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42A06NE0096 2 .12378 WHITNEY 010
Magnetic and VLF-EM Surveyon
The Lithium Corporation of Canadain
Whitney Township, Ontario
date: April 3, 1989
RECEIVED
APR l 'i 1989
MIMING LANDS SECTION
by: E. H. van Hees, M.Se., Consulting Geologist
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42Ae6NE0896 2.12378 WHITNEY 010C
TABLE OF CONTENTS
IntroductionLocation * AccessFigure 1 - Project LocationFigure 2 - Property Claim MapTopographyRegional GeologyFigure 3 - Local GeologyFigure 4 - Stratigraphic Nomenclature and
Correlation for the Timmins Area
Property GeologyHistory of ExplorationRecent Geophysical SurveysResults of the Geophysical SurveysConclusionsRecommendati onsCertificateAppendix
Page
1234569
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11121314161716
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l l l INTRODUCTION
l In early January of 1989, E. H. van Hees Geological Services Inc.,
was contracted by Lithium Corporation of Canada Limited to
l conduct an exploration program consisting of a Total Field
m Magnetic Survey and a VLF-EM Survey on a block of claims located
in east-central Whitney Township, Timmins, Ontario. A new grid,
l with lines every 100.0 metres and stations every 25.0 metres, was
cut at right angles to the baseline having an azimuth of 450 .
l Both surveys have readings every 12.5 metres along the lines.
The surveys were conducted in late January, 1989, and
February, 1989, with the claims covered by the west central part
l of the grid being completed first, in order to meet assessment
requirements before the end of January.
g This report decribes the method and results of the program.
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LOCATION AND ACCESS
m The property is located in the east-central part of Whitney
Township, in the city of Timmins, Porcupine Mining Division,
l Cochrane District, Northeastern Ontario. The block is comprised
of twenty-one (21) contiguous staked claims, covering parts of
m Lots 1, 2, and 3 in Concession IV, and parts of the south half of
M Lots 2 and 3 in Concession III (see Schedule of Claims, Appendix
A and Figure 2).
l The city centre of Timmins is approximately 19.0 km (11.8
miles) due west of the property, and the town of Porcupine is
l approximately 6.5 km (4 miles) west-north-west.
m Access to the property is good. A paved, all weather
highway (101) is followed for approximately 2.0 km (1.2 miles)
l east from Porcupine. Here a dirt road leads south for
approximately 0.5 km (0.3 miles) from the highway to a fork. The
l east fork is then followed for approximately 1.9 km (1.2 miles)
m east to a dammed creek which lies on the west boundary of the
south western claim block.
l The dirt road is generally not open in the winter, but it
was plowed to the creek for the duration of the survey. A four-
| wheel drive vehicle is required for the last 1.9 km (1.2 miles)
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in both winter and summer (See Figures 1 and 2).
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Figure l. Project Location
Figure 2 Property Claim Map
f1034559 f 1034560
Scole l"8|750'
l WW90
——!—l 1034556 l (034557 l l
1036302
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TOPOGRAPHY
l The claim group is generally of low relief with no major
changes in elevation. The ground is largely swampy with some dry
l areas. Goose Creek traverses portions of the western boundary
claims and the northeast corner of the claim block.
Vegetation is mixed, varying from alders and spruce in the
wet areas to spruce, pine and poplar with some birch in the drier
areas,
l No outcroppings of rock were noted on the property during
the survey.
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REGIONAL GEOLOGY
m The Porcupine Gold Camp is currently one of the largest gold
producing regions in Canada, and many of the camp's most
l important past and presently producing mines are located in the
immediate vicinity of Whitney Township. In particular, the
l Pamour #1 Mine and the Hallnor Mine (past producer) are within 5
I km (3.1 miles) of the Whitney Property.
The rocks of the camp are of Precambrian age (2.6-2.7
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billion years with minor middle Precambrian intrusives and
sediments (D.R. Pyke, 1982). Stratigraphically, these are
divided into the Deloro Group and the Tisdale Group (the Whitney
claim block is located within the Deloro Group). The Porcupine-
Destor Fault which strikes east-north-east through the camp
separates the Tisdale Group to the north from the Deloro Group to
the south.
The Deloro Group is believed by Pyke to be the older of the
two groups (1982). He describes it as being comprised of three
(3) main volcanic formations, the Lower, the Middle and the
Upper, for a total estimated thickness of 5000 metres.
According to Pyke, the Lower Volcanic Formation consists of
"... *i1 nor ultramafic volcanic rocks, maximum thickness 800 m , i r* engulfed
In a massive to weakly foliated diorite which forms the Marginal phase of a
large bathoiithic complex." This unit extends only into the
southwest corner of the Timmins area.
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The Middle Volcanic Formation is estimated to be about 3000
l metres and makes up the bulk of the group. The formation is
m comprised almost entirely of calc-alkaline basalt and andesite
with minor pyroclastics near the top. The majority of ultramafic
l intrusive rocks are also within this formation.
The Upper Volcanic Formation is between 2000 metres and 3000
l metres thick. Intercalated oxide and sulphide iron formations
are abundant with the calc-alkalic felsic pyroclastics dominating
the formation.
l The Whitney property is underlain by the middle and upper
Deloro Group volcanic units. (See Table 1).
l The Porcupine-Destore Fault strikes east-north-east through
j the central portion of Whitney Township approximately 2.6 km (1.6
miles) north of the property. Other faults within the vicinity
l of the property include a series of west-north-westerly striking
faults concordant to and situated between the Montreal River
l Fault, approximately 8.7 km (5.4 miles) to the southwest, and the
M Cross Lake Fault approximately 12.9 km (8 miles) due east of the
property. Of particular significance to the property is one of
l these west-north-west faults which bisects the property and
continues for a possible strike length of 40 km (25 miles) to the
l north (Timmins-Kirkland Lake Map #2205). Pyke (1982), further
H indicates two faults traversing the property, rather than one,
both with general north-south strikes. One is located along the
l property's western boundary (along Goose Creek), and the other is
located along the property's eastern boundary. Both appear to be
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sinistral. The western fault is most likely associated with the
l Pamour Number 1 Mine, approximately 3.0 km (1.9 miles) northwest
m of the property, where it is known as the shaft fault.
To the south of the Porcupine-Destor Fault, the dominating
l structure is the Shaw Dome (D.R. Pyke, 1982). Pyke (1982),
describes this fold structure as being "... elongated in a nortnweet-
eoutheaet direction and measures approximately 1 9 b y 29 km." The Whitney
property is located near the northeast margin of the dome where
stratigraphy would normally have steep north dips. However, the
superimposed Whitney Anticline, which strikes northeast with its
l axis just to the south of the property, gives a relatively flat
dip to the north.
l Figure 3 illustrates the General Geology of the Timmins
area.
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Figure ? Geology of tho claim group
Fig. 4 STRATIGRAPHIC NCMENCIATORE AND CORELATICN FOR THE TIMMINS AREA
This Report
3 sets of dikes
Algcman granites
ALgonan porphyry
sub volcanic 4- intrusives
Upper
Porcupine
Formation
Lower Porcupine Fm.
Krist Fontation
argillite
Gold Centre
Vipond
Central
Northern 4-
Boomerang Fm.
Redstone Fm.
Donut lake Fm. 4-
Pyke 1976
3 SetS Of HiTcPc;
Algotan granites
Algonan porphyry
sub volcanic 4- intrusives
Upper
Porcupine
Formation
Lower Porcupine Fm.
Upper Tisdale
Formation
Middle
Tisdale
Formation
Lower Tisdale Fm. 4-
Boonerang Fm.
Redstone Fm.
Donut Lake Fm. 4-
Ferguson 1968
2 sets of dikes
Algoman granites
Algerian porphyry
Haileyburian
6 greywacke/ slate 3 quartzite
4 greywacke, slate 3 qtzite, congl. 2 greywacke, slate 1 conglomerate
metasediments
Latite Breccia
argillite
Gold Centre
Vipond
Central
Northern
Deloro
Group
Dunbar 1948
Algcman granites
Algcman porphyry
Haileyburian
Timiskaming
sediments
Hoyle Group
Keewatin
(Tisdale
Keewatin
(Deloro)
Burrows 1924
Algcman granites
* Algcmanporphyry
Haileyburian
Timiskaming
sediments
* Rhyolite and
jtz fi dspr porphyry
not mapped
Keewatin
Greenstones
The Rocks
diabase dikes
granitic batholiths
quartz-feldspar porphyry
Diorite dikes and sills
slate, greywacke conglomerate
tuff, slate, gwky
acid pyroclastics
argillite
Tisdale
meta-volcanics
(Porcupine
Syncline)
Deloro
meta-volcanics
(Shaw Done)
X. SS9U
Intrusive RocksN.
P "O
133500 metres
1000 M
1300 metres
75 M
4300
metres
3000 -
5000
metresMapped as the same, + related
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PROPERTY GEOLOGY
l Rock exposure is non-existent on the property and
m i nterpretation concerning the underlying geology must be inferred
from the geology in the surrounding area, geophysics and some
l diamond drilling carried out in the past..
D. R. Pyke's 1982 report covers the majority of the property.
l The map accompanying his report discerns from geophysics that the
m underlying rocks are felsic, calc-alkalic metavolcanics. These
observations combined with geological mapping nearby, indicates
l that the stratigraphy strikes northeast with moderately flat dips
of 30 to 50 degrees to the north. According to Pyke, geophysics
l has also discerned two moderately wide iron formations, both
m striking northeast. One of these is located in the southwest
corner of the property and the other just south. Both are
l truncated and apparently sinistrally displaced, approximately 1.2
km (0.75 miles) along Goose Creek, by a north-south striking
l fault along the western edge of the property.
H Rock outcroppings, northwest of the property, delineate a
granodiorite intrusive that strikes northeastly to near the
l northwest corner of the property (see Figure 3), where it is
truncated by a north-south striking fault. As with the iron
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formations, this unit is most likely sinistrally displaced which
would put its eastern extension on the Whitney property.
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HISTORY OF EXPLORATION
An airborne electromagnetic survey conducted by Canadian
Aero Mineral Surveys in 1969 for Oro Mines Ltd. (not on file) is
the earliest mentioned exploration program covering the southwest
l portion of the current Whitney property. Interpreted results
from this survey delineated several conductors, the majority of
which were believed to be associated with iron formations. The
causes of some complex conductors located in the central part of
the property were not determined,
l In 1977 a second airborne electromagnetic survey was flown
over a total of sixty-one (61) claims, including the twenty-one
l (21) claims comprising the Whitney property. The survey was
m conducted in 1977 by Dighem Ltd. for Cominco Ltd. in joint
venture with Rosario Resources. Conductors delineated in the
l 1969 survey were confirmed and a number of others discovered. The
majority of these have northeast trends, with some being
l considered as caused by overburden and cultural. Iron formations
m were again interpreted as causing most of the anomalies.
Diamond drilling was carried out on the property in 1974 by
Summit Gold Mines Inc. Three holes having a total length of 1209
feet were drilled on the current claims number 996889.996890,and
1034555. This drilling encountered various sediments including
siltstone, argi11ite.and chert as well as massive and tuffaceous
dacite. Lamprophyre dikes were also encountered as were massive
pyrite units, and pyrite or pyrrhotite breccia's.
Most recently (1988), the government completed an airborne
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geophysical survey of some 64 townships in the Timmins area
l including Whitney. A Z-shaped magnetic and VLF anomaly was
identified on the Lithium claim block as in previous programs.
l RECENT GEOPHYSICAL SURVEYS
Geophysical surveys consisting of blanket total field
l magnetic and two channels of VLF electomagnetic surveys were
completed between late January and the end of February, 1989. The
surveying was completed on a new winter cut grid which had 100
l metre spaced grid lines cut at right angles to the 45 degree
azimuth baseline. Stations were picketed every 25 metres but
l read every 12.5 metres on all these surveys. The length of the
various lines was determined by the location of the claim
boundaries which were recut using lot and concession lines in
l this surveyed township. A total of 40 kilometres of grid were
cut and surveyed on the claims. Approximately 3200 stations were
l read during the survey for a density of 152.4 readings per claim
M for each survey.
The total field magnetic and VLF electromagnetic surveys
l were completed using the Scintrex IGS-2 system in conjunction
with a cycling base station to correct for diurnal drift in the
l magnetic survey. Instrument specifications are provided in
g Appendix A of this report. Data was collected by Mr. R. Arbic of
Timmins, Ontario. Problems with the surveying caused by the
l frequent shutdown of the VLF stations in Cutler and Annapolis
resulted in every line in the survey being walked at least twice
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and sometimes three times.
B The magnetic and VLF data was processed using the internal
B computer of the Scintrex IGS-2 system, as well as a Zenith AT 386
computer using the UDL program for plotting and contouring of the
l data. A Houston Instrument DMP-56 plotter was used to make the
plots of the data.
RESULTS OF THE GEOPHYSICAL SURVEYS
M T he magnetic survey results include several anomalies both
positive and negative (see maps in back pocket). Three distinct
l positive anomalies are present on the property. These extend
from 1+00 south on line 19+00 west to the baseline on line 4+00
l west; from 9+00 south on line 2+00 east, and westward from 2+00
m north on lines 2+00 to 10+00 west. Several other small positive
magnetic areas are present on the property in the vicinity of
l station 9+00 south on line 3+00 east, station 3+00 north on line
11+00 west and station 2+00 north on line 14+00 west. Negative
l anomalies lie parallel to and north of the magnetic high near the
m base line in several places. A magnetic low also occurs from
station 1+00 south on line 14+00 east to station 8+00 south on
l line 2+00 east.
The magnetic high near the baseline is for the most part
l very narrow and has a steep magnetic relief. At the eastern end
m of this anomaly, the width increases significantly and a small
hook appears to be present which trends 240 degrees. This hook
l as well as the increase in width suggests that the there is a
fold in the anomaly and that the small magnetic high anomaly
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on line 11+00 west may be part of the same anomaly. All the
" features present suggest that this is an iron formation like
B those known to occur in the top of the Deloro Group of volcanics.
This iron formation could be comprised of magnetite or of a
l combination of pyrite and pyrrhotite like that encountered by the
Summit Gold drilling in 1974. From the profile of the magnetic
high it appears that the anomalous unit is nearly vertical at the
B western end and developes a flat dip to the south at the east
end. The hook portion of the anomaly would appear to be vertical
B in attitude.
The cause of the small magnetic anomaly on line 14+00 west
l is uncertain but it again could be part of the iron formation
B suggested for the previously discussed anomaly. The magnetic low
anomalies that lie parallel to and north of the large magnetic
l high appear to be the normal lows related to the magnetic high.
The magnetic high located on the northwest corner of the
B eastern claim block appears to be very extensive and this
m suggests that there is a change in the lithology of the area or a
major change in the overburden depth. Within the area there is a
l small magnetic high between 3+00 and 7+00 east at 3+00 north.
This may be a deeply buried iron formation of magnetite or
l sulphide composition. The anomaly appears to be caused by a
m vertical to steeply south dipping source.
The three small, low intensity, spot highs located around
l station 8+00 south on line 3+00 east may represent fragments of
more magnetic material caught up in the fault which appears to be
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causing the long, north trending, magnetic low on this part of
the property.
The VLF-EM survey results are of minimal use as there appear
to be very few anomalies (see maps in back pocket). Those that
l do exist, as defined by fraser filter results, appear to be very
small and correlate with the large magnetic high located near the
baseline on the western grid. This lack of VLF anomalies, in an
area where there are anomalies probably caused by iron formation,
may be due to the presence of a thick cover of conductive clay
l overburden as well as the orientation of the conductors relative
to the transmiting stations.
m CONCLUSIONS
The Lithium Corporation Company of Canada property in the
l east central part of Whitney Township is a property underlain by
the upper units of the Deloro Group of Volcanics. This group of
l volcanics has intercalated iron formations which are evident on
m the property as a series of magnetic anomalies. These anomalies
appear to have lenghts that vary from 500 to 1400 metres and
l widths that are generally narrow. The Iron Formations have steep
dips for the most part except where there are folds in the Iron
Formation. Here the dips are significantly flatter and may be as
low as 45 degrees to the south.
The results of the VLF-EM survey are poor at best with very
little definition of any anomalies except for a small area that
correlates with the largest magnetic anomaly. The poor strength
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of the VLF anomalies is probably due to the depth of conductive
clay overburden and the orientation of the conductors relative to
the transmiting station.l l RECOMMENDATIONS
Based on the results of the magnetic and VLF-EM program,
B definition of the various anomalies by a MaxMin survey is
M recommended in order to better define the nature of the anomaly.
Upon compilation of the results of the geophysical programs, a
l reverse circulation or diamond drilling program should be
considered to test the various anomalies for gold. This work
l should be completed as soon as possible in order to assess the
m value of the property before Ducks Unlimited carry out much more
work in the area.
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CERTIFICATE
I, Edmond H. van Hees, do hereby certify:
j 1) that I am a consulting geologist and reside at 165
Tamarack St., Timmins, Ontario,
l 2) that I am a graduate of the University of Waterloo, 1975,
with the degree Honours Bachelor of Science (Earth
m Science).
m 3 ) that I am a graduate of the University of Western Ontario,
1979, with the degree of Master of Science (Geology).
I 4) that I have practised my profession full time since 1977
and part time since 1972.
l 5) that I am a fellow of the Geological Association of
m Canada.
6) that I do not have, nor do I expect to receive, directly
l or indirectly, any interest in the properties or
securities of The Lithium Corporation of Canada,
l 7) that this report is based on a personal knowledge of the
j property gained through a review of all published
geological data on the area as well as that stored in the
l MNDM files at 60 Wilson Street in Timmins, a number of
visits to the property, supervision of the work in this
l report and ten years of exploration experience in the
Timmins area.
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Timmins, Ontario Edmond H. van Hees M. Se.,s ' ' ' ' -.
March 28, 1989. Consulting
APPENDIX A
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t)8.0 SPECIFICATIONS
8.1 Magnetometry Specifications
Total Field Operating lange
Gradient Tolerance For Total Field:
Total Field Absolute Accuracy
Resolution
Tuning
leading Time
Continuous Cycle Times
Operating Temperature Range
8.2 Sensor Options
In the following options the actualhowever, mountings and cables vary.
Portable Total FieldSensor Option
-
20,000 to 100,000 nT(1 nT - 1 gamma).
5000 nT/m.
*1 nT at 50,000 nT 2 nT over total fieldoperating and temperature range.
0.1 nT.
Fully solid-state. Manual orautomatic node Is keyboardselectable.
2 seconds. For portablereadings this is the time taken from the push of abutton to the display of themeasured value.
Keyboard selectable in 1second increments upwards from2 seconds to 999 seconds.
-AO'C to *50*C providedoptional Display Heater is used below -20*C.
i
sensors are identical;
Includes sensor, staff, two2 m cables and backpack sensorharness. Weight of sensor, cable and staff is 1.9 kg.
HP: 8-1
lllllllllllllllllll
Staff Is 30 x 600 am collapsed and 1600 m extended.
Base Station Sensor Option Includes sensor, tripod, 50 B cable external power cable and analog chart recorder cable. Weight of sensor, cable and tripod Is 6.5 kg. Tripod Is 540 SOB collapsed, 1650 son extended.
Cradioaeter Sensor Option For use with the Portable Total Field Sensor Option, includes second sensor, cables and both a .Sot and a IB staff extender. Combined weight of Total Field and Gradiometer Sensor options with staff, extender and cables is 3.5 kg.
HP: 6-2
9.0 SPECIFICATIONS - VLF
Frequency Tuning Automatic digital tuning. Can be tuned to any frequency in the range 15.0 to 29.0 kHz with a bandwidth of 150 Hz. Up to three frequencies can be chosen by keyboard entry for sequential measurements.
Held Strength lange Fields as low as 100 nA/m can be received. In practice, background noise may require fields up to 5-10 times this level. Maximum received field is 2 mA/metre. These values are specified for 20 kHz. For any other frequency, calculate the above limits by multiply ing by the station frequency in kHz and dividing by 20.
Signal Filtering Narrow bandpass, low pass and harp cut-off high pass filters.
Measuring Time 0.5 seconds sample interval. As many as 2 16 samples can be stacked to improve measurement accuracy.
VLF-Magnetic Field Component* Measured
1) Horizontal amplitude, 2) vertical in-phase component, and 3) vertical quadrature components. Vertical components are displayed as a percentage of horizontal component and are related in phase to the horizontal component. Their range is 120Z; reading resolution IX.
VLF-Magnetic Field Sensor Two air-cored colls In a backpack mounted housing with an electronic level for automatic tilt compensation. The error in the vertical in-phase component is less than IX for tilts up to *15*.
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VLF-Klectric Field Dipole Two electrodes with integral preamplifiers and 5 m of cable. Probe input impedance exceeds 100 megaohos and capacitance is less than l picofarad*
VLF-Electric Field Componenti Measured
In-phase and quadrature components of the horizontal electric field phase related to the horizontal VLF-magnetic field. These components are not recorded but are used in the calculations of resistivity and phase. The reading resolution is l ohmoeter.
Apparent leslstivity Calculation
H
where:P - apparent resistivity in
ohmoeters Ex * horizontal electric
amplitude, calculated. Ex - (EX(I)2 * EX(Q)2)* By - horizontal magnetic
amplitude, measured f * VLF station frequency in
HertzM0 - permeability of the
ground in Henries/meter, a constant
The resistivity calculation has a range of l to 100,000 ohmoeters with a resolution of l ohmmeter.
Phase Angle Calculation The phase angle 4 is expressed as:
E,(Q)- arc tan
where:Ex(Q) * horizontal quadrature
VLF electric field,measured
VLF: 9-2
li4 4 i| 4t li li
EX(I) - horizontal in-phase VLF electric field, measured
The phase angle calculation has a range of -180* to 4-180* with a resolution of l*. By definition the angle is positive when the E field leads the H field.
4ft ft ft ftft ftftfth
VLPs 9-3
l l l l l— Appendix B
* Magnetic Data
l for
The Lithium Property
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UTHMAG.XYZ Thursday, March 9, 1989 3:06 prn Page 1
1
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T:" :
f:::..
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f--
\'•."
*1fi: ;teif*'"-i '
mtt"l;|t"!*JflfIpi ::i-It ;1
i
mf*:fir"
i
Total FieldLINE *
0.000.000.00
0.000.000.000.000.000.00
0.000.000.00
0.000.000.000.000.000.00
0.00LINE *
100.00100.00100.00100.00100.00100.00100.00100.00100.00100.00100.00100. OO100.00100.00100.00100.00100.00100.00100.00
100.00100.00100.00100.00100.00
; 100.00100.00100.00100. OO100.00
r 100.00100.00
; i: 100.00100.00
and Gradient MagneticsSTATION--75.00
-62 . 50-50.00
-37,50-25.00-12.5012.5025.0037 . 50
50.0062.5075 . 00
87 . 50100.00
112.50
. 125.00
137.50
1 50 . 00
160.00STATION-550.00-537 . 50-525 . 00-512.50
-500.00-487.50-475,00-462.50-450.00-437.50-425 . 00-412.50-400.00-387 . 50-375.00-362 . 50-350.00-337.50-325.00
-312.50-300.00-287.50
-275.00262,50-250.00-237., 50-225.00-212.50
-200.00-187.50- 1 75 . 00-162,50-150.00
TOTAL58674 . 2
58658 . 2
5S658 . 5
58656.158653.858652.058638.758634 . 2
58629.3
58618.058617.658626 . 4
58632 . ]58622.7
58621 .958626 . 358624 . 258636 . 0
58S35 . 6TOTAL
58801 . 758800 . 058799.2
58798 . 058803.6.5880? . 458799 . 758795 . 358791 . 558788 . 658787.658786.258778.9
58777 . 556:776.6.
58780.258784 . 75879.1 . 155:790.0
58789,058792 . 258796.558799 . 4
58797 . 858798.958793 , 75S791 .858X93.956=791 .658 707 . 858784 . 158783 , 85577*3.2
GRADIENT- 9999 . 0-9999.0
-9999 . 0
-9999.0-9999.0- 9999 . 0-9999.0-..999.:) . Q
-9999 . 0
-9999.0-9999.0-9999 . 0-9999.0-9999 . 0
-9999.0-9999.0-9999 . 0
-9999.0
-9999.0GRADIENT-9999 . 0-9999 . 0-9999.0-9999 . 0-,CJC3QC! Q
~ '^5*9'^ . 0
-9999.0-9999.0- 9999 . 0-9999.0-9999.0-9999 . 0
-9999 . 0-9999.0-9999 . 0-9999 . 0-999-9.0
-9999 . 0-9999 . 0-9999,0-9999 .0-9999.0-9999.0-9999.0-9999 . 0-9999.0-9999 , Q-9999 . 0
-9999 . 0-9009,0
-9999 . 0- 9999 . 0-9999.0
l
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LITHMAG.XYZ Thursday, March 9 ;, 1989 3:06 pro Page 2
t- . 100.00
pr ' 100.00
p: ' 100.006; 100.00f:-" 100.00
f 100.00
fi 100.00P3 ' 100.00
t 100.00
E 100.00
E" 100.00
FT loo.ooRf'1 100.00t 100.00||\ 100.00
R1 "" loo.ooc : . 100.00p 100.00p" - 100.00B'' 100.00
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-137.50
-125.00
-112.50
- 100.00
-87 . 50- 75.00
-62.50
-50.00
-37.50
-25.00
-12.50
0.00
12.50
25 . 00
37.50
50.0062.5075 . 00
87.50
100.00
STATION
-1205.00
-] 200. 00
-1187,5*
-1175.00
-1162.50
-1150.00
-1137.50
-1125.00
-1112.50
-noo.oo-1087.50
-3075.OO
-1062.50
-1050.00
1037.50
-1025.00
-1012.5.0- 1 000 . OO
-987,50
-975.00
-S62 . 50
-950 . 00
-937 , 50
-925.00
-912.50
-900.00
-387.5.0
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-862.50
-850 . 00
-837.50
-8? 5. 00
-312.50
-600 . 00
58774 . 3
58769.9
58765.7
58761 , i
58758.8
58753.0
58745.6
58724 . 4
5S709 . 5
58703.6
58703 .7
58699.1
58690.3
58690.9
58S92 . 8
58702.4
5S727.6;
5874 5 . 8
53750 . 3
58761 . 1
TOTAL
58855.1
58f :59 . 2
58858 . 4
58871 .3
58876.5
58882 . 3
58884 . 5
5f -iPfi 'r 7
58899 . 6
58908.2
58915.2
58929 , 5.
58949.8
5S992 . 5
59073 . P *59131 .0
59007.6
E.8S40.2
58739,4
587 j 1. f
58733 . 3
58751.6
58772.7
5880S . 8
58815.1
58828.7
5G822 . 8
5.3828 . 2
58836 , 9
58844 . 4
56852 . 6
58346 . 8
58849 . 2
586:52. J
-9999.0
- 999'5 . 0
-9999,0
-9999-0
-9999.0- 9999.0
- 9999 . 0
-9999. O
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GRADIENT'
-9999 . 0
- 9999 . 0
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-9999.0
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-9999 . 0
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-9999.0
-9999.0
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-9999.0...9999 , (;,
-9999.0
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-9999.0
-9999 . 0
l l l l l l l l l l l l l l l l l l l
UTHMAG.XYZ T hurst Jay, March 9 . 1 989 3:06 pen Page 3
200.200.200.200.200.200.200.200.200.200.200.200.200.2OO.200.200.200.200.200.200.200.200.200.200.200.2OO.200.200.200.2OO.200.200.200.200.200.200.200.200.200.2OO.200.200.200.200.200.200.200200.200.200.200.
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LITHMAG.XYZ Thursday, ha r c h 9, 1969 3:06 ptn Page
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58823 . 58818.58820.5,8817.58817.58814.58313.58814.58810.58804 .
58810.58832 .58850.58876 .589D4 .58943 .56*963 .59007 .59038.59066 .59083 .59103.59105.59104.59103.59094 .59071 .59027 .59008 .
53993 .58994 .53988 .58999-59019. 5904O. 59076. 59119. 5,9346.59164.59:156.59155.59173.59206 .5,9225, .59222 .5959.5.59150.59139.59150.59166.
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LITHMAG.XYZ Thursday, March 9, 1989 3:06 ptn
200.00200.00200.00200.00200.00200.00200.00200.00200.00200.00200.00200.00
LINE *300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.00300.003OO.OO300.00300.00300.00300.00300.00300.00300.00
, 300.00300.00300.00300.00300.00300.00300.00300.00
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600.00612.50625 . 00
637.50650.00662.50
675,00
687.50700 . 00
712.50725.00
STATION-1381 .00-1375.00-1362.50-1350.00-1337,50-1325.00-•1332.50
-1300.00-1287,50-1275.00
-1262.50-1250.00-1237.50-1225.00-1212.50-1200.00-1187,50-3175.00
-•1162.50-1150.00-1137,50-1125.00
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-1037.50-3025.00-1012.50-1000.00-987 . 50-975 . 00-962.50- 950 . 00-937 . 50-925,00-912.50-900.00-887 . 50-875.00
59393.059206 , 45921 1 . 559200 . 9
59175.0
59151 .359325. 9
59097 . 9
59074 . t :
59071.9
59074 . 3
59091.5
TOTAL
58825 . 5
58825.6)58831.958S38.558853.058857 . 353869 . 1
58867.258870.458871 . t.58872 . 058875 . 7
58880 . 7
58889 . 058895 . 458899.8
5S902.4
589O4 . g:
68914.95893 1 . 358921 . l58933 . 4
58934 . 6
58934 . 0
58942'. 1
5894 5 . 6
58954.7
58957 . 4
58966.658976.858 98 5.158995. s59006 ..859037.759064.759095., 7590 76 . 958971.558711.150693.258720.058743 . 3
- 9999 . 0-9999 . 0-9993.0- 9999 - 0
-9999 . 0
-9999 . 0
-9999.0
- 9999 . 0
- 9999 . 0..9999 m Q
-9999 . 0-9999.0GRADIENT- 9999 . 0
- 9999 . 0- qqqq ̂ Q
-9999.0-9999 . 0-9999.0
-9999 . 0
- 9999 . 0-9999.0
•9999.0
-9999.0- 99QQ . Q
-9999.0-9999. t'-9999.0-9999.0- 9999 . 0-9999.0
9999 . C-9999 . 0-9999.0-9999 . 0- 9999 . 0
-9999.0--9999 . 0.,.c.Qqq ̂ o
-9999.0
-9999. C
-9999 . 0
•-9999. 0
-9999 . 0-9999.0-9999 . 0-'9999 . 0-9999.0-9999.0-9999.0
-9999.0
- '9999 . 0-9999 . C-9999.0-9999 . 0
l l l l l l l l l l l l l l l l l l l
i : LITHMAG.XYZ Thursday, March 9, 1989 3:06 prn Page 6
300300300300300300300300300300300300300
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-712
-700
-687-675-662-650-63?—625
-61 2-600-587-575
- 562
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- 525-512-500-487-475-462
-450
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-352-•350-337-325-312-300-287-275-250-237
- 225-212-20Q
-t 87- 1 75
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5s:fe? ,58780.58795 .
58805 ,
58809 .58819.58820.58827.58830.58826 .58830.58827 .
58828.58825 .58821 .58818.53820 .58812.C]C;,-,..j C ,
58822.58818.58817 .
58819.58813.58809 .58799.58798.58795.58794 .58791. .58786.58786 .58780 .58776 ..
58774 .58774 ,5877;,.
58778.58779 .
58780 .
58782 ..58784 .5878-' .
58736 .58793
58797 .
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58810.
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58830 .
58834,
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LITHMAG.XYZ Thut'-sday, March 9, 1989 3:06 pai Page 7
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UTHWC.XYZ Thursday. t-Urch 9, 1989 3:06 pitt Page 8
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STATION 0.00
STATION0.00
STATION0.00
STATION0.00
STATION0.00
STATION 0.00
STATION0.00
STATION
TOTALSC 725 .4
TOTAL58758 . 3
TOTAL58799 . 7
TOTAL56828 f .
TOTAL
58825. 1TOTAL
-58820 . 7TOTAL
48S04 . 4 T01 A L
58730 , 5TOTAL
5678 1 0
TOTAL58782 . 7
TOTAL S8 /89 . 1
TOTAL^ P~7'P,"\ r-',
TOTAL5.8780 . 2
TOTALS8775 . 6
TOTALc^-r-r? g
TOTAL 18786 . y
TOTAL
58 79 1.7
TOTAL
58789 . 3
TOTAL
58767.9
TOTAL
58764.3TOTAL
S8767 . 7TOTAL
58761 .2TOTAL
58757. STOTAL
58751 .3
TOTAL
58756.9
TOTAL
58727.9
TOTAL
S? 74 4- 7
TOTAL
GRADIENT- 9999 . 0GRADIENT-9999 . 0 GRADIENT-9999 . 0GRADIENT- C'OOO ^.
GRADIENT-9999.0GRADIENT -9999.0GRADIENT- 9999 . 0 GRAD I ENT'
-9999 . 0GRADIENT-.QC.'CJC! Q
GRADIENT-9999 . 0GRADIENT -9999.0GRAD) ENT
-5999.0 GRADIENT-9999 . 0GRADIENT-9999.0 GRADIENT-•-;'W'J.O
GRADIENT -9999.0GRADIENT
-9999 . 0GRADIENT-9990,0
GRADI ENT-9999 . 0 GRADIENT-9999.0GRADIENT -9999.0GRADIENT-9999 . 0GRAD] ENT-9999.0GRAD] ENT-9999.0 GRADIENT-9999 . 0GRADIENT -9999.0GRADIENT-•9999.0
GRADIENT
111111111iiiiiiii
UTHMAG.XYZ Thursday, MoU'cli 9, .1989 3 :06 firn Page 30
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TOTAL 58.-M0.9
TOTAL58853 . 0TOTAL
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58732.6
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58757.0
58759,5
58768,3
58778.9
58783.3
58797 . 258804 . :-'
S8811 .3
588 i 9. 6
58832-8
58343.:"'
5C878 . 1
58904 . 0
58960.8
-QQQ-; o
GRADIENT
-9999.0
GRADIENT
-9999.0
GRADIENT
-9999.0
GRADIENT
-9999 . 0
GRADIENT
-9999.0
GRADIENT
-9999.0
GRADIENT
-9999.0
GRADIENT
-9999.0
-9999 . 0
-9999 . 0
-9999 . 0
-9999.0
-9999.0
-9999 . 0
-9999.0
-9999 . 0
-9999 . 0
-9995.0
-9999.0
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-9993 . 0
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TOTAL58919.5
TOTAL 58907 . S
TOTAL58695 . 6 58694 . 158728.058744 . Si58760 . 458768.;58789 758794 , 3 58809 . 158809.358800 . 2 53776.358754 . 75872?' . 058733.058731 .;.58740.5
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58379.9TOTAL
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58135.0T01 AL
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TOTAL57864 9
TOTAL57416.2
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56706.. 2
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57933.6-TOTAL
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56:707 . 2TOTAL
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Page 33
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TOTAL59891.5
TOTAL59650 . 8TOTAL
59718.5TOTAL
59766.6TOTAL
59490.9TOTAL
59291 . 1TOTAL
59060.2TOTAL
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58693.0
58697.5K1S9S.2
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58497 . 3
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58856 . 459082,459231 . 159230.259148.659039.058894 . 558647 . 5
day, March 9, 3989 3:06 pin
-9999.0-QCjqC; 0
-9999.0
-9999. C
-9999.0-9399.0-9999 . 0-9999.0-9999.0-9992 . 0-9999 . 0-9999.0-9999. G- 9999 . 0
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-9999.0-9999.0-9999.0-9999.0-9999.0-9999.0
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Pag© 36.
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Thursday, March 9 r. 1989 3:06 pro Page 3?
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-287 -275-262-250-237
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- 1 25-112
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58417.
58204 .
53030.
57876,
57902.
58035.
58110.
S8102.
58079.
58083 .
58120 .
58199.
58254.
58343 .
58406.
58510.
58603 .
58736.
58760 .
58774 .
58731 .
58635.
58515.
58434 .
862
4
4
4
4
5
9
7
2
2
212C'
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7
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2TOTAL
58532 .
58478.
58437.
58443.
58473 .
68521.
58526- .
58510.
58499.
58486 .
561453.
53424.
58436.
58417.
584-04 .
.58415.
56:445.
58510.
58623.
68742.
58797.
58888 .
58986 .
59061.
58938.-587C1 ,58553 .58372 .58332.58143.
50
69
4
602c;
60 6o
c;
630
q
604
528220
-9999.- 9999 .-9999.
000
-9999.0 -9999.0-9999.-9999 .-9999.-9999 .
0000
111
-9999.0-9999, -9999 .-9999 .-9999 .-9999.. 9999 ,
0 00
000
-9999.0-9999.
-9999 .- 9999 .
-9999.-9999.
0 000 000
GRADIENT-9999.- 9999 .-9993 . -9999 .-9999.-9999.
-9999.-9999.-9999 .-999v-! .
-9999..9999 . -9999 .-9999,-9999 . -9999 .-•3999 .-999-3.
-9999 .-999S1 .
-9999.-9999 . -9999.-9991?.
-9999.
0000
00 000
0
0
0
0
0
0
0
0
0
0
0
000000
- 99*99 . 0- 9999 .-9999.
0
0
-9999.0
11111111111111
-LITHMAG.XYZ Thursday, March 9 , 1 989 3:06 prri Page 38
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-1700.-1700.-1700.-1700. -1700.
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-387.
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00
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-125.00-112. 5-0
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f -1600.00 -37. f -1600.00 -25.
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STftTI-325. -312.
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57791 .
57880.S8245.57977 . 57839 .57959 .58195. 58361 .58490.5857S .
58493.
58381 .
9408
2
64
68
08
TOTAL58733 .
58739 .
53718.58726 . 58742 .58756.S8766.58774 . 58762.58750.
58755-58764 .58769.5876.8 .58762.58773.58788. 58810.58844 .5893"'.
59040 .591.89.59334 .594 58 .59573 .59766 .59991. 60443.60563.59437. 58864 .58459.58414.58687 .59126.59082 .59743. 59455.
54
5
43
7
31 6o
9294
1
2
c
3366
7
6
8
3
1
82
c
•7
9 6
TOTAL5.8740 . 58718.
1 1
- 9999 .-9999 .-9999 .-9999. -9999.-9999.-9999 . -9999 .-9999 .- 9999 .-9999 .-9999.
0000 000 00
000
1111
GRADIENT-9999 . -9999 .-9999 ̂
0 00
-9999.0 -9999.0-9999.- 9999 .-9999. -9999.-9999.-9939. -9999.-9993.
-9999 .-9999 .—Cj'-JQQ
-999-1 .
-9999. -9999 .- 9999 .-9999. -9999 .-9999.-9999 .- 9999 ...9999 f
-9999.-9999. -9999.-9999 .
-9999 .-9999.-9999.-9999.-9999 .-9999.-9999. -9999.
G0
0 000 000Q0c0 000 00000
0Q
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GRADIENT- 9999 . -9999.
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Thursday. March
-300.00-287.50-275,00-262 . 50-250.00-237.50-22 S. 00-21 2. SO-200.00-187.50-175.00-162.60-150.00-137.50-125.00-112.50-100.00-8 7. SO
-75.00-62.50-SO. 00-37.50
-25.00-12.50
0.0012.5025.0037.5050.00f .2 . 5075 . 0067.50100.00112.50125.00137.50150.00
STATIC*-!
-233.00-225,00•2. 1 2. SO-200 . 00-187.50
-175.00
-162.50-150.00-137.50-125,00-112.50-100.00-97 . 50-75.00-82 . 50-50.00-37.50
58726 . 753776,258799 . 958808,458814.658767.2
56747.3
5S747.958730.858848 , 759025.659141 . ~53288 . 159512.359467 . 0
59499 . 4
59527.5
59500.0
59395.4
59283 . 5S9520 1
59631 . A
59460.958377,3S7676.256840.556717,757010.657647.6588 16. e.59619.758934 . A.58766.856571 .560130.959576 . c.'
58031 .5TOTAL
58693.258692 . 558730.458701 .358713.2587 16. J.
58759 . 058809 . 358939.059046,. 859356.759761 . 060163.260436.360865.9
61 476. l60164.9
-9999 . 0-999:-' . 0
-9999 . 0-9999 . 0-9999.0- 9999 . 0-9999.0-9999.0-9999.0-9999.0-9999 . 0-9999.0-9999.0
-9999.0-9999 . 0-9999 . 0
-9999.0-9999.0
-9999.0-9999.0-9999.0-9999.0
-9999.0-9999.0-9999 . 0-9999.0-9999.0-9999.0
-9999.0- 9999 . 0-9999 . 0-9999 . 0-9999.0- 9999 . 0-9999 . 0-9993.0-9999.0GF;fiDIF.NT
-3999.0-9999 . 0-9999 . 0- 9999 . 0-9999 . 0-9999.0
-9999.0-9999.0••'3999. C
-9999.0-9999.0- 9999 . 0-'S99I9 . 0
-9999. C-9999 . 0-9999.0
-9999 . 0
Page 39
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UTWWG.XYZ Thursday, March 9. 1.988 3:06 prn Page 40
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LINE *-1300.00 -1300.00-1300.00-1300.00-1300.00 -1300.00-1300.00-1300.00 -1300.00-1300.00-1300.00-1300.00-1300.00-1300.00-1300.00 -1300.00-1300.00-1300.00 -1300.00-1300.00 -1300.00-1300.00-1300.00-1300.00 -1300.00 -13OO.OO-1300.00-1300.00-1300.00 -1300. OO-1300.00
-25 . 00-12,50
o.oo12.5025 . 0037.5050.0062 . 5075.0087.50100.00112.50125.00137.50150.00 162.50175.00187.50200.00 212.50225.00237 . 50250.00
STATION-200.00 -187.50
-175.00-362.50-150.00 -137.50-125.00-112.50 -100.00-87 . 50- 75 . 00-62.50-50.00- 37 . 50
-23.00 -12.50
0.001 2 . 50
25 . 00
37 . 50
50 . 00
62 . 5075 . 0087.50 100.00 1 1 2 . 50125.00
1.37.50150.001 62 . 5,0
175.00
58575.05S323.6;58883.760145.460415.960099.759502.058828.158522.358538 . 0588 1 5 . 8 59319.659544.160364 . 160974.3 59849.458647 . 3565042.058039.9 58121.358203 . 158272 . 458341.6
TOTAL58798 . 3 58728.358714.358790 . 95897S . 8 5906.4 . 'J
58866 . 958868 . 5 590S2.559307 . 759851 . 160615.562455.362298: . 2
58 1 5 1 , 2
56736 . 7
56615.456609.2 56629 . 156576 . 5 56729 . 156724 . E.57366.057136.6 56998.9 57078 . 957342 . 057559 0
57811 .5 58035.658275.8
-9999.0-9999 . 0-9999 . 0-9999.0-9999.0-9999.0-9999.0-9999.0-9999 . 0-9993.0-9999.0 -9999.0-9999 . 0- 9999 . 0- 9999 . 0 -9999 . 0-9999.0-9999.0-9999.0 -9999 . 0-9999.0-9999 . 0- 9999 . 0GRADIENT-9999.0 -.QQOC; . 0
-9999.0- 9999 . 0-9999 . 0 -9999. o-9999 . 0-9999 . 0 -9999 . 0- 9399 . 0-9959.0-9999.0-'5999.0
-9999 . 0-9999.0 -9999.0- 9999 . 0- 9999 . 0 -5999.0-9999 . 0
-9999 . 0
-9999.0-9999.0
-9999.0 -9993.0-9999.0-9999.0-9999 . 0 -9999.0-9999, G
l l l l l l l l l l l l l l l l l l l
LITHMAG.XYZ Thursday, March 9, 1989 3:06 pm Page 41
ii-
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-1300.00'"" -1300.00
-1300.00
-1300.00-1300.00-1300.00-1300.00-1300.00-1300.00-1300.00-1300.00-1300.00-1300.00
LINE *-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00
1 -1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00-1200.00
- -1200.00-1200.00-1200.00
, -1200.00-1200.00-1200.00
! -1200.00-1200.00-1200.00
" -1200.00-1200.00-1200.00-12OO.OO
187.50200 . 00212.50225.00237.50250 . 00262.50275.00287 . 50
300.00312,50325.00
337 . 50STATION-312.50-300 . 00-287.50-275.00
-262 . 50-250.00-237 . 50-225.00-212.50-200-00-187. .50-175.00-162.50-150.00-137.50-125. TO*-112.50-100.00-87,50-75 .00
-62.50-50.00-37.50-25.00-25.00" -i li' ' v.'V 1
0.0012.5025.0037 . 50
50 . 0062 . 5075 . 006:7.5.0
100.00112.50125.001 37 . 50
150,00
162,50175.00
58346.858583.158371 .9
58097 . 458211.6583781.0
S3440 . 15848? . 6CgertQ ~l
58526.058 539 . 358576.7
58638 . 8TOTAL
59410.459018.758606 . 658660 . 653726 . 758879.959037 . 458909 . A58753 . 1
58694 . e58758.458875.. 159027.05905?, f :59137.65907&.6.59094 . 459139.559524 *l
60262.561307.062325.162631 . 759591 . 5
59214.758675.957040 . 55C.079 . 053410,256209.857243.457690.8S7917.4
58046.-;!58116.158145.858171 .758196.458252.1
5,8306; , 5ffi'-'-'"-'- '--
-9999 . 0-9993.0-9999 . 0
-9999.0- 9999 . 0- 9999 . 0
-9999.0-9999.0- 9999 . 0
-9999 . 0-9999.0
-9999.0
-9999.0GRriDj EN
-9999.0-9999.0- 9999 . 0-9999.0
- 9999 . 0-9999.0- 9999 . 0-9999.0
-9999 . 0
-9999.0-9999 . C-9999.0-9999 . 0-9999 . 0-9999.0- 9999 - Q-9999 . 0- 9999 . 0
-9999.0
-9999.0-9999.0- 9999 . C*-9999 . 0-9999.0-9999.0- 9999 . 0-9999.0-9999.0-9999 . 0-9999.0
-9999.0-99'?? . 0-9999 . 0- 9999 . 0-9999 . 0- 9999 . 0-9999.0-9999.0-9999 , 0
-9999,0-9999,0
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-1200.00"V LINE *:: : .i -iioo.oof1' -1100.00f:"'' -1100.00| :"" -1100.00St -1100.00W, -1100.00i' -1100.00f^ -1100.00-p" -1100.00f';"' -1100.00
M; -1100.00
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ip. -1100.00|; - -1100.00F"' -1100.00
t -1100.00IF . -iioo.oot' -1100.00Ir; -1100.00T"' - 1100.00l,;,, -1100.00Ur: -1100.00p1 . -1100.00f" -1100.00P''" -1100.00
if1 -1100.00
Thursday, March 9, 1989 3:06 pxn
137.50200.00212.50225.00237 . SO250.00262.50275.00287 . 50300.00312.50325. CO337.50350.00362.50375.0.0387 . 50400. '00412.50425.00
STATION-425.00-412.50-400.00-387 . 50-375-. 00-362.50-350.00-337 . SO-325,00-312.50-300.00-287 . 50-275.00-262 . -5O
-250.00
-237.50-225.00-212.50-200.00-187.50--175.00
-162.50-15:.0.00-137 . 50
-125.00-112.50-100,00-87 , SO-75 . 00
-62 . 50
-50.00
-37,50-25.00
-12.50
58246 , 4
5828? . 958426.75.8490. 158617 .758647.558530.158485. 458469 . 2
58484 . 758501. S
58513.358-533.45,85,57.158574.65,85.89 . a5861 5 . 25.8626 . 058644.6cp'f^Kt Q
TOTAL5,8587.658579 . 55.85,67.5,58 570 . 9585^3 3
58 580 . 458675.458837 . 958929 . 758921 . 158646 . 4
58561 . 15,86' :i5 . 458738 . 4
58785.1
58724.0
58844 . 6
5,8874.6
5,392fc: . 953939 . 1
58999 . 5
S3978 . 858943.058923 . 95,8868 . 558817.858947 . 959311.359763 . 7
59848 . 5
60480 . t",
60959 . 1
59284 . 9
54711.7
- 9999 . 0
-9999 . 0-9999.0-9999.0-9999.0
-9999.0-9999.0
-9999 . 0-9999 . 0- 9999 . 0- 9999 . 0
-9999.0-9999 . 0-9999.0-9999.0-9999.0- 9999 . 0
- 9999 . 0-9999 . 0- Qqoq . oGRADIEIHI- 9999 . 0-'J999.0
-9999.0-9999 . 0— Cj'QQC,' fj
-9999 . 0- 9999 . 0-9999.0
-9993.0-9999.0-9999.0
-9999.0-9999.0-9999.0-9999.0-9999.0- 999J; . Q
-9999 . 0- 9999 . 0-9999.0
-95599.0
-9999.0-9999 . 0
-9999.0-9999.0-9999.0
-9999.0- 9999 . 0-9999.0-9999.0-9999.0-9999.0
-9999.0•9999.0
Page 42
l l l l l l l l l l l l l l l l l l l
Thursday, March 9. 1989 3:06 pin Page 43
: " -1100.00-1100.00-1100.00
; -1100.00i. -1100.00
-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00.-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00-1100.00
'LINE *-1000.00-1000.00-1000.00-1000.00-1000.00-1000.00-1000.00-1000.00— 1 fWi (Vi— A \FiSiJ . ^.X'
-1000.00
0.0012. SO25,0037. 50SO. 0062. SO75.0087 . 50
100.0011 2 , SO1 25 . 00137.50150.00162.50175.00187.50200.00212.50225.00237.50250.00262 . 50Z 75.0O287 . 50300 . 00312.50325,00337.50350.00362. SO375.00387.50400 . 00'512.50425.00437 . 50450.00462 . 50475 . 00487 . 50500 . 00512.50525.00S3? . 50
STATION-537 . 50-•5 ;: 5. 00-512.50-500.00-487.50-475.00-462.50-450.00-437.50-42 5. .00
55668 . 4M 292. 356263 . 356.927.357761.458028.65S2l9.il58287 . 058269.55S299 . 058311 . J58303 . 558301. .0Ktfl~3;, '"'C-' c i
5846:1.258734 . 660S57 . 662015.360360 . 859324 . 258620 . 558146. 758101.4582'1 4. 35&5G3 . l53463. e58377 . 858409 . 958426 . 158437. f58473 . 558500.058547.55S573.75661 1 .0S&&26.558650.15S&&8 . 958712.45.8730.8K C.; "7"?;"; C
5.8731 . 358697 . 058662 . 4
TOTAL58672 . AS&691 .458720 . 158747 , 558779 . 258782.758760.2S8713.858682 . 358697 . 9
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LITHMAG.XYZ Thursday, March 9, 1989 3:06 prn Page 48
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58935^..58895.5884S;.58774 .58:7 00 .58610,58543.68456.58406 .58352,5,8339.58274 .5,8264 .58269 .58308C ;~~ C. C
58:352.53303,
i
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-9999-9999-9999-9999-9999-9999-9999-9999-9999- QClO'*,,
-9999-•9999
-9999- 9999-9999-9999
. 0
.0
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.0
.0
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.0
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.0. 0
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.0.0.0
-9999.0-9999-9999-9999-9999- 9999- 9999-9999-'9999
- 9999-9999-999:'
-9999^ oooc-
-'9999-9999-9999-9.993
.0
.0
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. 0
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2 -9999.0K,
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l l l l l l l l l l l l l l l l l l l
LITHMAG.XYZ 1989 3:06 p f n Page- 57
: -400.00-400.00-400.00-400.00
' -400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00
' -400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00-400.00
LINE f-300.00-300.00
* -300.00-300.00-300.00-300.00-300.00
•' -300.00-300. TO-300.00-300.00-300.00-300 . 00-300.00-300.00-300.00-300.00-300.00-3OO.OO-300.00-300.00-300.00-300.00-300.00-300.00
2002122252372502622752873003123253373503623753874004 1 2425437460462475487500612j (C. O
537550
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•y •••f j~ --i- 11 .
-326-312
- 300-28 r/•275-262-250-237-225-212-200-187-175
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566.08 .58:620 .58632 .5864 2.58644 ,58666 .58679 .58693 .5S706.58713.58718.58725 .58729 .58735 .
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-300.-300.-300.-300.-300.-300.-300.-300.-300.-300.-300.-300.
-300.-300.-300.-3OO.-300.-300.-300.
00000000000000000000000000000000000000
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U'J'U'-' lxl1 ' ' ' •elf'^-Ktnistryoi Report of Work 11.1 8908*1*11
Northern Development * 1(u ' *-Jand Mines (Geophysical, Geological,
Ontario , Geochemical and Expenditures)
^PPoTsTMining Act
42AB6NE8096 2.12378 WHITNEY
Survey!*)Magnetic and VLF-EM
Claim Holder(s)
The Lithium Corporation of Canada Ltd.
wnihip or Are*Whitney Twp.
Prospector'* Licence No
T 4929Address
Suite 1404, 141 Adelaide St. W., Toronto, Ont. M5H 3L5Survey Company
E. H. van Hees Geol. Ser. Inc.Due of Survey (from ft to) [Toul Miles of line Cut
8 . l 8 9 129 . l 89 3.5 mi.*y j Wo. r Tf. l T)ay j Mo. f TC. l ___ ______Name and Address of Author (of Geo-Technical report)
E. van Hees 165 Tamarack St Timmins, Ontario, P4N 6P7Credits Requested per Each Claim in Columns at fightSpecial Provisions
For first furvey:Enter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse sidg — and enter total (Rh^jf^ J"
MAR 1,
MINING LAN!
Airborne Credits
Note: Special provisions credits do not apply to Airborne Surveys.
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Geophysical
1 \^WcF^m"Snetic
- Magnetometer
; 1QQQ) KWWbiometrlc
- Other
"S.SSHIOHGeochemical
Electromagnetic
Magnetometer
Radiometric
Days per Claim
40
20
Days per Claim
Days per Claim
Expenditures (excludes power stripping)Type of Work Performed
Performed on Claim(s)
Calculation of Expenditure Days Credits
Total Expenditures
15Instructions
Total Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.
Date'January 30/f Recorded Holder or Agent (Signature)" ^^-~^j __~~S—""-—————
Certification Verifying Report of Work
Mining Claims Traversed (List in numerical sequence)
bbSSMENT FIOFFICE-—
Total n umber of m ining claims covered by this report of work.
l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.
Name and Postal Address of Person CertifyingE. van Hees 165 Tamarack St. Timmins Ont. P4N 6P7
Date Certified ,Jan.30/89
Certified by (Signature)
Ministry ofNorthern Developmentand Mines
Ontario
Report of Work(Geophysical, Geological, - Geochemical and Expenditures)
"DOCUMEWr W 8906o|iBr)
Mining Act
ions: — Please type or print.i— If number of mining claims traversed
exceeds space on this form, attach a list. Note: — Only days credits calculated *in the
"Expenditures" section may be entered in the "Expend. Days Cr." columns.
— Do not use shaded areas below.Type of SurveyU)
Magnetic and VLF-EM o 19^7/C , J, /w O *Claim HolderlsT
The Lithium Corporation of Canada Ltd.
Township or Area
Whitney Twp. -Prospectors Licence~Ro.
T 4929Address
Suite 1404, 141 Adelaide St. W., Toronto, Ont.Survey Company
E.H. van Hees Geol. Ser. Inc.
M5H 3L5Date of Survey (from 81 to)31. l ,89 128 , 2Day l Mo. | Yr. j Day J Mo.Name and Address of Author (of Geo-Technical report)
E.H. van Hees 165 Tamarack St. Timmins/ Ontario
Total Miles of line Cut
18.5 mi.
.P4N 6B7' Credits Requested per Each Claim in Columns at rightSpecial Provisions
For first survey:Enter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
i
OMVCMIO. .i/.e.t.r.rc,^
MAR 1-
f MINING LAI,.; ' ' .
1 ^i Airborne Credits f r Note: Special provisions l credits do not apply f to Airborne Surveys. ii
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Geophysical
; j V'EtOiagnetic
\MaoDetometer
- Radiometric
IDS ACTIONGeological
Geochemical
Electromagnetic
Magnetometer
Radiometric
Days per Claim
40
20
Days per Claim
Days per Claim
Expenditures (excludes power stripping)Type Of Work Performed
1i Vformed on Claim(s)
i - lt Calculation of Expenditure Days Credits V Total 1 Total Expenditures Days Credits
' |S -i- 15 *ij Instructions j Total Days Credits may be apportioned at the claim holder's i choice. Enter number of days credits per claim selected i r In columns at right.
Mining Claims Traversed (List in numerical sequence)Mining Claim
Prefix Number
103455510345561034557.0.3.4 55 8
.034559
10363011036302 f\1032629103263010326311031666JU3JLfi.6i.
10316691031670
31674. U 03167 2"Vi
Expend. Days Cr.
!D.te Recjjrdetf HpldBrot^AgsrvrtSTgnature)
Mining ClaimPrefix
mm •f&iffi•'S&&'
Number
f'tVj
;^v-'?"-*V.'i i .--
Expend, Days Cr.
Total number of mining claims covered by this report of work. 18
For Office Use OnlyTotal Days O. Recorded
Bftification Verifying Report of Work
Date Recorded j
HAfri/fflDate Apcoved tt R ecorci
Mining
Bra
l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.j Ml me and Postal Address of Person Certifying
Hees_ —
'-Timmins. OM P4M fiP7Date Certifiedf
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E. H. van Hees Geological Services Inc165 Tamarack StreetTimmins, OntarioP4N 6P7(705) 268-9947FAX 267-7534
Instrument: Scintrex Integrated System Serial Number: 825876 Base Station
Serial Number: 801306 Surveyed By: R. Arbic Survey Date: February, 1989
E. H. van Hees .ne.Lithium Corporation of Canada Limited
VLF-EM SURVEY SURVEY PROFILES
rnr nmittiru] Station Cutler, Muir i ov q 11 on c y -
East Gridri z
Location: Whitney Township. TimminsMining Division: Porcupine, Cochrane DistrictReferences:Drawn By: J.R.W.Scale: 1 : 2500
Checked; J.R.W.Date: March. 1989
Province: OntarioProject: East WhitneyN.T.S.: 42 A/WDrawing Number:
LEW-89-0342A06NE0096 2.1237B WHITNEY 210
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o ol ft
Instrument: Scintrex Integrated System Serial Number: 825876 Base Station
Serial Number: 801306 Surveyed By: R. Arbic Survey Date: February, 1989
E. H. van Hees Geological Services Inc. Lithium Corporation of Canada Limited
VLF-EM SURVEY SURVEY PROFILES
riittinq Station Armapo!frequency 21.4 kHz
East GridLocation: Whitney Township. Timmins
Mining Division: Porcupine, Cochrane District
References:
Drawn By: J.R.W.Scale:! : 2500
Checked: J.R.W.Date: March, 1989
Province: OntarioProject: East Whitney
N.T.5.: 42 A/WDrawing Number:
LEW-89-03
42A06NE0096 2 .12378 WHITNEY
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Serial Number: 801306 Surveyed By: R. Arbic Survey Date: February, 1989Contour Interval: 5/S
E. H. van Hees Geological Services Inc.———————————————————— Jfcr
Lithium Corporation of Canada Limited
VLF-EM SURVEY FRASER FILTER CONTOURS
Utnt. Cutle
East Grid
Location: Whitney Township. Timmins
Mining Division: Porcupine, Cochrane District
References;
Drawn By: J.R.W.Scale: 1 : 2500
Checked: J.R.W.Dote: March. 1989
Province: OntarioProject: East Whitney
N.T.S.: 42 A/WDrawing Number:
LEW-89-03
42A06NE0&96 2.12378 WHITNEY250
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E. H. van Hees Geological Services Inc.105 Tamarack StreetTimmins, OntarioP4N 6P7(705) 268-9947FAX 267-7534
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instrument: Scintrex Integrated System Serial Number; 825876 Base Station
Serial Number: 801306 Surveyed By: R. Arbic Survey Date: February, 1989Contour Interval: 5%
E. H. van Hees Geologica Inc.Lithium Corporation of Canada Limited
VLF-EM SURVAY FRASER FILTER CONTOUR
MAPIrons, otnt Annap ois ;-"roq. 21.4 kHz
East GridLocation: Whitney Township, Timmins
Mining Division: Porcupine, Cochrane DistrictReferences:
Drawn By: J.R.W.Scale: 1 : 2500
Checked: J.R.W.Date: March. 1989
Province: Ontario
Project: East WhitneyN.T.5.: 42 A/WDrawing Number:
LEW-89-0342A06NE0996 2 .12378 WHITNEY
-J
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800
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2.12378
E. H. van Hees Geological Services Inc.165 Tamarack StreetTinunins, OntarioP4N 6P7(705) 268-9947FAX 287-7534
Instrument: Scintrex Integrated System Serial Number: 825876 Base Station Serial Number: 801306
Surveyed By: R. Arbic Survey Date: February, 1989
E. H. van Hees Inc.lithium Corporation of Canada limited
Total Fie d Magnetic Survey
Contour Map East Grid
.ocotion: Whitney Township, TimminsMining Division: Porcupine, Cochrane DistrictReferences:Drawn By: J.R.W.Scale: 1 ; 2500
Checked: J.R.W.Date: March. 1989
Province: OntarioProject: East WhitneyN.T.S.: 42 A/WDrawing Number:
LEW-89-(42AC6Ne0096 2 .12378 WHITNEY390
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