Apella Stakes Magnetite Bay Iron Deposit Interest

16 Jun 2009 - 6:30am

Apella Resources Inc.(TSX.V: APA); (Frankfurt Symbol: NWN) and its Board of Directors are pleased to announce the acquisition of 19 mineral claims which when finalized will include a 2.4 kilometer strike length of the Magnetite Bay Iron Deposit.  The deposit is close to existing mining-rail-hydroelectric infrastructure being about 11 miles (18 kms) east of Chibougamau, Quebec, only 2 kilometers from a major logging route and 320 kilometers from the La Baie seaport on the Saguenay. Magnetite Bay is 6.8 miles (11 kms) from Apella’s Lac Dore Iron-Vanadium-Titanium interests.

The Magnetite Bay deposit had been entirely controlled since 1961 by Campbell Resources until most of it recently came open.  It was last drilled for its iron potential in the early 1960’s decade.  Magnetite-rich layers in the Layered Series of the Lac Dore Anorthosite Complex occur in a steeply dipping continuous zone that is about 50 to 70 metres thick.  The deposit on Apella’s claims was initially tested by trenches and 37 drill holes (20,774 ft or 6,332 m) on 10 sections that were spaced about 820 ft (250 m) apart.  In 1974 the Quebec Department of Mines essentially confirmed by re-analysis Campbell Chibougamau Mines assays done in the 1960’s.  A resource was estimated by Campbell Chibougamau Mines Ltd in 1975 for the Ferchib South Zone.  The resource portion under the Apella claims was estimated to be 92.8 million tons at 26% iron, and 1% titanium. Initial metallurgical testing in 1974 by the Quebec Bureau of Mines suggested 31.75 million tons of concentrate could be made containing 66.7% iron and 1% TiO2..  Qualified persons have not done sufficient work to classify the above historical estimates as current mineral resources or recoveries and Apella is not treating the historical estimates as current mineral resources or recoveries. The historical estimates should not be relied upon.

Apella sees this deposit acquisition as part of its larger plans for iron-vanadium-titanium developments in the Chibougamau region.  Improvements in exploration, geological and metallurgical technologies and techniques in the past 40 years can now be applied to the Magnetite Bay deposit for the first time.  Detailed magnetometer surveys, surface sawn channel sampling and inclined drill holes will better define geochemical variations in the steeply dipping magmatic- layered magnetite-rich units.  In addition to its iron potential, other elements such as vanadium will be systemically explored for in the deposit.  The Magnetite Bay deposit occurs in more magnesium-rich rocks than the other stratiform iron deposits in the Lac Dore Complex.  Sulfide occurrences have also been noted in the historical drilling.  Both the higher magnesium host rocks and the sulfide occurrences are favourable for exploring the potential for platinum group element (PGE) mineralization.

For reference purposes only, Apella presents the following table detailing some of the historical diamond drill iron assay results from the claims that Apella has acquired.  Average iron grades were calculated by Robert D. Stewart using data from the original Campbell Chibougamau Mines assay tables and applying a 15% iron cutoff for determining the start and end of intersections.  Note that most holes were drilled vertically in sub-vertically dipping formations so true widths for these intersections cannot be determined at this time. 

 

 

 

TABLE 1:

Weighted Averages of Original Campbell Chibougamau Mines Ltd. Assays for Drill-Hole Intersections Determined Using a 15% Iron Cutoff (Robert D. Stewart, P.Geo.)

 

Project Name

DDH

Year Sampled

From (ft)

To (ft)

Length (ft)

Length (m)

Fe %

Owner

Magnetite Bay

FS-41

1966

6

607

601

183.4

32.9

Apella

Magnetite Bay

FS-45

1966

10

585

575

175.2

32.7

Apella

Magnetite Bay

FS-51

1966

16

606

590

179.9

30.9

Apella

Magnetite Bay

FE-6

1965

15

550

535

163.1

27.2

Apella

Magnetite Bay

FS-47

1966

42

570

528

161.0

27.3

Apella

Magnetite Bay

FS-42

1966

3

601

598

182.3

23.8

Apella

Magnetite Bay

FE-7

1972

5

548

543

165.5

23.7

Apella

Magnetite Bay

FS-52

1966

27

448

422

128.5

27.9

Apella

Magnetite Bay

FE-14

1965

3

550

547

166.8

21.3

Apella

Magnetite Bay

FE-3

1965

12

507

495

150.9

22.5

Apella

Magnetite Bay

FS-43

1966

3

657

654

199.4

15.8

Apella

Magnetite Bay

FE-1

1962

12

390

378

115.2

26.5

Apella

Magnetite Bay

FE-17

1965

225

500

275

83.8

32.2

Apella

Magnetite Bay

FE-13

1965

339

644

305

92.9

24.3

Apella

Magnetite Bay

FE-11

1965

50

299

249

75.9

28.5

Apella

Magnetite Bay

FS-56

1966

250

475

225

68.6

30.6

Apella

Magnetite Bay

FE-18

1965

255

500

245

74.7

26.9

Apella

Magnetite Bay

FE-18

1965

6

207

201

61.1

31.4

Apella

Magnetite Bay

FE-10

1965

158

394

236

72.0

26.0

Apella

Magnetite Bay

FS-64

1966

55

298

244

74.2

24.5

Apella

Magnetite Bay

FE-13

1965

50

266

216

65.7

22.7

Apella

Magnetite Bay

FS-66

1966

135

286

151

46.0

32.3

Apella

Magnetite Bay

FS-43

1966

160

300

140

42.7

28.3

Apella

Magnetite Bay

FS-52

1966

500

606

106

32.3

33.5

Apella

Magnetite Bay

FE-5

1965

511

700

189

57.7

16.7

Apella

Magnetite Bay

FS-66

1966

18

113

95

29.0

31.4

Apella

Magnetite Bay

FE-5

1965

950

1085

135

41.2

19.3

Apella

Magnetite Bay

FS-59

1966

75

210

135

41.0

17.4

Apella

Magnetite Bay

FE-17

1965

100

172

72

22.0

30.3

Apella

Magnetite Bay

FE-15

1965

250

370

120

36.6

16.7

Apella

Magnetite Bay

FS-59

1966

350

414

64

19.5

30.6

Apella

Magnetite Bay

FS-44

1966

398

471

73

22.3

23.6

Apella

Magnetite Bay

FS-69

1966

3

62

59

18.0

26.2

Apella

Magnetite Bay

FS-57

1966

10

67

58

17.5

21.5

Apella

Magnetite Bay

FE-4

1965

379

437

58

17.7

19.9

Apella

Magnetite Bay

FE-8

1965

60

117

57

17.3

20.2

Apella

Magnetite Bay

FS-44

1966

8

50

42

12.8

26.3

Apella

Magnetite Bay

FE-15

1965

475

519

44

13.4

23.2

Apella

Magnetite Bay

FS-57

1966

375

414

39

11.9

24.7

Apella

Magnetite Bay

FE-2

1965

36

72

36

11.0

25.7

Apella

Magnetite Bay

FE-2

1965

177

226

49

14.8

18.7

Apella

Magnetite Bay

FS-43

1966

325

350

25

7.6

32.8

Apella

Magnetite Bay

FE-32

1966

140

182

42

12.7

19.2

Apella

Magnetite Bay

FE-5

1965

409

439

31

9.3

18.0

Apella

Magnetite Bay

FS-44

1966

580

602

22

6.6

24.8

Apella

Magnetite Bay

FE-4

1965

100

127

27

8.4

19.4

Apella

Magnetite Bay

FS-43

1966

125

150

25

7.6

20.3

Apella

Magnetite Bay

FE-4

1965

52

83

31

9.3

16.5

Apella

Magnetite Bay

FE-43

1966

50

75

25

7.6

19.4

Apella

Magnetite Bay

FS-43

1966

6

25

19

5.8

20.8

Apella

Magnetite Bay

FS-64

1966

7

25

18

5.4

21.4

Apella

Magnetite Bay

FE-4

1965

476

501

25

7.5

15.1

Apella

Magnetite Bay

FS-44

1966

297

318

21

6.5

16.9

Apella

Magnetite Bay

FS-44

1966

125

141

16

4.7

21.7

Apella

Magnetite Bay

FE-15

1965

4

25

21

6.4

15.4

Apella

Magnetite Bay

FE-4

1965

4

19

15

4.4

20.5

Apella

Magnetite Bay

FS-42

1966

8

15

8

2.3

28.0

Apella

Magnetite Bay

FS-56

1966

570

576

6

1.9

26.0

Apella

Magnetite Bay

FS-44

1966

65

70

5

1.6

21.8

Apella

 

The Qualified Person for this news release is Robert D. Stewart, P.Geo.

Apella invites the public to visit its website at http://www.apellaresources.com or e-mail us at apella@apellaresources.com to be added to the Company’s e-mail list for press releases and updates.

ON BEHALF OF THE BOARD OF DIRECTORS OF APELLA RESOURCES INC.

“Patrick D. O’Brien”                            

Patrick D. O’Brien – Chairman

S.E.C. Exemption 12(g)3-2(b)  File No. 82-3822, Standard & Poors Listed, Dun & Bradstreet Listed                             

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