JERVOIS MINING N.L.																			JERVOIS MINING N.L.														
BEACONSFIELD PROJECT AIR CORE DRILL LOG																			BEACONSFIELD PROJECT AIR CORE DRILL LOG														
																																	
COLLAR CO-ORDS:			AGD:	5438892	mN	479946	mE		LOCATION:			Mt Vulcan	HOLE NO:			S017			COLLAR CO-ORDS:		AMG:	5438892	mN	479946	mE	LOCATION:		Mt Vulcan		HOLE NO:		S017	
ELEVATION:				56.00	mAHD				START DATE:			Feb/Mch 1997	FINAL DEPTH:			17m			ELEVATION:			56.00	mAHD			START DATE:		Feb/Mch 1997		FINAL DEPTH:		17m	
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		Red brown hematitic some pisolites.							1.00		423	0.120	0.010				0-1														
1	2	Hematitic clay		Red brown minor pisolites minor pale green w serp (contamination).							2.92		237	0.074	0.006				1-2														
2	3	Limonitic clay		Light orange brown.							3.90		80	0.080	0.006				2-3														
3	4	Limonitic clay		Light medium brown.							4.44		116	0.106	0.016				3-4														
4	5	Saprolite		Dark brown minor orange and green smectitic clay.							6.66	damp    1-2% magnesite	330	0.370	0.042				4-5														
5	6	Saprolite		Red brown with pale to dark green flecks smectitic clay.							6.60	damp	348	0.906	0.068	29.52	24	1.90	5-6	3.84	5	0.13	30210	9	2530	-5	-5	110	316				
6	7	Saprolite		Dark green brown orange mottled smectitic clay.							5.52	damp	567	1.10	0.200	26.35	20	2.20	6-7	3.49	-5	0.12	22800	9	6090	-5	-5	27	351				
7	8	Saprolite		Dark green brown orange mottled smectitic clay.							4.96	damp	701	1.02	0.124	31.74	21	2.13	7-8	1.92	5	0.10	19300	8	3690	-5	8	14	245				
8	9	Saprolite		Dark green brown orange mottled smectitic clay.							5.80	damp	690	1.09	0.082	29.43	21	2.38	8-9	1.98	9	0.12	22400	11	2970	-5	-5	-10	338				
9	10	Saprolite		Dark green grey speckled with pale green smectitic clay.							5.62	damp	260	1.50	0.074	24.15	17	4.07	9-10	2.63	-5	0.14	22000	10	3230	-5	-5	27	457				
10	11	Weathered serpentinite		Pale grey green mottled with cream flecks clayey.							5.68	damp	419	1.09	0.036	14.69	10	13.36	10-11	1.92	-5	0.05	12800	-5	2080	-5	-5	35	349				
11	12	Weathered serpentinite		Dark grey green lesser pale grey green sl smectitic clayey.							5.52	damp	258	1.21	0.058	19.30	14	6.07	11-12	3.11	-5	0.08	26400	9	4050	-5	-5	13	454				
12	13	Saprolite		Green brown smectitic clay with flecks of cream weathered serpentinite.							6.08	damp	296	1.58	0.070	24.81	24	3.77	12-13	1.40	-5	0.08	12800	12	3120	-5	-5	50	221				
13	14	Saprolite		Green brown smectitic clay with more cream weathered serpentinite.							4.56	damp	384	1.01	0.036	15.24	12	13.73	13-14	1.16	-5	0.05	9210	7	1970	-5	-5	40	181				
14	15	Weathered serpentinite		Pale grey green minor dark green grey clayey.							8.02	damp	312	0.790	0.024	11.60	9	16.75	14-15	1.26	-5	0.03	9810	-5	1820	-5	-5	30	207				
15	16	Weathered serpentinite		Pale grey green minor dark green grey clayey.							5.80	damp	208	0.902	0.028	11.34	11	16.30	15-16	0.82	-5	0.06	5490	-5	1400	-5	-5	26	126				
16	17	Weathered serpentinite		Pale grey green minor dark green grey clayey.							8.44	damp	226	0.722	0.040	12.72	10	16.18	16-17	1.64	-5	0.05	7490	6	1830	-5	-5	41	150				
17	18																		17-18														
18	19			Hole completed at 17m															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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