JERVOIS MINING N.L.																			JERVOIS MINING N.L.														
BEACONSFIELD PROJECT AIR CORE DRILL LOG																			BEACONSFIELD PROJECT AIR CORE DRILL LOG														
																																	
COLLAR CO-ORDS:			AGD:	5436919	mN	481202	mE		LOCATION:			Barnes Hill	HOLE NO:			S022			COLLAR CO-ORDS:		AMG:	5436919	mN	481202	mE	LOCATION:		Barnes Hill		HOLE NO:		S022	
ELEVATION:				102.00	mAHD				START DATE:			Feb/Mch 1997	FINAL DEPTH:			21m			ELEVATION:			102.00	mAHD			START DATE:		Feb/Mch 1997		FINAL DEPTH:		21m	
AZIMUTH:				0°					FINISH DATE:				LOGGED BY:			A.Jannink			AZIMUTH:			0°				FINISH DATE:				LOGGED BY:		A.Jannink	
DECLINATION:				90°					DRILLED BY:		Diamond Drilling (Tas) P.L.		PAGE:		1	OF	2		DECLINATION:			90°				DRILLED BY:		Diamond Drilling (Tas) P.L.			PAGE: 2	OF	2
 DEPTH(m)		DESCRIPTION										MINERALISATION		   ASSAY RESULTS					INTERVAL (m)	"ASSAY VALUES
IC587"										M275			
From	To										Kg		Mag Sus	%Ni	%Co	%Fe	ppmSc	%Mg		"Al 
%"	"As
ppm"	"Ca
%"	"Cr
ppm"	"Cu
ppm"	"Mn
%"	"Mo
ppm"	"Pb
ppm"	"S
ppm"	"Zn
ppm"	"SiO2
%"			
0	1	No sample																	0-1														
1	2	Hematitic clay		Red brown some pale green weathered serpentinite (?contamination).							7.84		253	0.280	0.013				1-2														
2	3	Hematitic clay		Medium brown to red brown sl pisolitic.							9.08		125	0.050	0.005				2-3														
3	4	Hematitic clay		Red brown pisolitic.							11.20		48	0.026	0.005				3-4														
4	5	Clay		Light brown indurated sl limonitic.							10.80		34	0.023	<0.002				4-5														
5	6	Limonitic clay		Pale orange brown tr pisolites.							9.00		21	0.040	0.005				5-6														
6	7	Limonitic clay		Pale orange brown tr pisolites.							8.64		39	0.060	0.006				6-7														
7	8	Limonitic clay		Pale orange brown tr pisolites.							7.04		28	0.130	0.014				7-8														
8	9	Limonitic clay		Mediium brown with flecks of cream  ?weathered serpentinite.							7.20		25	0.120	0.006				8-9														
9	10	Limonitic clay		Light brown minor medium brown.							6.94		29	0.220	0.011				9-10														
10	11	Limonitic clay		Light brown minor medium brown.							7.76		40	0.255	0.010				10-11														
11	12	Limonitic clay		Light brown minor medium brown.							7.50	damp	58	0.105	0.006				11-12														
12	13	Saprolite		Red brown smectitic clay minor flecks cream weathered serpentinite.							8.36	damp	162	0.160	0.048				12-13														
13	14	Saprolite		Pale to medium brown smectitic clay some pale to dark green laminated w serp.							5.92	damp	396	0.695	0.075	25.38	18	1.04	13-14	2.60	-5	0.04	17000	-5	3070	-5	7	472	155				
14	15	Saprolite		Medium brown smectitic clay some pale to dark green laminated w serp.							5.92	damp	133	1.30	0.105	22.80	18	2.28	14-15	2.99	-5	0.08	16300	-5	4900	-5	-5	239	305				
15	16	Saprolite		Pale to medium brown smectitic clay lesser cream weathered  serpentinite chips.							6.80	damp	265	0.855	0.080	16.72	11	4.78	15-16	3.77	-5	0.06	9360	-5	5470	-5	-5	171	374				
16	17	Saprolite		Pale to medium brown smectitic clay more pale grey green w  serp chips.							6.76	damp	505	1.22	0.055	15.56	7	7.88	16-17	0.64	-5	0.05	8060	-5	2300	-5	-5	57	631				
17	18	Saprolite		Pale to medium brown smectitic clay more pale grey green w  serp chips.							3.68	damp	257	1.48	0.040	14.44	7	9.88	17-18	0.59	-5	0.05	21400	-5	2620	-5	-5	49	407				
18	19	Saprolite		Red brown and pale grey green smectitic clay lesser pale grey green w serp chips.							5.32	damp	265	1.26	0.035	12.91	8	11.14	18-19	0.65	-5	0.04	19800	-5	2010	-5	-5	78	168				
19	20	Weathered serpentinite		Pale grey green chips with pale grey green clay.							12.84	damp            tr asbestos	194						19-20														
20	21	Weathered serpentinite		Pale grey green clayey chips some black fresh serpentinite.							2.20	damp            tr asbestos	294						20-21														
21	22																		21-22														
22	23			Hole completed at 21m															22-23														
23	24																		23-24																												
24	25																		24-25																												
25	26																		25-26																												
26	27																		26-27																												
27	28																		27-28																												
28	29																		28-29																												
29	30																		29-30																												
30	31																		30-31																												
31	32																		31-32																												
32	33																		32-33																												
33	34																		33-34																												
																																															
																																															
																																															
																																															
																																															
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
																		
										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