JERVOIS MINING N.L.																			JERVOIS MINING N.L.														
BEACONSFIELD PROJECT AIR CORE DRILL LOG																			BEACONSFIELD PROJECT AIR CORE DRILL LOG														
																																	
COLLAR CO-ORDS:			AGD:	5436967	mN	481417	mE		LOCATION:			Barnes Hill	HOLE NO:			S027			COLLAR CO-ORDS:		AMG:	5436967	mN	481417	mE	LOCATION:		Barnes Hill		HOLE NO:		S027	
ELEVATION:				80.00	mAHD				START DATE:			Feb/Mch 1997	FINAL DEPTH:			20m			ELEVATION:			80.00	mAHD			START DATE:		Feb/Mch 1997		FINAL DEPTH:		20m	
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	    Clay		Light brown tr pale green chips							6.08		100	0.160	0.009				0-1														
1	2												91						1-2														
2	3	Clay		Orange brown tr grey green sand/gravel							8.24		77	0.080	0.008				2-3														
3	4	Limonitic clay		Chocolate brown							7.08		55	0.095	0.006				3-4														
4	5	Limonitic clay		Light brown 							6.76		74	0.295	0.021				4-5														
5	6	Limonitic clay		Light brown tr boxworks							7.76		143	0.160	0.013				5-6														
6	7	Limonitic clay		Light brown some pink hematitic minor cream							7.68		112	0.125	0.008				6-7														
7	8	Limonitic clay		Pink hematitic 							6.98	2-3% magnesite	46	0.095	0.005				7-8														
8	9	Limonitic clay		Pink/light brown sl hematitic 							6.24	tr magnesite	63	0.170	0.010				8-9														
9	10	Limonitic clay		Light yellow brown							6.56		150	0.185	0.028				9-10														
10	11	Limonitic clay		Light brown minor pink sl smectitic							6.20		66	0.145	0.040				10-11														
11	12	Limonitic clay		Light brown pink sl smectitic							7.28		84	0.120	0.034				11-12														
12	13	Saprolite		Brown pink minor pale green with cream and grey chips							7.64	damp	110	0.310	0.065				12-13														
13	14	Saprolite		Medium dark brown smectitic with pale to dark green w serp chips							8.00	damp	154	1.02	0.075	19.32	23	4.03	13-14	5.36	-5	0.06	14810	-5	3400	-5	-5	197	194				
14	15	Saprolite		Grey green smectitic with cream white w serp chips							5.20	damp	200	1.81	0.140	24.59	21	3.06	14-15	1.53	-5	0.08	13600	-5	10400	-5	7	135	328				
15	16	Saprolite		Pale grey green smectitic and cream w serp chips							10.70	damp	133	1.16	0.055	18.45	24	7.88	15-16	2.47	-5	0.04	10800	-5	4310	-5	-5	330	234				
16	17	Saprolite		Pale grey green smectitic and cream w serp chips							5.84	damp	274	0.825	0.019	9.03	7	16.86	16-17	0.34	-5	0.02	2750	-5	2410	-5	-5	64	103				
17	18	Weathered serpentinite		Pale cream chips lesser grey green clay							5.68	damp	765	0.780	0.024	17.40	7	12.54	17-18	0.68	-5	0.02	4040	-5	1860	-5	-5	36	65				
18	19	Weathered serpentinite		Pale green cream clayey							6.84	damp	360	0.780	0.026	13.44	8	14.35	18-19	0.71	-5	0.03	5780	-5	1310	-5	-5	39	90				
19	20	Fresh serpentinite		Grey green hard chips minor clay							5.72	wet      tr asbestos	260	0.655	0.020	6.65	8	18.45	19-20	0.48	-5	0.02	3080	-5	839	-5	-5	38	77				
20	21																		20-21														
21	22			Hole completed at 20m															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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