JERVOIS MINING N.L.																			JERVOIS MINING N.L.														
BEACONSFIELD PROJECT AIR CORE DRILL LOG																			BEACONSFIELD PROJECT AIR CORE DRILL LOG														
																																	
COLLAR CO-ORDS:			AGD:	5439718	mN	479725	mE		LOCATION:			Scotts Hill	HOLE NO:			S005			COLLAR CO-ORDS:		AGD:	5439718	mN	479725	mE	LOCATION:		Scotts Hill		HOLE NO:		S005	
ELEVATION:				34.00	mAHD				START DATE:			Feb/Mch 1997	FINAL DEPTH:			27m			ELEVATION:			34.00	mAHD			START DATE:		Feb/Mch 1997		FINAL DEPTH:		27m	
AZIMUTH:				0°					FINISH DATE:				LOGGED BY:			A.Jannink			AZIMUTH:			0°				FINISH DATE:		0		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, pisolitic."							1.76		106	0.092	0.010				1-2														
2	3	Hematitic clay		"Brown red, pisolitic."							2.88		74	0.090	0.008				2-3														
3	4	Hematitic clay		"Brown red, less pisolitic more clayey."							3.10		54	0.140	0.016				3-4														
4	5	Hematitic clay		"Red brown, clayey, sl pisolitic."							1.84		67	0.134	0.020				4-5														
5	6	Limonitic clay		Light brown.							5.96		30	0.124	0.018				5-6														
6	7	Limonitic clay		"Light brown, tr sand."							3.72		25	0.092	0.034				6-7														
7	8	Limonitic clay		"Grey brown, tr pisolites."							5.86		28	0.226	0.320				7-8														
8	9	Limonitic clay		"Brown red, tr pisolites."							2.96		25	0.168	0.116				8-9														
9	10	Limonitic clay		"Red brown, sl hematitic."							2.80		21	0.148	0.054				9-10														
10	11	Limonitic clay		"Light brown, sl hematitic."							3.56		21	0.118	0.040				10-11														
11	12	Limonitic clay		"Medium brown, sl hematitic."							3.54		75	0.156	0.054				11-12														
12	13	Limonitic clay		"Medium brown, sl hematitic."							5.92	damp	330	0.228	0.078				12-13														
13	14	Saprolite		Red brown some cream clay.							4.40	damp	80	0.196	0.066				13-14														
14	15	Saprolite		Red brown some cream clay.							3.84	damp	27	0.292	0.088				14-15														
15	16	Saprolite		Red brown tr cream and black sl smectitic clay.							2.40	damp	59	0.230	0.036				15-16														
16	17	Saprolite		Red brown and light brown smectitic clay.							4.04	damp	158	0.458	0.064				16-17														
17	18	Saprolite		Red brown and light brown smectitic clay.							4.00	damp	355	0.282	0.072				17-18														
18	19	Saprolite		Red brown and green black mottled smectitic clay  tr weathered serpentinite.							0.58	damp	2915	0.364	0.134	38.86	22	0.85	18-19	4.78	-5	0.02	22300	10	7280	-5	-5	260	186				
19	20	Saprolite		Red brown and green black mottled smectitic clay  tr weathered serpentinite.							2.70	damp	1596	0.358	0.086	37.28	25	0.89	19-20	5.29	6	0.02	23500	11	5240	-5	-5	268	186				
20	21	Saprolite		Red brown and green black mottled smectitic clay  tr weathered serpentinite.							1.90	damp	1273	0.390	0.076	35.37	26	1.14	20-21	4.99	7	0.03	26800	12	4570	-5	6	257	205				
21	22	    Saprolite		Brown green mottled clay some weathered serpentinite.							6.24	damp	400	0.550	0.032	16.05	13	11.51	21-22	3.33	7	0.02	12100	7	2300	-5	-5	228	194				
22	23											damp	227						22-23														
23	24	Weathered serpentinite		Pale to dark green black some fresh.							14.08		150	0.240	0.014				23-24																												
24	25	Fresh serpentinite		Dark green black chips.							14.94		328	0.238	0.014				24-25																												
25	26	Fresh serpentinite		Pale green to dark green black chips and powder.							16.34		97	0.284	0.018				25-26																												
26	27	Fresh serpentinite		Pale green to dark green black chips and powder.							17.56		164	0.294	0.018				26-27																												
27	28																		27-28																												
28	29			Hole completed at 27m															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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