir or Madam: Submission Number: 2.20926
Subject: Transaction Number(s):
Status
W0190.00008 Approval
We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The
attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS
SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.
If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any
steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the
Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day
Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment
Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in
Section #6 of the Declaration of Assessment work form.
Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the
response date on the summary.
If you have any questions regarding this correspondence, please contact LUCILLE JEROME by e-mail at
lucille.jerome@ndm.gov.on.ca or by telephone at (705) 670-5858.
Yours sincerely,
ORIGINAL SIGNED BY
Lucille Jerome
Acting Supervisor, Geoscience Assessment Office
Mining Lands Section
Correspondence ID: 15824
Copy for: Assessment Library

Work Report Assessment Results
Submission Number: 2 .20926
Date Correspondence Sent: April 03, 2001
AssessorLUCILLE JEROME
Transaction
Number
First Claim
Number
Township(s) l Area(s)
Status
Approval Date
W0190.00008 1076804
GRIMSTHORPE
Approval
April 02, 2001
Section:
17 Assays ASSAY
Correspondence to:
Resident Geologist
Tweed, ON
Recorded Holder(s) and/or Agent(s):
ROBERT JAMES DILLMAN
MT BRYDGES, Ontario
Assessment Files Library
Sudbury, ON
Page: 1
Correspondence ID: 15824

4 IN 4ON ^9N 38N 37N
i
36N
35N
34N
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33N 32N 3IN 30N 28N
l
27N
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26N
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25N 24N 23N
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22N 2IN 2 ON
cr-w
GRIMSTHORPE TWP., PLAN N". M97
'Gopher Showing
21^ grt Au/0.15 m
9.2 g/t An/0.4 m
G-3 2 Zn-chromite
1 Sub-chrome augite
0.09g7tAu
GRIM-l
2 Ca-Mg edogtte almandine '
GWM-2
l Ca-Mg eclogite almandine
W9S2 0.M * A. -^i./ ^*9Si O.OJgrtAu
TL-1 *30.02 g/t Ao, -0.02 gft Pt, O.02 g/t Pd
S
GRJM-10
2 Zn-chromite
1 Ca-Mg almandine
L2-3.2 art Aa
G-2 1 Ca-Mg almandine
56.8 g/t Aa
4.6 gAt An/0.55 m
G RIM-11 1 gold grain 03 g/t AB/ 1.0 oi
16953 23,9 g/t Au
16954 0.87 g/t Au G-4 11 Zn-chromite
2 Mg-chromite
GREtt-8
5 Ca-Mg edogite almandine
-if GEND-
5
4
3
2
l
Mafic Dyke
Felsic Dyke
Gabbro
Metasedimentaiy Schists
Metavolcanic Flows
V\AA. shear zone
trench
magnetic anomaly
magnetic anomaly + VLF EM conductor
float
M/,
Indicator Mineral
glacial striation
swamp
Barren Sample Location
GRIM-7
l Ca-Mg eclogite almandine
l Chromite (KIM?)
GREtf-4
l Ca-Mg eclogite almandine
l Cr Diopside
31C14SW2006 2.20926 GRIMSTHORPE 200
LOCATION OF GOLD AND POSSIBLE
KIMBERUTE INDICATOR MINERALS
COMPILATION MAP
BLACK RIVER PROPERTY,
GRIMSTHORPE TWP, ONTARIO
SCALE 1:25,000
DRAWN BY: RJD
revised; Feb 16, 2001
DATE:
FEBRUARY
2000

MINING LAND TENURE
MAP
\v'j\fvV.-)T^A^is^7
I *, - \fjt' "^J*\ ' . \ ^S7\,.^:'^±
AND TENURE WITH D RAW ALI
f ; ^ l
i MPOBTANf N OTICI
^A:3m
as-A^i
31CHSW2006 2.20926 GRIMSTHORPE
210