JERVOIS MINING N.L.																			JERVOIS MINING N.L.														
BEACONSFIELD PROJECT AIR CORE DRILL LOG																			BEACONSFIELD PROJECT AIR CORE DRILL LOG														
																																	
COLLAR CO-ORDS:			AGD:	5436943	mN	481008	mE		LOCATION:			Barnes Hill	HOLE NO:			S023			COLLAR CO-ORDS:		AMG:	5436943	mN	481008	mE	LOCATION:		Barnes Hill		HOLE NO:		S023	
ELEVATION:				99.00	mAHD				START DATE:			Feb/Mch 1997	FINAL DEPTH:			16m			ELEVATION:			99.00	mAHD			START DATE:		Feb/Mch 1997		FINAL DEPTH:		16m	
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	    Soil		Orange brown sandy with w serp and saprolite contamination.							1.64		191	0.585	0.024				0-1														
1	2												170						1-2														
2	3	Limonitic clay		Orange brown.							5.26		107	0.205	0.024				2-3														
3	4	Limonitic clay		Orange brown.							9.08		69	0.335	0.020				3-4														
4	5	Saprolite		Med brown smectitic & orange brown limonitic clay tr cream black smectitic flecks.							8.88	damp	268	0.760	0.055	52.22	19	0.49	4-5	0.87	-5	-0.01	15510	-5	1260	-5	7	242	251				
5	6	Saprolite		Green grey light brown smectitic sl mottled clay.							6.40	damp	644	1.11	0.210	42.47	23	1.18	5-6	1.40	-5	0.01	16100	-5	9870	-5	-5	120	226				
6	7	Saprolite		Medium brown and dark green black smectitic clay minor dark w serp chips.							3.88	damp	591	1.58	0.140	34.79	17	2.03	6-7	0.74	-5	0.03	18710	-5	6340	-5	-5	78	335				
7	8	Saprolite		Pale grey green brown smectitic clay minor grey green w serp chips.							5.12	damp	232	1.60	0.044	13.06	16	3.60	7-8	10.51	-5	0.03	3970	-5	7770	-5	6	37	315				
8	9	Saprolite		Light brown orange brown smectitic clay with white magnesite nodules.							4.80	damp       ? 20% magnesite	100	1.22	0.050	10.47	14	4.08	8-9	10.71	-5	0.03	2800	-5	6690	-5	-5	39	243				
9	10	Saprolite		Light brown orange brown pink dark green mottled smectitic clay.							5.04	damp       ? 10% magnesite	111	1.09	0.048	9.07	14	2.91	9-10	12.16	-5	0.02	2270	-5	10910	-5	-5	38	234				
10	11	Saprolite		Medium brown pink dark green mottled smectitic clay.							8.94	damp	97	0.835	0.050	15.16	17	2.29	10-11	9.81	-5	0.03	6280	-5	9270	-5	6	42	168				
11	12	Saprolite		Med brown pink dk green mottled smectitic clay some dk green soft w serp chips.							4.72	damp         tr magnesite	79	1.31	0.055	14.62	15	3.85	11-12	6.30	-5	0.04	11700	-5	6750	-5	7	42	261				
12	13	Saprolite		Med brown pink dk green mottled smectitic clay some dk green soft w serp chips.							8.48	damp         tr magnesite	59	1.07	0.020	10.99	10	6.76	12-13	6.54	-5	0.23	6530	-5	7040	-5	6	33	274				
13	14	Saprolite		Med brown pink dk green mottled smectitic clay min pale grey green w serp chips.							7.00	damp	99	1.12	0.032	10.48	10	10.24	13-14	3.88	-5	0.09	7750	-5	4010	-5	-5	40	190				
14	15	Weathered serpentinite		Pale grey green clayey minor medium brown smectitic clay tr pale grey asbestos.							7.32	damp	112						14-15														
15	16	Fresh serpentinite		Pale grey green sl weathered some dark green hard chips minor clay.							4.80	damp	409						15-16														
16	17																		16-17														
17	18			Hole completed at 16m															17-18														
18	19																		18-19														
19	20																		19-20														
20	21																		20-21														
21	22																		21-22														
22	23																		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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