REPORT ON AN AIRBORNE MAGNETIC AND VLF-EM SURVEY WEBB LAKE PROJECT PATRICIA MINING DIVISION, ONTARIO. for ST. JOE CANADA INC.

Transcription

1 5aP03NWe020 S HEATHER LAKE REPORT ON AN 00 AIRBORNE MAGNETIC AND VLF-EM SURVEY WEBB LAKE PROJECT PATRICIA MINING DIVISION, ONTARIO for ST. JOE CANADA INC. by TERRAQUEST LTD. Toronto, Canada January 2, 987 RECEIVED FEB \ MINING LANDS SECTION A-730

2 . INTRODUCTION 2. THE PROPERTIES 3. GEOLOGY 4. SURVEY SPECIFICATIONS 4. Instruments 4.2 Lines and Data 4.3 Toerances 4.4 Photomosaics 5. DATA PROCESSING 6. INTERPRETATION 6. Genera Approach 6.2 Interpretation 7. SUMMARY TABLE OF CONTENTS a.8844 HEATHER LAKE 00C LIST OF FIGURES Fig. - Genera Location Map Fig. 2 - Survey Area Map Fig. 3 - Sampe Record Fig. 4 - Terraquest Cassification Of VLF-EM Conductor Axes Fig. 5 - MAGMOD-3 Mode, August Creek Property No. A-730-, No. A-730-2, No. A-730-3, No. A-730-4, Note: LIST OF MAPS IN JACKET Tota Magnetic Fied Vertica Magnetic Gradient VLF-EM Survey Interpretation Page There are 3 separate properties presented on seven mosaics and therefore there are seven of each of the above isted maps. TERRAQUESr LTD

3 TERRAQUEST LTD, LIST OF PROPERTIES Mosaic Property s A-730. Pashko Lake, East Pashko Lake and Greenbush Lake A Pashko Rapids A Jemima Lake and Jemima North A Frain Lake and Lowry Creek A August Creek and August West A August North and Iron Fas A Vaas Lake

4 . INTRODUCTION - - This report describes the specifications and resuts of a geophysica survey carried out for St. Joe Canada Inc. of 6- Richmond Street West, Toronto, Ontario, M5H 2J4 by Terraquest Ltd., 240 Adeaide Street West, Toronto, Canada. The fied work was performed between October 24 and December 8, 987 and the data processing, interpretation and reporting from December 9, 987 to January 2, 999. The purpose of a survey of this type is two-fod. One is to prospect directy for anomaousy conductive and magnetic areas in the earth's crust which may be caused by, or at east reated to, minera deposits. A second is to use the magnetic and conductivity patterns derived from the survey resuts to assist in mapping geoogy, and to indicate the presence of fauts, shear zones, foding, ateration zones and other structures potentiay favourabe to the presence of god and base-meta concentration. To achieve this purpose the survey area was systematicay traversed by an aircraft carrying geophysica instruments aong parae fight ines spaced at even intervas, 00 meters above the terrain surface, and aigned so as to intersect the regiona geoogy in a way to provide the optimum contour patterns of geophysica data. 2. THE PROPERTIES PASHKO LAKE, EAST PASHKO LAKE AND GREENBUSH LAKE PROPERTIES (A-730.) These three properties are ocated in the Pashkokogan Lake (G-265) and Greenbush Lake (G-2054) Areas approximatey 55 kiometres south of the town of Picke Lake. The properties are approximatey 2 kiometres east of Highway 599 and can be accessed by foat pane. The average atitude and ongitude are 50 degrees 57 minutes, and 90 degrees 3 minutes respectivey, and the N.T.S. reference is 52J/6. The caim numbers are shown in figure 2A and isted beow: Pashko Lake Pashko East Greenbush Lake TERRAQUESr LTD. PA PA PA (58) (2) (3) Tota 0 caims

5 TERRAQUESTff). Figure. Genera Location i tij

6 FIGURE 2A Caim Location Map (exact ocations not certified) S i Q r~ i sk JS -s

7 PASHKO RAPIDS (A-730.2) The property is ocated in the Caron Lake Area (G-984) in the Patricia Mining Division of Ontario about 55 kiometres south of the town of Picke Lake. The property ies in the southwest quadrant of Caron Lake map sheet, approximatey 5 kiometres east of Highway 599. The atitude and ongitude are 5 degrees 02 minutes and 90 degrees minutes respectivey, and the N.T.S. reference is 520/. The caim numbers are shown in figure 2B and isted beow: PA (6)... Tota 6 caims JEMIMA LAKE AND JEMIMA NORTH (A-730.3) These two properties are ocated on four caim map sheets, Greenbush Lake (G-2054), Caron Lake (G-984), Webster Lake (G-48) and Lowry Lake (G-207) in the Patricia Mining division of Ontario about 55 kiometres south of the town of Picke Lake. The properties ie about 7 kiometres east of Highway 599, and can be accessed by foat pane. The atitude and ongitude are 5 degrees and 9 degrees respectivey and the N.T.S. references are 52/3, 52J/6, 520/ and 52P/4. The caim numbers are shown in figure 2C and isted beow: JEMIMA LAKE JEMIMA NORTH PA PA FRAIN LAKE AND LOWRY CREEK PROPERTIES (A-730.4) (9) (3) (6) (8)... Tota 46 caims (3) (6)... Tota 9 caims These two properties are ocated on the western haf of the Lowry Lake caims map sheet (G-207) in the Patricia Mining division of Ontario about 55 kiometres south of the town of Picke Lake. The properties are about 7 kiometres east of Highway 599 and can be reached by foat pane, anding on Frain Lake. The average atitude and ongitude are 5 degrees 4 minutes and 89 degrees 57 minutes respectivey and the N.T.S. reference is 52P/4. TERRAQUESr LTD. i 6

8 CD cr TO m 03 * o m, V. o *-.. m o. 240 Adeaide Street West, Toronto, Canada M5H W7, 'eephonc (46) , I'ax (46)

9 o c: ;o m 0 O x O) n O C+ Q) t-- r-*- O ^. 3 O fd -s O" m ex 240 Adeaide Street West, Toronto, Canada M5H W7, Teephone (46) , Fax (46)

10 : m i ii (, f' ' * A - \\. /; - ;. i *,; * " i '.. ' '. '. - - J(. ' 2 S 5. 8 rv. i ii i i i ii i i i i i i i i : f { :. } K ; (, V -O/ - s s " \. r X v' \ r/ ':\ '^ i, P i,' S \ i i ^ f. ' ^ V i V ;. - ' ;'' " i "^ y i \ \ ' ' \ i. ' J ' i f j ; Y' FIGURE 23 I i t "j, i, "i V ' * ff" '^ T 0^ "^ ^^, L u Is ; ' :;:.-i ;; s ",. ' -i\ " Caim Location Map (exact ocations rot certified),,.,, \~ f- * j * i i ". i "., j * -. : i,. j* -. t 7 - ''. ',- ^'. --. i - o g, S rc in i (3 H K v^ *N TERRAQUESTff). "

11 - 3 - The caim numbers are shown in Figure 2D and isted beow: FRAIN LAKE LOWRY CREEK PA PA AUGUST CREEK AND AUGUST WEST PROPERTIES (A-730.5) (3) (4) () (2)... Tota 30 caims (5) (0)... Tota 5 caims These properties are ocated in the Lowry Lake (G-207) and August Lake (G-940) map areas in the Patricia Mining Division of Ontario about 60 kiometres southeast of the town of Picke Lake. The properties ie in the southeast quadrant of the Lowry Lake map sheet and the southwest quadrant of the August Lake map sheet approximatey 28 kiometres east of Highway 599. The average atitude and ongitude are 5 degrees 02 minutes and 89 degrees 45 minutes respectivey, and the N.T.S. reference is 52P/4. The caim numbers are shown in Figure 2E and isted beow: AUGUST CREEK PROPERTY AUGUST WEST PROPERTY PA PA PA PA PA PA PA (8) (25) (5) (D AUGUST NORTH AND IRON FALLS PROPERTIES (A-730.6).Tota 49 caims (7) (5) (9)...Tota 2 caims These properties are ocated in the August Lake (G-940) and Achapi Lake (G-920) caim maps in the Patricia Mining division of Ontario approximatey 56 kiometres southwest of the town of Picke Lake. The properties ie approximatey 42 kiometres east of Highway 599 and are accessibe by heicopter. The average atitude and ongitude are 5 degrees 8 minutes and 89 degrees 34 minutes respectivey and the N.T.S. reference is 52P/4. TERRAQUEST LTD.

12 , V.^ fr'':j^ : Vi ^ v'^m', ~" i \' '' ^g^. -S-... -f ^ -;; ' -U '. ',- ' 'i;-'\' \ ( ' i ) ' r, j ' i \ i'~ ' ( - i.. --" ' 'R - V,-' v - '. -. \ ' f. -.f' ~ il... ' \ * ' 'J i ''. -- ' 'jf-- i -.i i ' ' i ' -' i ''is'* -.'i, ' ',T^'~."if^"~"'. '- ' ' - ' :o :sf - i...' si ",. ~ * " -,-, j i*-i*-- JU- Ir. j\ ' N '- i. :' *,- ' V TERRAQUESTIW. o.^ FIGURE 2E j b. U is. i^.-.! - - r -. i \ -I - 3" ' C' V.. " j k '-..: i v ; ; p- "i i "j. -::.'"j'- :- ^ i -i ; '; :?! J ^ ^ ( :i ' '." ' ' -i..i,.,;:;:.4,.,:j,,.: Y".:':;';r -i in) : --' \- ' i ~- " ; " r'sr--"' ;: Si "' \ ; ' ; i' '.~r :',' VI.j ' U ' -..- : -. i '\...-y.-. " '"' - ; ' V , \ '- ~- ' '! \, V - ' - -;.... -'. * -' ' i -. i ' '' f N" ;\ "\ ' ' \!/,'. \\ \,;. " x v--.,- \-.v- v-,,'r ',viij \ p^ -j r r - " "i)'" 5." "C,- ;..-i'.. '. zj si :: ^ -, -" o V "^ ' i 0 \. - ' -. \ i ' --.f- - -., v ^ s - s.i v ( ; -.i -. ' -. \ i IM^MI ' i ' ',,. -Vi ' x :- --i - \^i -v \! : 'y ' ji ',i \!'" -, : -' " J r i' - '''i..^!... ^.?. i- - i. - : vi ' :! '.!, ' f i ; : "* "^ ' 7 ' o /' -: ;-.."'! ( - '-'i -" :,/ r, ;: -^U'j T. x^ Caim Location Map (exact ocations not certified) Q Ie 4 ssi J ii J I s

13

14 - 4 - The caim numbers are shown in Figure 2F and are isted beow: AUGUST NORTH PROPERTY PA () (2) (4) (4) (9)... Tota 30 caims IRON FALLS PROPERTY PA ()... Tota caims VALLAS LAKE PROPERTY (A-730.7) The Vaas Lake property is ocated on the Heather Lake caims map (G-2063) in the Patricia Mining division of Ontario approximatey 64 kiometres southeast of the town of Picke Lake. The property ies on the west haf of the caim sheet between Vaas Lake and Misehkow River. It is approximatey 54 kiometres east of Highway 599 and can be reached by foat pane on Vaas Lake. The average ongitude and atitude are 5 degrees 0 minutes and 89 degrees 27 minutes respectivey and the N.T.S. reference is 52P/3. The caim numbers are shown in Figure 2G and are isted beow: VALLAS LAKE PROPERTY PA (6) (3) (5) (5)... Tota 39 caims 3. GEOLOGY Map References. Map 2094: Pashkokogan Lake Sheet. scae :3,680. O.D.M Map 228: Cat Lake-Picke Lake, Geoogica Compiation Series, scae :253,440. O.D.M Map 2442: Sioux Lookout-Armstrong, Geoogica Compiation Series. scae :253,440. O.G.S PASHKO, EAST PASHKO AND GREENBUSH LAKES PROPERTIES (A-730.) A three properties are underain predominanty by east to northeast trending mafic to intermediate metavocanics with intercaations of fesic and sedimentary rocks. Castic metasediments occur south of the Greenbush Lake Faut which trends to the northeast TERRAQUEST ffi).

15 en c 73 TO O cs \ **2,i2' *,j,3s "j i: -fc.4?'-'* * * o (T) i i O ~- o H- rt- O *-. O 2 rr QJ o"0 fd H- \ 240 Adeaide Street West, Toronto, Canada M5H W7, Teephone (46) , Fax (46)

16 - 5 - and skirts the southern edge of the properties. These sediments host a geophysicay interpreted iron formation just north of Greenbush Lake. Two stocks, the Pashkokogan Lake Stock and the East Pashkokogan Lake Stock occur in the survey area and are composed of massive to foiated biotite and amphiboe-biotite trondhjemite granodiorite. Lithium, graphite and suphide mineraization occur within the more fesic rocks aong the shores of East Pashkokogan Lake. A diamond dri hoe aong the southern contact of the East Pashkokogan Lake Stock has intersected pyrite and graphite. PASHKO RAPIDS (A-730.2) The Pashko Rapids property is underain by mafic to fesic metavocanics with minor intercaated metasediments trending to the northeast. Minor metagabbro occurs to the west. Pyrrhotite, pyrite and graphite occur within castic metasediments aong strike to the southwest. JEMIMA LAKE AND JEMIMA NORTH PROPERTIES (A-730.3) These two properties are underain primariy by northeast trending mafic to intermediate metavocanics. The northeast trending Greenbush Lake Faut across the southern edge of the survey area forms a contact with the metasediments to the south. These host iron formation in the vicinity of the survey area and tourmaine aong strike to the southwest. A narrow band of fesic to intermediate metavocanics occurs east of the survey area. FRAIN LAKE AND LOWRY CREEK PROPERTIES (A-730.4) These two properties are underain by east to northeast trending mafic to intermediate metavocanics with narrow horizons of fesic to intermediate metavocanics and metasediments. A syncine passes aong the southern edge of the survey area. Numerous suphide showings occur north and south of the properties. AUGUST CREEK AND AUGUST WEST PROPERTIES (A-730.5) These two properties are underain by a thick unit of fesic to intermediate metavocanics to the northwest, a thin band of fesic to intermediate metavocanics trending to the northeast, and a very thick unit of castic metasediments to the south. Beyond the survey area these metasediments host east trending iron formation. A diabase dyke cuts a ithoogies, trending to the northwest. TERMQUEST LTD.

17 - 6 - AUGUST NORTH AND IRON FALLS PROPERTIES (A-730.6) The August North property is underain by castic metasediments to the north, a thin band of fesic to intermediate metavocanics trending to the northeast and mafic to intermediate metavocanics to the southeast. The Iron Fas property is underain totay by mafic to intermediate metavocanics. An east trending iron formation horizon passes aong the southern edge of the Iron Fas property, to the Misehkow River where it curs around to the southwest and approaches the August North property from the northeast. Severa suphide showings occur within the castic metasediments in the area. VALLAS LAKE PROPERTY (A-730.7) The Vaas Lake property is underain predominanty by mafic to intermediate metavocanics. Fesic to intermediate metavocanics a iron formation occur to the northwest aong the Misehkow River va A massive granitic puton occurs to the southeast of the property. 4. SURVEY SPECIFICATIONS 4. Instruments The survey was carried out using a Cessna 206 aircraft, registration C-GGLS, which carries a magnetometer and a VLF eectromagnetic detector. The magnetometer is a high sensitivity airborne proton (Overhauser) type with the sensor eement mounted in a towed bird at a distance of 4 metres beow and 24 metres behind the aircraft. It's specifications are as foows: Resoution: 0.0 gamma Accuracy: 0.03 gamma for 2 readings per second Cyce time: 0.5 second Range: gammas Gradient toerance: Up to 5000 gammas per meter Mode: Manufacturer: GSM- GEM Systems Inc., 05 Scarsdae Rd., Don Mis, Ontario, MSB 2R5 The VLF-EM unit uses three orthogano detector cois to measure (a) the tota fied strength of the time-varying EM fied and (b) the phase reationship between the vertica coi and both the "aong ine" coi (LINE) and the "cross-ine" coi (ORTHO). The LINE coi is tuned to a transmitter station that is ideay positioned at right anges to the fight ines, whie the ORTHO coi transmitter shoud be in ine TERRAQUESTLTD. -j js

18 - 7 - with the fight ines. It's specifications are: Accuracy: "L*. Reading interva: /2 second Mode: TOTEM 2A Manufacturer: Herz Industries, Toronto The VLF sensor is mounted in the eft wing tip ex tension. Other instruments are: King KRA-0A Radar atimeter UDAS-00 data processor with Digidata nine track manufactured by Urtec Ltd., Markham, Ontario. Geocam video camera and recorder for fight path manufactured by Geotech Ltd., Markham, Ontario Lines and Data a) Line spacing: 00 metres b) Line direction: 360 degrees 45 degrees August North Vaas Lake c) Terrain cearance: 00 metres d) Average ground speed: 93 km/hr. e) Data point interva: Magnetic: metres VLF-EM: metres f) Tie Line interva: 2 kiometres g) Channe (LINE): NAA Cuter, 24.0 khz h) Channe 2 {ORTHO): NLK Seatte, 24.8 khz i) Line km over tota survey area: 847 kms j) Line km over caim groups: Pasko Lake Property... Pasko East Property... Greenbush Lake Property Pashko Rapids Property. Jemima Lake Property... Jemima North Property.. Frane Property. Lowry Creek Property... August Creek Property.. August West Property... August North Property.. Iron Fas Property... Vaas Lake Property... tape recorder, recovery,, Iron Fas and Properties.. 6 kms 24 kms 62 kms 2 kms.. 00 kms 40 kms 60 kms 30 kms.. 00 kms 45 kms 60 kms 25 kms 80 kms (46) Fax 3, 97? c Ci. "B X i s (2 B Adeaide 40 (N TERRAQUEST LTD. T

19 :VLF station:! VLF station 2 IU ^ Magnetometer (coars ^ fjne scae) Li J H- Fiducias TERRAQUESTLTD. "i O CC CO -H C" O ' ' ' ' ' " ' ' ' ' ' " ' ' ' 'It U M i III i i t j M M f t M -i LI-L-L-..f J4,) If. M --M Atimeter j" S V. ' --.,. ^, 'ULMpniaKu..^ ' - f^ - f - ' - ' - - ' V ' ' ' '.^.J^' ' s"'. "r*~tii..l ' ' 'j* - ' t^-pvr r~' ' r-n-j - * ''i-.tomhrt:f S~ - (M....iM "ii ^,.,,,.,,,,,,^,.,^.^*/..-...,-! \^^,r... ' co 'c i t ' j Tj'T -i vi ''rt r-* - -,- n-,-t'n' r r'i T r'i ri't ri T T' c LI j u:: LI:.: o: o ij LJ C''j FIGURE 3. Sampe of anaogue data -j rr r-j T rir r]-i n T-I-n vi p I-T-TT

20 4.3 Toerances a) Line spacing: Any gaps wider than twice the ine spacing and onger than 0 times the ine spacing were fied in by a new ine. b) Terrain cearance: Portions of ine which were fown above 25 metres for more than one km were refown if safety considerations were acceptabe. c) Diurna magnetic variation: Less than ten gammas deviation from a smooth background over a period of two minutes or ess as seen on the base station anaogue record. d) Manoeuvre noise: ni 4.4 Photomosaics For navigating the aircraft and recovering the fight path, semi-controed mosaics of aeria photographs were made from existing air photos. Each individua photograph was photographicay adjusted to conform to the NTS map system before the mosaic was assembed. 5. DATA PROCESSING Fight path recovery was carried out in the fied using a video tape viewer to observe the fight path as recorded by the Geocam video camera system. The fight path recovery was competed daiy to enabe refights to be seected where needed for the foowing day. The magnetic data was eveed in the standard manner by tying survey ines to the tie ines. The IGRF has not been removed. The tota fied was contoured by computer using a program provided by Datapotting Services Inc. To do this the fina eveed data set is gridded at a grid ce spacing of /Oth of an inch at map scae. The vertica magnetic gradient is computed from the tota fied data using a method of transforming the data set into the frequency domain, appying a transfer function to cacuate the gradient, and then transforming back into the spatia domain. The method is described by a number of authors incuding Grant, 972 and Spector, 968. The computer program for this purpose is provided by Paterson, Grant and Watson Ltd. of Toronto. The VLF data was treated automaticay so as to normaize the non conductive background areas to 00 {tota fied strength) and zero (quadrature). The agorithms to do this were deveoped by Terraquest and wi be provided to anyone interested by appication to the company. TERRAQUEST LTD.

21 - 9 - A of these dataprocessing cacuations and map contouring were carried out by Datapotting Services Inc. of Toronto. INTERPRETATION 6. Genera Approach To satisfy the purpose of the survey as stated in the introduction, the interpretation procedure was carried out on both the magnetic and VLF data. On a oca scae the magnetic gradient contour patterns were used to outine geoogica units which have different magnetic intensity and patterns or "signatures". Where possibe these are reated to existing geoogy to provide a geoogica identity to the units. On a regiona scae the tota fied contour patterns were used in the same way. Fauts and shear zones are interpreted mainy from atera dispacements of otherwise inear magnetic anomaies but aso from ong narrow "ows". The direction of regiona fauting in the genera area is taken into account when seecting fauts. Foding is usuay seen as curved regiona patterns. Ateration zones can show :up as anomaousy quiet areas, often adjacent to strong, circuar anomaies that represent intrusives. Magnetic anomaies that are caused by iron deposits of ore quaity are usuay obvious owing to their high ampitude, often in tens of thousands of gammas. VLF anomaies are categorized according to whether the phase response is norma, reverse, or no phase at a. The significance of the differing phase responses is not competey understood athough in genera reverse phase indicates either overburden as the source or a conductor with considerabe depth extent, or both. Norma phase response is theoreticay caused by surface conductors with imited depth extent. Areas showing a smooth response somewhat above background (ie. 0 or so) are ikey caused by overburden which is thick enough and conductive enough to saturate at these frequencies. In this case no response from bedrock is seen. Grant, F.S. and Spector A., 970: Statistica Modes for Interpreting Aeromagnetic Data; Geophysics, Vo 35 Grant, F.S., 972: Review of Data Processing and Interpretation Methods in Gravity and Magnetics; Geophysics 37-4 Spector, A., 968: Spectra Anaysis of Aeromagnetic maps; unpubished thesis; University of Toronto, 968. TERRAQUESTLTD.

22 - 0 - The VLF-EM conductor axes have been identified and evauated according to the Terraquest cassification system {Figure 4). This system correates the nature and orientation of the conductor axes with stratigraphic, structura and topographic features to obtain an association from which one or more origins may be seected. Aternate associations are indicated in parentheses. 6.2 Interpretation The magnetic and VLF-EM data are shown in contoured format on maps at a scae of :0,000 in the back pocket. An interpretation is aso provided. The foowing notes are intended to suppement these maps. PASHKO, EAST PASHKO AND GREENBUSH LAKES PROPERTIES (A-730.) The tota magnetic fied has a very arge reief in excess of 8,200 gammas. The highest responses come from the southeast and dominate and overwhem the responses from other ithoogies over amost haf the survey area. East and northeast trending anomaies occur over the northwestern haf of the survey area. The vertica magnetic gradient data substantiay improves the resoution of the very high magnetic responses and enhances the weaker magnetic trends, particuary those to the northwest and northeast. The very strong magnetic anomay to the southeast correates with the previousy, geophysicay interpreted iron formation. Responses of this magnitude are characteristic of typica iron formations. The second strongest anomay trends uniformy to the northeast and coincides with the Greenbush Lake Faut. It is interpreted to be reated to a possibe mafic intrusive {Unit 4) such as a diorite that intrudes the faut zone. The granodiorite intrusives (Unit 7) correate with moderate to weak magnetic responses and a random pattern of moderate gradient vaues on the vertica gradient magnetic map. The contact with the Pashkokogan Lake Stock is best outined on the tota magnetic fied map. The remaining magnetic responses are interpreted as mafic to intermediate metavocanics (Unit ) and fesic to intermediate metavocanics (Unit 2). The stronger magnetic vaues are interpreted to correate with the mafic to intermediate metavocanics. Horizons of increased magnetic activity within these ithoogies (Units m and 2m, respectivey) are probaby reated to increased concentrations of magnetic mineras such as magnetite or pyrrhotite, or possiby to more mafic compositions or intrusive rocks. The very subte 2m horizon aong the northern edge of the Pashko Lake property can ony be detected on the vertica magnetic gradient map. TERRAQUEST LTD.

23 FIGURE 4 TERRAQUEST CLASSIFICATION OF VLF-EM CONDUCTOR AXES SYMBOL a, A b, B c C d. D f, F ob, OB cu, CUL CORRELATION Coincident with magnetic stratigraphy Parae to magnetic stratigraphy No correation with magnetic stratigraphy Coincident with magnetic dyke Coincident with topographic ineament or parae to faut system Contours of tota fied response conform to topographic depression Coincident with cutura sources ASSOCIATION: Possib.e Origins Bedrock magnetic horizons: stratabound mineraogic origin or shear zone Bedrock non-magnetic horizons: stratabound mineraogic origin or sh'ear zone Association not known: possibe sma scae stratabound mineraogic origin, faut or shear zone, overburden Dyke or possibe faut: mineraogic or eectroytic Faut zone: mineraogic or eectroytic Most ikey overburden: cayey sediments, swampy mud Eectrica, pipe or raiway ines NOTES - Upper case symbos denote a reativey strong tota fied strength 2 - Underined symbos denote a reativey strong quadrature response 3 - Mineraogic origins incude suphides, graphite, and in faut zones, gouge 4 - Eectroytic origins impy conductivity reated to porosity or high moisture content

24 - - Magneticay interpreted fauts trend predominanty to the northeast and a few to the northwest and east. East trending faut dispacements incuding the Greenbush Lake Faut are difficut to identify as they parae the magnetic stratigraphy over most of the survey area. The Greenbush Lake Faut is detected by the magnetic character of the intrusive rocks which foow the ines of weakness, not by the dispacement of magnetic trends. The VLF-EM data shows numerous weak to strong conductor axes. Most of these trend to the east and southeast showing an orientation bias toward the Cuter transmitter. Many show a correation with akes and swampy areas suggesting that conductive cayey overburden is confined to topographic depressions. Those conductor axes that cross-cut magnetic stratigraphy or are i parae to intrepreted or observed structure are associated with ^ structura origins, either faut or shear zones. This type of ^ conductivity may be reated to a) mineras such as suphides, graphite or gouge aong the structure or b) an ionic effect such as porosity or - water within the structure or to cay in overying topographic depression. Note that severa strong conductors parae the Greenbush Lake Faut zone. Those conductor axes that either coincide with or parae the magnetic stratigraphy possess potentia for stratabound bedrock origins such as suphides or graphite. These warrant further investigation on the ground by either EM or IP methods. PASHKO RAPIDS (A-730.2) The tota magnetic fied has a reief of approximatey 700 gammas and shows two broad and severa minor northeast trending anomaies. The vertica magnetic gradient improves the resoution of a these anomaies. The strong anomay to the north beyond the property is interpreted to originate from a semiconformabe pod of mafic intrusives, probaby gabbro, simiar to that which outcrops aong strike to the west of the property. The remaining responses are interpreted to be reated to mafic to fesic metavocanics, the more mafic components correating with the more magnetic responses. Magneticay active horizons are shown as Unit m and are probaby derived from increased concentrations of pyrrhotite and magnetite such as those found in the metasediments to the southwest. The southern most anomay may in fact be on strike with the metasediments suggesting that they may extend onto the southern part of the property. TERMQUESrm i S

25 Magneticay interpreted fauts trend to the northwest. Any northeast trending fauts woud be difficut to detect as they woud parae the magnetic stratigraphy. Three VLF-EM conductor axes have been identified. The strongestone to the north correates with a widening in the Pashkokogan River and is probaby due to cayey, conductive overburden. The two remaining conductor axes are very weak but are parae to the magnetic stratigraphy. These possess potentia for bedrock origins and shoud be foowed up on the ground using EM or IP methods. JEMIMA LAKE AND JEMIMA NORTH PROPERTIES (A-730.3) The tota magnetic fied has a reief of over 3,400 gammas over the Jemima Lake property and 550 gammas over the Jemima North property and show northeast trending magnetic units. The strong magnetic J anomay across the Jemima Lake property dominates and overwhems the responses from the surrounding ithoogies. The vertica magnetic gradient offers improved resoution aong this anomay. The strong magnetic anomay is interpreted as iron formation and shows typica responses for iron rich horizons. Magnetic modeing aong Fight Line 29, using computer software MAGMOD III by Geosoft Inc. (Figure 5), suggests that the iron formation has a width of approximatey 20 metres and a depth of 35 metres (beow aircraft). A the responses to the north correate with mafic to intermediate metavocanics (Unit ). Magneticay active horizons within this unit are probaby reated to increased concentrations of magnetite or pyrrhotite or to more mafic horizons. The magnetic responses south of the iron formation correate with migmatites (Unit 3). Moderatey strong magnetic anomaies (Unit 3m) within this unit may correate with the homogeneous diatexite as shown on the regiona and geoogica compiation map or possiby to iron rich sedimentary or vocanic intercaations. The dominant northeast trending structure cannot be detected on the magnetic map as it is parae to the magnetic trends. Disruptions of the magnetic horizons indicate numerous northwesttrending offsets some of which correate with VLF-EM responses. Many VLF-EM conductor axes correate with akes or river vaeys indicating that conductive overburden is restricted to some but not a of the topographic depressions. At east eight moderate to strong conductor axes correate we with magnetic units and therefore possess good potentia for bedrock origins. These incude graphite and suphides and shoud be foowed TERMQUEST LTD.

26 , ^ JEMIMA LAKE L ne 29 ( Sou t h to Nor t h) Observed F I ed D Base Leve P c -D i 0 ^ u _ j? **T Dx^sjp T \ X - tv O^ ^ ^ S UH g X O^ ^D~ ^ t in o" c 0 T5 ^ ^ V^"tr-tr-0-ri!MJ -,u- jtx g i 800 : ! I a ^ i MODEL PARAMETERS: i GEOMAGNETIC FIELD: Mode Type TABULAR Fied Strength nt Depth F 35M Incination deg Haf Width F 62. 8M Decination -.5 deg Dip F 94 deg Suscept Ib I ty F 0.083emu P] AKI ntdfriinm^r-\ *i* r~"7o(^" xf^f^ia ilrnuj.kl.l'iiuino* Post t ion F M Base Leve F nt Str Ike Perp 0 deg Base Sope F nt/m Line Direction 0 deg (F-ftted, X-fxed, L- Imt ~ 00 s: - j. 200 Geosoft MAGMOD-3 Modeing Resut 88/0/2 TERRAQUEST LTD. T

27 - 3 - up on the ground using EM or IP methods. In paces it is difficut to ascertain whether the responses are derived from ithoogica sources or structura origins parae to the stratigraphy. FRAIN LAKE AND LOWRY LAKE PROPERTIES (A-730.4) The tota magnetic fied over the Frain Lake and Lowry Lake properties are approximatey 520 gammas and 00 gammas respectivey and show the genera east to northeast trend of the ithoogies. The vertica magnetic gradient data enhances the more subte magnetic trends. Most of the magnetic responses correate with the mafic to intermediate metavocanics (Unit ). Magneticay active horizons (Unit m) within this ithoogy are probaby associated with magnetite or pyrrhotite rich horizons or more mafic compositions. It is -^ suspected that the northwest trending magnetic units may originate ^ from diabase dykes'(unit 9). The fesic to intermediate metavocanics (Unit 2) and the castic metasediments (Unit 3) as shown on the regiona geoogica map : correate with weaker magnetic responses. Numerous northwest trending fauts and two northeast trending fauts have been interpreted from the magnetic data across the Frain Lake property. Five northeast trending fauts have been identified across the Lowry Lake property. Note that there is a detection bias in favour of cross fauts. The VLF-EM data show numerous weak to moderate strength conductor axes with a bias in favour of those that trend toward the Cuter transmitter azimuth. Those that are obique to the magnetic stratigraphy are interpreted to possess structura origins such as fauts or shear zones. Most of the conductor axes are either coincident with or parae to magnetic stratigraphy and therefore possess potentia for stratbound bedrock sources such as suphides or graphite. The stronger of these conductors with a high degree of correation shoud be foowed up on the ground using EM or IP methods. AUGUST CREEK AND AUGUST WEST PROPERTIES (A-730.5) The tota magnetic fieds across the August Creek and August West properties are quite arge, 7,200 gammas and 4,50 gammas respectivey. These strong responses appear to originate from the same east trending horizon and dominate most of the remaining responses across the survey areas. One moderatey strong anomay trends to the north-northwest. The vertica magnetic gradient TERRAQUESr LTD. f

28 - 4 - improves the resoution of the strong anomaies and removes much of their associated gradients across the survey area. The strong anomaies are interpreted as iron formation across the southern part of both properties. The interpreted width may be exaggerated due to an overwheming effect often associated with high susceptibiities. The remaining responses have been interpreted according to the known geoogy as mafic to intermediate metavocanics (Unit ), fesic to intermediate metavocanics (Unit 2) and castic metasediments (Unit 3). These units are generay in order of decreasing magnetic susceptibiity. Magneticay active horizons within these units (shown by the suffix m) are probaby reated to increased concentrations of magnetite or pyrrhotite or possiby to more mafic compositions. Aternativey some of these horizons may be interpreted as conformabe mafic intrusives. The strong northwest trending anomay is interpreted as a diabase dyke (Unit 9). Magneticay interpreted fauts trend to the northwest and northeast and show a variabe correation with topographic ineaments. The northwest trending diabase dyke probaby intrudes a faut zone. It is specuated that both faut orientations occur in a areas, however there may be a oca detection bias in favour of those structures that possess greater dispacements or occur at a higher ange to stratigraphy. The VLF-EM data show narrow moderate strength conductive zones and broad strongy conductive areas. The atter correate with swamps and akes and probaby originate from conductive overburden. Two conductor axes coincide with magnetic stratigraphy and two are parae to the magnetic units. In paces a portion of these responses may be reated to conductive overburden but in genera they possess potentia for stratabound bedrock origins such as suphides or graphite and warrant ground foow up. Those conductor axes that are obique to the stratigraphy are interpreted to originate from structura sources. IRON FALLS AND AUGUST NORTH PROPERTIES (A-730.6) TERMQUEST LTD.

29 - 5 - the resoution sighty of the anomay at the Iron Fas property and enhances the magnetic stratigraphy across the August North property. The strong magnetic reief across the southern part of the Iron Fas property is characteristic of an iron formation. Despite the improvement in the resoution offered by the vertica magnetic gradient data the actua thickness of the iron formation is narrower than suggested by the magnetics due to an overwheming effect often associated with bodies of high magnetic susceptibiities. The strong responses to the northeast of the August North property are indicative of the approaching iron formation as shown in the regiona geoogica map. The remaining responses are interpreted according to the regiona geoogica map as either mafic to intermediate metavocanics (Unit ), fesic to intermediate metavocanics (Unit 2), or castic metasediments (Unit 3). Magnetic horizons within these ithoogies (shown with the suffix m) are probaby reated to increased concentrations of magnetic mineras, most ikey magnetite or pyrrhotite. The stronger horizons may be the aong strike extensions of the iron formation. In other cases, some of the magnetic horizons may be reated to more mafic compositions. Contrasting structura styes have been interpreted on these properties. The Iron Fas property shows north to northeast trending fauts parae to the main river vaey. The fauts and shear zones across the August North property trend predominanty to the northwest with a few to the east. There is probaby a detection bias in favour of those structures that cross magnetic stratigraphy at a high ange. The VLF-EM data show numerous moderate strength conductive zones and severa strong conductor axes with good definition. The broad conductive zone across the August North property conform to topographic depressions and are probaby associated with conductive overburden. The very strong conductor axes to the north correate we with the iron formation and are probaby caused by suphides within thatrock unit. Simiary severa moderate strength conductor axes coincide with magnetic horizons across the August North property and possess potentia for stratabound bedrock origins such as suphides or graphite. A these warrant further investigation on the ground using IP or EM to pinpoint and verify their existence. Two conductor axes are obique to the magnetic stratigraphy and are interpreted to possess structura origins. The strong conductor axes to the north on the Iron Fas property is associated with a faut or shear zone which may possess potentia for a god bearing structure. TERRAQUESrm

30 VALLAS LAKE PROPERTY (A-730.7) The tota magnetic fied has a reief of approximatey,000 gammas and shows a strong gradient from the northwest to the southeast, overwheming the oca magnetic character. This is improved substantiay by the vertica magnetic gradient data which shows numerous subte northeast trending units. The strong magnetic anomay to the northwest is coincident with i the iron formation and the weak magnetic responses to the southeast S correate with the granitic puton (Unit 7). A the remaining responses are interpreted to be derived from mafic to intermediate metavocanics (Unit ) and their sighty magnetic sub-members (Unit m). The interpretation of the m horizons toward the iron formation become increasingy subjective. It is specuated that any northwesttrending anomaies may originate from diabase dykes (Unit 9). 5 Numerous north to northeast trending cross fauts have been * interpreted from the magnetic data. The dominant dispacement appears to be sinistra aong the iron formation horizon, but is perhaps more compicated within the metavocanics.. The VLF-EM responses are weak to moderate with poor definition, most of them have been interpreted to possess overburden origins. There appears to be a strong overriding bias in favour of those conductor axes that trend toward the Cuter transmitter. The quadrature responses of those conductors that are parae to the fight ine have reduced interpretationa vaue. The conductor axes cose to the iron formation possess a better correation with magnetic stratrigraphy, suggesting a reduction in the conductive overburden. At east three conductors correate we with the stratigraphy and therefore may possess stratabound bedrock origins such as graphite or suphides. These warrant further investigation. TERRAQUESTLTD.

31 7. SUMMARY An airborne combined magnetic and VLF-EM mapping survey has been carried out on thirteen properties at 00 metre ine intervas with data reading stations at metres aong the fight ines. A data is produced on maps at a scae of :0,000. The magnetic data has been used to modify and update the existing geoogy and has shown a number of new contacts and fauts. A number of VLF-EM conductor axes were found most of which are associated with structura sources and overburden. A few are beieved to have potentia suphide origins and have been recommended for additiona investigation. TERRA Chares Q. Barrie, M.Se. Geoogist TERRAQUEST LTD. ^ 6) " o S IT) -i S 2 ^ i j3

32 fype of Survey(s) Ministry of Northern Deveopment Mines Report of Work (Geophysica. Geoogica, Geochemica and Expenditures) ^ Mi 52P83NVree HEATHER LAKE Township or Area 9(2)0 Airborne Magnetic St VLF/EM Sreenbush/Lowry/Pashkokogan Caim HoderU) Prospector's Licence No. St. Joe Canada Inc. T-3608 Address 6- Richmond St Toronto, Ontario M5H 2J4 Survey Company Date of Survey (from Si to) Tota Mies of ine Cut Terraquest Ltd. 5, Day Mo. Yr.^ Day j Mo. Yr. Name and Address of Author (of Geo-Technica report) Chares Qu. Barrie, Richmond St. W. Toronto, Ontario M5H 2K Credits Requested per Each Caim in Coumns at right Specia Provisions Geophysica For first survey: Enter 40 days. (This incudes ine cutting) - Eectromagnetic - Magnetometer Mining Caims Traversed (List in numerica sequence) For each additiona survey: using the same grid: Enter 20 days (for each) - Radiometric - Other Geoogica Geochemica Man Days Compete reverse side and enter tota(s) here Geophysica Eectromagnetic i Airborne Credits - Other Geochemica. SEC Note: Specia provisions i Eectromagnetic i (L s\ credits do not appy to Airborne Surveys. Magnetometer Radiometric Expenditures (excudes power stripping) Type Of Work Performed Performed on Caim(s) Cacuation of Expenditure Days Credits Tota Expenditures S -i- 5 c Tota Days Credits Instructions Tota Days Credits may be apportioned at the caim hoder's choice. Enter number of days credits per caim seected in coumns at right. Tota number of mining caims covered by this report of work. Date Certification Verifying Report of Work hereby certify that have a persona and intimate knowedge of the facts set forth in the Report bf Work annexed hereto, having performed the work or witnessed same during and/or after its competion and the annexed report is true. Name and Posta Address of Person Certifying Mrs. Robin Jowett, 883 Sunningdae Bend, Mississauga, Ontario L5JG Cerioid by (Sgnatu 362 (65/2)

33 Orffario Type of Survey(s) Caim Hoder(s) Address Survey Company. Ministry of Northern Deveopment and Mines Report of Work (Geophysica, Geoogica, Geochemica and Expenditures) Airborne Magnetic 4V St. Joe Canada Inc. VLF/EM Q Mining Act 6- Richmond St. W. Toronto, Ontario M5H 2J4 Terraquest Ltd. Instructions: Pease type or print. If number of minin^^aims traversed exceeds space on this form, attach a ist. Note: Ony days credits cacuated in the "Expenditures" section may be entered in the "Expend. Days Cr." coumns. Do not use shaded areas beow. Township or Area G~-*4. C--/'/ *(JK' Date of Survey (from 8 to). 87r. ;U Greenbush/Lowry/Pashkokog Prospector's Licence No. T-3608 Tota Mies of ine Cut Name and Address of Author (of Geo-Technica! report) Chares Q. Barrie, Richmond St. W. Toronto, Ontario M5H 2K Credits Requested per Each Caim in Coumns at right Specia Provisions Geophysica Days per Caim For first survey: - Eectromagnetic Enter 40 days. (This incudes ine cutting) - Magnetometer Mining Caims Traversed (List in numerica sequence) Mining Caim Expend. Mining Caim Prefix Number Days Cr. Prefix Number See schedue att iched Expend. Days Cr. in For each additiona survey: using the same grid: Enter 20 days (for each) - Radiometric - Other Geoogica..'- f ^* :.. Geochemica Man Days Compete reverse side and enter tota (s) here Geophysica - Eectromagnetic - Magnetometer Days per Caim c -\ - Radiometric - Other Geoogica Geochemica Airborne Credits Note: Specia provisions credits do not appy to Airborne Surveys. Eectromagnetic Magnetometer Radiometric Expenditures (excudes power stripping) Type of Work Performed Days per Caim Performed on Caimis) Cacuation of Expenditure Days Credits Tota Expenditures Tota Days Credits Instructions Tota Days Credits may be apportioned at the caim hoder's choice. Enter number of days credits por caim seected in coumns at right. Date A/ov Certification Verifying Report of Work Recojxjod Hoder or Agorit (Signature) kfw2*r~ Date Recorded /Jot;, it, t f gf heieby certify that have a persona nnd intimate knowedge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its competion and the annexed report is true. Name and Posta Address of Person Cortifyinri Mrs. Robin Jewett, 883 Sunningdae Bend, Mississauga, Ontario L5J G Date Certified Nov. 2/87

34 SCHEDULE A ! !! B B ! B ! B ! !

35 SCHEDULE A(cont'd) B S S B B

36 Ministry of Natura Resources Fie. Ontario GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORT FACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC. Type of Survey(s) c ^ Township or Area Caim Hoder(s) "S/V r W MINING CLAIMS TRAVERSED List numericay Survey Company. Author of Report. Address of Author J^ihLQ. LO Covering Dates of Survey C*cA. ^4 j 8~ "Vo De* (ir/ecutting to office) Tota Mies of Line Cut (prefix) (number) SPECIAL PROVISIONS CREDITS REQUESTED Geophysica DAYS per caim ENTER 40 days (incudes ine cutting) for first survey. Eectromagnetic. Magnetometer. Radiometric ENTER 20 days for each additiona survey using same grid. Other Geoogica. Geochemica. AIRBORNE CREDITS (Specia provision credit* do not appy to airborne urveyi) Magnetometer hid-eectromagnetic H.o Radiometric (enter dayi per caim) DATE:. SIGNATURE: Res. Geo...Quaifications. Previous Surveys Fie No. Type Date Caim Hoder I TOTAL CLAIMS.

37 GEOPHYSICAL TECHNICAL DATA GROUND SURVEYS If more than one survey, specify data for each type of survey Number of Stations Number of Readings Station interva. ^ ^^ Line spacing - Profie scae^^ ^-^^ ^^ -. Contour interva. U iz C Instrument Accuracy Scae constant. Diurna correction method. Base Station check-in interva (hours). Base Station ocation and vaue Instrument ECTROMAGNETK Coi configuration. Apn Method: CD Fixed transmitter CD Shoot back CD In ine CD Parae ine Fremienrv Parameters measured. Instrument. Scae constant Corrections made. O Base station vaue and ocation. Eevation accuracy. p Z (it g0-r Q y Q 2 H E c/; tf Method CD Time Domain CD Frequency Domain P3rfnvtpinc - On time Frequency -Off time Range... DHay t'mf Integration time Power Eectrode array. - Eectrode spacing, Tvne of eectrode....,.

38 4 * SELF POTENTIAL Instrument. Range. Survey Method ^ - ^ ^ ^^ Corrections made. RADIOMETRIC Instrument - Vaues measured. Energy windows (eves).^^^ ^ -^^ ^..^-^..^-^^^..--^. Height of instrument Background Count. Size of detector -^ ^ - ^- ^ -.^... ^.^^^.- -. ^ Overburden. ^.^- -.^ ^ ^ ^. -- -^--..^.. (type, depth incude outcrop map) OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey ^ -^ ^ ^ Instrument ^ - Accuracy ^^^ ^^- ^ ^ Parameters measured. Additiona information (for understanding resuts). AIRBORNE SURVEYS Type of.iirvi-y(.). Instrument(s) Arryrary Aircraft used Sensor atitude ig.s.o.o^e'c- V^rXv^ VVvavxe,oryv^Bc- J (specify fdrvach type of urvey/ r O ^ L-*2 ^ Navigation and fight path ^ QO^-Ct^WsjCX "t VfS '-O ^VNO. 'T.O U (specify for each type of survey) ^V^ -orx ~) \OOr^v /* \ reroverv method. Crg.O CCXX*\,^^vcXer^ <Lo.w,* c^ oocva ^ c^^p C Aircraft atiturfp \OO w^v Line Spacing Mies fown over tota area ~~fc.^a \ V^^-^ Over caims nny ^ *A \c

39 GEOCHEMICAL SURVEY - PROCEDURE RECORD Numbers of caims from which sampes taken. Tota Number of Sampes. Type of Sampe. (Nature of Materia) Average Sampe Weight Method of Coection Vaues expressed in: Cu, Pb, ANALYTICAL METHODS per cent p. p. m. p. p. b. D a Zn, Ni, Co, Ag, Mo, As.-(circe) Soi Horizon Samped. Horizon Deveopment. Sampe Depth Terrain Drainage Deveopment Estimated Range of Overburden Thickness. SAMPLE PREPARATION (Incudes drying, screening, crushing, ashing) Mesh size of fraction used for anaysis Others Fied Anaysis (. Extraction Method. Anaytica Method- Reagents Used Fied Laboratory Anaysis No. -^^ ^^^ Extraction Method. Anaytica Method - Reagents Used, Commercia Laboratory (. Name of Laboratory- Extraction Method Anaytica Method Reagents Used ^.tests).tests) -tests) Genera. Genera.

40 SCHEDULE A IB B B ' ;

41 SCHEDULE A{cont'd) B B ' B "5*2277 '6227S 962S8! * B ! ] 9626e BOB 96B

42 LEGEND HIGHWAY AND "OUTE No 5I 007'30' (- 0 07'JO' OTHER ROADS TRAILS SURVEYED L INI i TOWNSHIPS. BASE LINES ETC LOTS. MINING CLAIMS PARCFiS ETC UNSURVEYED L'NES LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC RAILWAY AND R IGHT OF WAV -..i.v.r 2t i yiicjj IPSS0J" if*" "*i. JL t '""" i "". * "T UTILITY LINES NONPERENNIA, STREAM FLOODING OR f OODiNG "IGH^S ; SUBDIVISION OR COMPOSITE P'. AN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG S MINES TRAVERSE MONnMENT DISPOSITION OF CROWN LANDS TYPE OF DOCUMENT SYMBOL -. -aj ^^ PATENT. SURFACE ft MINING RI. SURFACE RIGHTS ON L. MINING RIGHTS ON- ~ L EASE. SURF ACF S MINING KiO ". SUR^AC: RIGHTS ON. ^ MINING RIGHTS ON, ' LICENCE OF OCf'.'P&T'ON ORDER IN COUN'.'-IL RESERVATION CANCELLED SAND A o NOTE T, B v t V A" ifil-rtflj'rii J^^^f ' Vtjof ' y i 7 T, vfc7 r/j.^(.^r/y j^tjjt'i REFERENCES AREASJ/VITHDRAVVN FROM DISPOSITION s,w i ' 2LVi ' ifftltt 9t^i M.R.O. - MINING RIGHTS ONLY S.R.O. - SURFACE RIGHTS ONLY M.+ S. - MINING AND SUHrACE RIGHTS Description Order No. Date Disposition F de PARK RESERVE.N47/83 B /^r '?3 MRS " P 5 x' _ LJL Yty. APP' V - D U'NI K: Vv \^ ^t ^ U' ^J r 2-itH, ~~~""~~~,. h- - -, t -f r SCALE: f INCH ^ 40 CHAINS i DO C.'OOO *ooc 6OOO aooo ^,'-f^- ^f p s~ -ss-p^- X / Vt AREA O 200 0OO ' ' M 2000 (2 KM LOWRY LAKE MN.R. ADMINISTRATE SIOUX MINING DIVISION PATRICIA LOOK A.M. MAY P.M. LAND TITLES/ REGISTRY DIVISIOJI THUNDER BAY f Land ' 5t 0 00' Ontario Natura Resources Management Branch 52P03NW002B HEATHER LAKE aoo A*' A; t AJ V- FEBRUARY, 984. Numb* r G-207

43 LEGEND ' * f^^tf 88ft4* \gff42t j fgrs37 [737 ] 79/Jg^Z ] 79/393 j!" j ^ Wrj r*j^*j. L5^.'';ii^^*^'^, i-p s y i y p /\ J rg^^y f ** f * ^ I**M*J y HIGHWAY AND ROUTE No OTHER ROADS TRAILS SURVEYED LINES TOWNSHIPS. BASE LINES, ETC LOTS. MINING CLAIMS. PARCELS. ETC UNSURVEYED LINES LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC RAILWAY AND RIGHT OF WAY UTILITY LINES NON PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT DISPOSITION OF CROWN LANDS... J Q TYPE OF DOCUMENT PATENT, SURFACE b MINING RIGHTS.SURFACE RIGHTSONLY.., MINING RIGHTS ONLY LEASE. SURFACE Si MINING RIGHTS ".SURFACE RIGHTSONLY, ". MINING RIGHTSONLY.... LICENCE OF OCCUPATION...,,. ORDER-IN COUNCIL.... RESERVATION. CANCELLED,.,..... SAND* GRAVEL... SYMBOL 0... e Q H a V oc WOTf: MINING 93 vtstfd IN ORIGINAL 'ATENTtt ev THE LANDS ACT RSO I9TO CMAP 3*O St C 63. SUSStC REFERENCES WITHDRAWN FROM DISPOSITION K r-- vi M.R.O. - MINING RIGHTS ONLY S.R.O. - SURFACE RIGHTS ONLY M.* s. - MINING AND SURFACE RIGHTS Dncnpion Order No Oat* Dupotition Fi* ^H. " -r i- i- -A - c r ^ Y 2V, 3~? u ^ M. Ifo S7 PATRICIA " ~ MINING " " DV. M SCALE, INCH - 40 CHAINS o -ooo ;ooo 6OOO aooo O 200 METRES ooo KM 20OO (2 KM AREA AUGUST LAKE M.M.R. ADMINISTRATIVE DISTRICT SIOUX MINING DIVISION PATRICIA LOOKOUT LAND TITLES/ REGISTRY DIVISION THUNDER BAY 5 0OO * 4i ' ' 5f 000 Ontario Ministryof Natura Resources Land Management Branch HEATHER LAKE 20 HB93 Diu FEBRUARY, 904. G-I940

44 LEGEND 5 0 t ' HIGHWAY AND ROUTE No. OTHER ROADS TRAILS SURVEYED LINES- TOWNSHIPS, BASE LINES. ETC... LOTS, MINING CLAIMS. PARCELS, ETC UNSURVEYED LINES: LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC RAILWAY AND RIGHT OF WAY -i UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT DISPOSITION OF CROWN LAF TYPE OF DOCUMENT SYMBOL PATENT, SUR F ACE fc MINING RIGHTS SURFACE RIGHTS ONLY...-,...,...,.,, MINING RIGHTS ONLY M...,., C LEASE,SURFACE A M'NINC RIGHTS S ".SURFACE RIGHTS ONLY...^...^...-. H ", MINING RIGHTS ON L Y... Q LICENCE O^ OCCUPATION ^. T ORDER-IN-COUNC'L......, ^...^.. OC RESERVATION...^...^, ^... Q CANCELLED......^...,....,......,.! SAND S; GRAVE! -...,. NOTE' MMNG RI ~ NTS!K PABCt.S ^ - "F ^ " T J' "c, r r ^ C M A v f, 93 V E S ^ E r tv O P i C i N A L. F A T E ^ * t i f v ' M? f",'t C LANDS AC' R S. O 9.'O C H i-.* 3 c?; S- C ST, f, ^ Bf L ' ' E FER E N C E S AREAS Wf M.R-0. - MINING RIGHTS ONLY S.R.O. - SURFACE RIGHTS ONLY M.+ S. -MINING AND SURFACE RIGHTS Dmcription Oroer No. O^'-f Dtipoftton Fie T^ MIN'Nu t, ir, f: i- dn s-cr L-':-ti.rr 7/87 ft, t a '*"'f,*n, Lyf^ tftite *^(uy^ly^t^~^^"v' SCALE: INCH * 40 CHAINS L ""t gj t"~t!-^iki ' j"~" -2fj f"" WrSCii j'^^t' U t i 9'**?t j w/ifj \9ifft* j * 9/9 f J *iim 9, r-\ \ gvotfo! I ' ' ' ^ -X/ Ti Fn* " ~ "'^V~7 r* ^"AJJ* "T-^fc^?! t/0 / F EET O OO 4OOO eooo ^, woo O 2QO OOO METRES M KM' AREA t LJ t A F"*k L? It E i ri A r L..N.R. ADMINISTRATIVE DISTRICT 2SOO 52 KM FINING DIVISIOI* 5! ' 44' i' " f i w ^- \ 9/34*9 " ^ ", f- - s. *w*^-* ^/croevv 4/VC5 43' 42' 4,' 40' 39' 38' 3?' ^ 36* 35' ! J^ j ''vf^ -' f LAftD TITLES/ REGISTRY DIVSiOK ^ KENORA {PATRICIA PORTION/THUNDER Ministry of Natura Resources uniario... ; Land M^nage-nent Branch 52P83NWa HEATHER LAKE ^^"^ i Oit * PESaUAfY, G /"*\ f\ f - i Q Pi I C/L.V-

45 LEGEND SO 3. 5 E N( PORTION OSNABURGH LAKE G HIGHWAY AND ROUTE No OTHER ROADS TRAILS - SURVEYED LINES ' TOWNSHIPS, BASE LINES. ETC LOTS, MINING CLAIMS. PARCELS. ETC UNSURVEYED LINES LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC. RAILWAY AND RIGHT Of WAY UTILITY LINES NON-PERENNIAt STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT 2 '; M DISPOSITION OF CROWN LANDS TYPE OF DOCUMENT SYMBOL PATENT, SURFACE ft MINING RIGHTS ,... *.SURFACE RIGHTSONLY... O.MINING RGHTSONLY.^...,... O Os r oo'jrgh indian :9M, 5 LEASE, SURFACE A MINING RIGHTS B ".SURFACE RIGHTS ONLY...,...,... B ".MINING RIGHTSONLY...^...,,.,-.,^,. U LICENCE OF OCCUPATION..^...,..^...,.^.,..... V OROER-IN-COUNCIL...,... OC RESERVATION..., CANCELLED,...,... Rese r, c. t -' Caron SAND A GRAVEL._...,... (J) NOTE: MINING RIGHTS IN PARCELS PATENTED PRIOR TO MAY G. 93, VESTED IN ORIGINAL PATENTEE *V THE PUBLIC LANDS ACT RS O 97O, CHAP MO, SEC S3. SUBSEC oo REFERENCES CM i O LU No 63 B? W,0 +H7M '-S \, y / J o LjJ VVITHDRAWN FROM DISPOSITION M.R.O. - MINING RIGHTS ONLY S.R.O. - SURFACE RIGHTS ONLY M.+ S. - MINING AND SURFACE RIGHTS Description Order No. D*tt DtfKMition Fi* CtPBOESCRVE (47/9^ 8/2S/85 MBS 89 i DISPOSITION Bt EXPL^SATtWr LICENCE Of i C "i/ tti :n QVL- abbl* TO MINIM s o tr! i r ' f i2f3z\ *i! 974*08 rr^ - Ct ^ O -J PATRICIA *2* qtf8)t. iz9i3 j H28JQ \ f^vf/ ~. '^iif'' ^L \f^'ffo\9f ~~' "T" i T ne M V "t T- i 7-H4. FLOODING F oo ding rights on Lake St. Joseph to Contour 230 ' to 2927 i L? TTVfi/! fr**36 i?rvtf3f *444Z Uti V Ontario Hydro. L.O. 865Z. Pan Y4I-9. Fies 99322, SCALE: INCH = 40 CHAINS T f V *- 0.T. ^ _ t f f f f y J \ 7 f ^ T J tt 7 f r r ^ '.T/TTI ^^ - ~ i-^^ - ^ --t -T---T---r ' ' T h i roiti^i. i \4tto, *v{^ ftf ' *il*- *fji^jih^i?i***?-l*?h 0 r \ r r r r!!5 M -J F E tt O 20O METRES AREA O IOOO 2OOO WOO 6OOO BOOO IOOO i KM' 300O (2 KM: CARON LAKE M4M / M.N.R. ADMINISTRATIVE DISTRICT SIOUX MtNUfG DIVISION LOOKOUT PATRICIA LAND TITLES/ REGISTRY DIVISION KENORA (PATRICIA PORTION)/THUNDER BAY n3 M ' 5I 000 Ontario Ministryof a Natura Resources Land M*na9*ment Br.nch ac s S2P03N*M2B 2.8B44 HEATHER LAKE 230 GREENBUSH LAKE G-2054 Oat* FEBRUARY, 984 G-I984

46 ro * G O o O o o GREEN BUSH LAKE G- V* V 03 C H :o O O o. x* w. r~ > 7Z m o J. (J) 0 ru O) UJ o DAWN LAKE G-28 Q JJ ^ -^ 0) 0) ~ CO "^ -J 0 ^ W c: - o) - o (D 0 en () - Z S J-' * i i t m rf-^ 2 3 C/) ±2 _ i -o H S m O g o x > 9 t, P v " w o J* ui m x --\ w GO -o O GO O DO O S -n ^ 00 - o to O '^ OD OD 00 A rn ^ k y* *- JP^f * J3L * \z# vi **** o CO

47 LEGEND \JJ.V/!y W 4St28-t Iif2t\ vafz,9jzy^ V7o 90 0 OC HIGHWAY AND POUTF No OTHER ROADS TRAILS SURVEYED LINES TOWNSHIPS. BASE LINES, ETC. LOTS, MINING CLAIMS, PARCELS, ETC UNSURVEVED LINES LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC RAILWAY AND RIGHT OF WAY UTILITY LINES NON-PFRfNNIAL ST^fcAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORF L INT MARSH OR MUSKEG MINES TRAVERSE MONUMENT DISPOSITION OF CROWN LANDS TYPE OF DOCUMENT SYMBOL PATENT SURFACE 8* MINING RIGHTS...,.. 9.SURFACE RIGHTSONLY..., MINING RIGHTSONLY...,... Q LEASE.SURFACE 8. MINING RIGHTS , - B ".SURFACE RIGHTSONLY... B ". MINING RIGHTSONLY... B LICENCE OF OCCUPATION... T ORDER-IN-COUNCiL,...,...,.....,... OC RESERVATION......,... CANCELLED,._...,.-,..-,...^.. SAND ft GRAVEL...,... 0 UtO).It ~ -~~ 2202/2/0 r NOTE; MINING RIGHTS IN PARCELS PATENTED PRIOR TO MAY VESTED IN ORIGINAL PATENTEE BV THE PUBLIC LANDS ACT RSO 970 CHAP 3HO. SEC 63 SUBSEC REFER ENCES AREAS WITHDRAWN FROM DISPOSITION M.R.O S.R.O. M,-t S VINfjG RIGHTS ONL^ SUPF ACE RIGHTS ONLY - :.".IMNG AND S, ^^ACE RIGHTS Description Order No Date Disposnion Fie NOV0987 PATRICIA MfWtWS SCALE: INCH = 40 CHAINS O 000?OOO 4OOO 6OOO aooo O 200 METRES 0OO KM 20OO (2 ^M AREA GREENBUSH LAKE M.N R ADV.INSTRA7IVE DISTRICT SIOUX LOOKOUT MINING DIVISION PATRICIA LAND TITLES/ REGISTRY DIVISION THUNDER BAY Land OC' Ontario Management Branch HEATHER LAKE 250 BCh 50690, Dan FEBRUARY, 984 N umbr G-2054

48 H) 0) O -f w ' ^i * o " * * a. 5 ACHAPI LAKE G-920 o? t? O C S. j* Tt t * *s -MINING A Z O CO c D T O m 3 O x 0 to i3 -SURFACE 30 Q X - CO O Zrir *- MINING - JU C x H to O zf- * 33 m g s ITHDRAW Z n X O g CO T) O to H O Z a, m t -^ B' * n m n. 2 O rn o ;o m r m m o i ro o o* O! 3 m x rn o i ro o 0 ro OD to BEAVIS LAKE AREA G-952 ni CD to o CD? r ro o O) (D D) w p- 3. O ^ W c S 5 s *^ S a? s 3 0 -j 5 TJ S CO S O 3, m ^ ^ z: D x s O S O 5 3!C ^ - s i > - C 2 " 2 O S 5 SI m 3 Q m r^ o M O Vt m H a m o z o x o I z to - o- z 'n <0 "3s H S O 5S 'SS 8? o x O r- m H o - ^ m c z n 5 6 z i 8 X m o 2 II O v*!i S 2m o r TJ H m Z Q m O O C m Z M i CO 9 O 00 O m 3) t/j m S O z c z m z -t S S O 30 jn -n Z C w 30 m c. r" Z S CO OD O m fi. o rn Q Q w x Z 5? O s? m i' O C V) z o O z O 5 o 5 8 O o S o Si H m S o? x > V) in 2 H * 3^5 m r ^ z z ** z m g > CO O r- 30 ^ o d x O -n 2^ 2 Pg C j: w O C H 3 O Q y! i i^ w S sarf ~ (rt " Z - Z L. ci OD m z o > 5? w m r~ W S2 rn - m T) Cf s 2 w m o c 5 3D > O X 3 g 0 S tn O O H m Z o S o m

49 5I 000' RIACH LAKE AREA- G JO 90?5' n 5 000' 59 HIGHWAY AND ROUTE No OTHER ROADS LEGEND TRAILS SURVEYED LINES' TOWNSHIPS. BASE LINES. ETC LOTS, MINING CLAIMS PARCELS. ETC UNSURVEYED LINES LOT LINES PARCEL BOUNDARY MINING CLAIMSETC RAILWAY AND RIGHT OF WAY UTILITY LINES NON PERENNIAL STREAM F LOCOING OR FLOODING RIGHTS SUBDIVISION OR COMPOS! T E PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT DISPOSITION OF CROWN LANDS TYPE OF DOCUMENT SYMBOL PATENT SURF ACE i MIVNu SURFACE RIGHTS 58 MINING RGHTSONL v LEASE SURFACE S MINING RIG ".SURFACE RIGHTSONLt ", MINING RIGHTS ONL v LICENCE OF OCCUPATION ORDER-IN COUNCIL RESERVATION m B a v oc CANCELLED.... SAND S. GRAVE L e O o OJ o 5 7 IT) O (\J CD NOTE MINING R i r, m s s p ARCi.s "A T trv T ED 'Ri o P T o M A v e 93 VESTfrD 'N O"r,iSA, t-attntee B* THE PUBLIC LANDS ACT PSO -a'o C^A" 3BC SEC 6J SUBSEC ' REFERENCES AREAS WITHDRAWN FROM DISPOSITION < UJ o: i < UJ o: M.R O. SRO MINING RIGHTS ONLV s^h^act MIGHTS o f *L Y M - S YiNV.: AM[J S- Hi A. r H'GH T S D**cription Ora*' No Da- Diipotmon Fie UJ UJ S U hji o: O o Z2±. f 56 Z) 00 -z. UJ UJ o: (S- (S Zf '76 : B O PATRICiA WINING prv. " IQ B i IV o if, 55 A.M. JIJH P.M. SCALE INCH ^ 40 CHAINS O OOO?OOO 4OOO r^ooc BOOO D METRLS 2QQ i OOO "M 54 AREA PASHKO KOGAN LAK MN.R. ADMINISTRATIVE DISTRICT SIOUX LOOKOUT MINING DIVISION PATRICIA LAND TITLES/ REGISTRY DIVISION THUNDER BAY ' Ontario Mtnistrycf Natura Resources Land Management Branch 52Pe3NW802* HEATHER LAKE 270 MCCREA LAKE AREA- G-220 BCh O " MARCH, 984 N v G-265

50 EAST PASHKO LAKE PROPERTY Terrain Cearance Line Spacing TOTAL MAGNETIC FIELD 000 gammas 250 gammas 50 gammas 0 gammas 00 meters 00 meters GREENBUSH LAKE PROPER? ST. JOE CANADA INC. AIRBORNE MAGNETIC SURVEY TOTAL MAGNETIC FIELD PASHKO, EAST PASHKO ft GREENBUSH LAKE PROPERTIES NTS N0 52J;6 DRAWING NO A - A~730 ~ SCALE : 0,000 DATE December 987 "ERRAQUEST LTD CM en in in ^ en PASHKO LAKE PROPERTY PB3NWei02ia HEATHER LAKE 280

51 2.0S44 ST. JOE CANADA INC Terrain Cearance Line Spacing... LEGEND 00 meters 00 meters AIRBORNE MAGNETIC SURVEY TOTAL MAGNETIC FIELD TOTAL MAGNETIC FIELD 000 gammas 250 gammas 50 gammas 0 gammas PASHKO RAPIDS Caron Lake, Ontario N.T.S. NO 520/ DRAWING NO. A P03NW HEATHER LAKE 290 SCALE :0,000 TERRAQUEST LTD. I'ORONTO. CANADA DATE December 987

52 --*- CM CO ^ [0 tn to in in in 00 O) Q ^ CM CO ^ in if) to to o) (o CD in tor- (O C0UD 004 JEMIMA NORTH 0D3 JEMIMA LAKE in to r*:. CO O Terrain Cearance Line Spacing.. LEGEND TOTAL MAGNETIC FIELD 000 gammas 250 gammas 50 gammas 0 gammas 00 meters 00 meters ST. JOE CANADA INC. AIRBORNE MAGNETIC SURVEY TOTAL MAGNETIC FIELD Webb Lake Project N S NO 5 2 O 52 J/ 6, 52/3 DRAWING NO A ^3-5PP03NW ieS*4 HEATHER LAKE 300 TERRAQUESr HI). S(;ALt 0,000 [)ATt J a n 'a, y 988

53 in to to to 008 LOWRY LAKE 4- CSI r* CO r- in r- CO r- O) r* o CO CO CO CM s. OT^ifV'o^ 0 o tn CD co en -t O) cm jn^^ 005 FRAIN LAKE Terrain Cearance Line Spacing... LEGEND TOTAL MAGNETIC FIELD 000 gammas 250 gammas 50 gammas 0 gammas 00 meters 00 meters ST. JOE CANADA ING. FRAIN LAKE fc LOWRY LAKE Webb Lake Project N T h Nt 52P/4 o Nt A Si. A L :0,000 JTMRAQUESr LW. January 9S8 52P03NW HEATHER LAKE 30

54 -. -*.. -t.,-,- ^. - v; i*. ' *-;- vhr ; -'' "- c - :- S --./.. -.-,A' -J i w :-....,. '"^^- i-gif'-**.''''' 33S"3'/--' -^- ':-"'v. ''^^^v-.""''''^r;'i^"' ' i '*' '^^fx '', 'fyf ^- y-'^'-'-^;. ; -'gr^."'^ "M:. r?^^vv^'if '/ : - ' ^-'-' ^^^-/'; '^;^^'^-, \-.- ' f-^t.---'f :--*te--- J :- ^--, A - Terrain Cearance Line Spacing LEGEND TOTAL MAGNETIC FIELD 000 gammas 250 gammas 50 gammas 0 gammas 00 meters 00 meters AUGUST WEST 0 2, 0844 ST, JOE CANADA INC. AIRBORNE MAGNETIC SURVEY TOTAL MAGNETIC FIELD AUGUST CREEK 4 AUGUST WE:ST PROPERTIES 52P/4 '- "- A O. 5 - December 987 CM en

55 IRON FALLS PROPERTY AUGUST NORTH PROPERTY N ; Terrain Cearance Line Spacing.. LEGEND TOTAL MAGNETIC FIELD 000 gammas 250 gammas 50 gammas 0 gammas 00 meters 00 meters ST. JOE CANADA INC. AIRBORNE MAGNETIC SURVEY TOTAL MAGNETIC FIELD IRON FALLS 4 AUGUST NORTH PROPERTIES Webb Lake Project NT.S NO 5 2 P/4 DRAWING G " S(:ALr :0,000 DATE January 98G TERRAQWST LTD. 2.0B44 HEATHER LAKE 330

56 (P (O S (p Terrain Cearance Line Spacing LEGEND TOTAL MAGNETIC FIELD 000 gammas 250 gammas 50 gammas 0 gammas 00 meters 00 meters ST. JOE CANADA INC. AIRBORNE MAGNETIC SURVEY TOTAL MAGNETIC FIELD VALLAS LAKE PROPERTY Webb Lake Project f NTS NO 53P/3 NO A it.al 0,000 January HEATHER LAKE

57 EAST PASHKO LAKE PROPERTY Terrain Cearance Line Spacing LEGEND VERTICAL MAGNETIC GRADIENT 00 gammas/meter 025 gammas/meter 0.05 gammas /meter 00 meters 00 meters GREENBUSH LAKE PROPER! ,0844 ST. JOE CANADA INC. AIRBORNE MAGNETIC SURVEY VERTICAL MAGNETIC GRADIENT Cacuated From Tota Fied PASHKO, EAST PASHKO a GREENBUSH LAKE PROPERTIES SCALE :0,000 DATE December 987 TERRAQUEST ff). PASHKO LAKE PROPERTY in OD r- cocn NTS NO 52 J/ 6 DRAWING NO A~ PP83MW00E0 E,'0844 HEATHER LAKE 350

58 ^ m CD csj on ST. JOE CANADA INC. Terrain Cearance Line Spacing... LEGEND 00 meters 00 meters AIRBORNE MAGNETIC SURVEY VERTICAL MAGNETIC GRADIENT Cacuated From Tota Fied VERTICAL MAGNETIC GRADIENT gammas/meter.500 gammas/meter.00 gammas/meter.025 gammas/meter PASHKO RAPIDS Caron Lake. Ontario NTS NO 520/ DRAWING NO A-730.2~2 52P03NW002B P.0B44 HEATHER LAKE 3G0 SCALI :0,000 DATE December 987 TERRAQIJEST LTD.

59 CO O) Q i CM CO If) to 03 CD (D LO U3 cor- COCO 004 JEMIMA NORTH 003 i t!;f^m^k**f;3^sjjm MKj ; JEMIMA LAKE CD LDCDr^OOO) O r- co OT o co ' CsJ CM CsJ CO (M (S) in CO CJ O) O CO CO CXJ oo co -*r no on Terrain Cearance Ltne Spacing LEGEND VERTICAL MAGNETIC GRADIENT -, Qf, gammas; meter i Qd gammas/meter O ;'-~. gammas/metei O j^ gammas/meter 00 meters too meters ST. JOE CANADA inc RBORNE MAGNETIC SURVEY Vf- RMTAI. MAO M F T M JEMIMA LAKE ci JEMIMA NORTH Webb Lake Project 370

60 LOWRY LAKE 0D6 005 FRAIN LAKE 005 Terrain Cearance Line Spacing LEGEND VERTICAL MAGNETIC GRADIENT gammas- meter ~.500 gammas/meter 00 gammas/mete 025 gammas/meter 00 meters 00 meters ST. JOE CANADA INC AIRBORNE MAGNETIC SURVEY VERTICAL MAGNETIC GRADIENT C die u a ted From Tota Fied FRAIN LAKE S LOWRY LAKE Webb Lake Project 52P/4! TERRAOI '/-X/ m 7 3 O 4 January

61 SF-C.REEK PROPERTY Terrain Cearance Line Spacing LEGEND VERTICAL MAGNETIC GRADIENT gammas/meter gammas/meter.500 gammas/meter.00 gammas/meter 00 meters 00 meters AUGUST WEST PROPERTY ST JOE CANADA inc. 0 0 AIRBORNE MAGNETIC SURVEY VERTICAL MAGNETIC GRADIENT Cacuated From Tota Fied AUGUST CREEK S AUGUST WEST PROPERTIES 52P/4 0,000 A * in en CM m -h C\J Ln to r-- (c en o ^ 390

62 IRON FALLS PROPERTY AUGUST NORTH PROPERTY cp Terrain Cearance Line Spacing. LEGEND VERTICAL MAGNETIC GRADIENT gammas/meter ~.500 gammas/meter.00 gammas/meter 025 gammas/meter 00 meters 00 meters ST. JOE CANADA INC. AIRBORNE MAGNETIC SURVEY V'FRTICAL MAGNFTIC CPAni-NT ("i*f:ufated Frrirn Tct;i! F icu! IRON FALLS S AUGUST NORTH PROPERTIES i Webb Lake Project 77A'A'or;.s HEATHER.AKF 400

63 (P Terrain Cearance Line Spacing.. LEGEND VERTICAL MAGNETIC GRADIENT 2,500 gammas/meter ~ 500 gammas/mete; 00 gammas/meter 025 gammas/meter 00 meters 00 meters ST. JOE CANADA INC. AIRBORNE MAGNETIC SURVEY VERTICAL MAGNETIC GRADIENT Cacuated From Tota Fird VALLAS LAKE PROPERTY Webb Lake Project 3844 HEATHFR LAKE 40 rm. January 988

64 EAST PASHKO LAKE PROPERTY Terrain Cearance Line Spacing LEGEND TOTAL FIELD STRENGTH (Contours 50 H 0 0'o 00 meters 00 meters QUADRATURE (Profies- Norma Sope Reverse Sope GREENBUSH LAKE PROPERTY ST. JOE CANADA INC AIRBORNE VLF-EM SURVEY CONTOURS OF TOTAL FIELD STRENGTH PROFILES OF QUADRATURE 52 J/ PASHKO, EAST PASHKO A GREENBUSH LAKE PROPERTIES TERRAQ'EST LW, :."ia v, N-. A t December f ' C\J LO in cn C\J PASHKO LAKE PROPERTY iooi VLF Transmitter NAA Cuter, 24.0 khz Aztmutn HEAIHER LAKE 420