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RUMBLE RESOURCES LIMITED — Capital/Financing Update 2018
Apr 26, 2018
65736_rns_2018-04-26_112a2111-cefc-4643-92ad-699fabbd58a8.pdf
Capital/Financing Update
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Rumble Exercises Option to Earn into the Barramine High Grade Base Metal Project
Highlights
Barramine High Grade Cu- Pb-Zn- Ag Project, Western Australia
- High-grade Cu, Pb, Zn, and Ag prospects associated with NNW structures have not been tested by drilling or modern exploration.
- o Camel Hump Prospect large open mineralised structure returned:
- Cu to 13.4%, Pb to 3.08%, Zn to 1.79% and Ag to 131 g/t
- o Barramine Cu Prospect fault structure hosting significant Cu mineralisation, including:
- 25.32% Cu, 279 g/t Ag
- o Camel Hump Prospect large open mineralised structure returned:
- The same geology and structures that hosts the high-grade Braeside Zn and Pb mineralisation extends into the Barramine Project.
- o Recent exploration by Rumble within the Braeside Project, that adjoins the Barramine Project to the SSE, has identified anomalous Zn and Pb trends in soil geochemistry with VTEM conductors.
- o Reconnaissance RC drilling by Rumble at Braeside recently identified significant widths of alteration and Pb/Zn mineralisation at the Barker Well Prospect, which lies 2km south of the Barramine Project southern boundary.
- Rumble successfully renegotiated the terms to significantly reduce the earn in expenditure requirement down by half, from $1.5m to $750k, to earn 70%.
Rumble Resources Ltd (ASX: RTR) ("Rumble" or "the Company") is pleased to announce that it has exercised its option to acquire the Barramine Cu-Pb-Zn-Ag Project. The Barramine Project (E45/4368) is located approximately 150km ENE of Marble Bar in the Pilbara Region of Western Australia (Image 1) and is contiguous to Rumble's Braeside project.
Rumble's Managing Director, Mr Shane Sikora, said: "Rumble are pleased to exercise the option to acquire the high grade Barramine base metal Project on more favourable terms than originally agreed. The Barramine Project is a strategic opportunity to secure the northern extension to the Braeside Project's 34km mineralised structure, increasing the total strike length to over 40km's.
A recent reconnaissance RC drill program at Rumble's neighbouring Braeside Project significantly identified base metal mineralisation in 17 of 19 holes and included a highgrade zinc discovery on the first ever RC drill program completed at Braeside.
At the northern boundary of the Braeside Project, the identified base metal soil geochemistry trends (associated with the Barker Well large mineralised alteration on the main geological structure) are interpreted to extend into the Barramine Project to the north. This interpretation, recent drilling results at Braeside and stream and rock chips samples on the contiguous geological structures at the Barramine Project have provided Rumble with confidence that there is a high potential of finding high-grade base metal discoveries at the Barramine Project.
Rumble will fast track modern, systematic base metal exploration at the Barramine Project to generate first order targets for drill testing".

Rumble Resources Ltd
Suite 9, 36 Ord Street, West Perth, WA 6005
T +61 8 6555 3980
F +61 8 6555 3981
rumbleresources.com.au
ASX RTR
Executives & Management
Mr Shane Sikora Managing Director
Mr Brett Keillor Technical Director
Mr Matthew Banks Non-executive Director
Mr Michael Smith Non-executive Director
Mr Steven Wood Company Secretary

Image 1 – Barramine Project and Braeside Project Location Plan
Previous Exploration
Previous exploration mainly focused on multiple Mn prospects that lie within the Carawine Dolomite, Pinjian Chert Breccia and to a lesser extent, the Jeerinah Formation (see image 2). Historic exploration for base metals and gold included select areas of stream sediment sampling with limited soil sampling and rock chip sampling follow up. Some 245 stream sediment samples, collected during the early 1990's (see image 2 for locations), returned widespread low order gold and silver anomalism. Grab sampling was generally limited and poorly located with only approximately 12 samples with confirmed locations.
Two areas of base metal mineralisation have been explored. The Barramine and Camel Hump prospects consist of small historic diggings associated with major NNW trending structures. The structures and style of mineralisation are similar to recently defined base metal prospects within Rumble's Braeside project (see image 1). Grab sampling results returned generally high-grade Cu, with strongly anomalous Pb, Zn and Ag and are associated with mafic volcanics/volcaniclastics/shales of the Fortescue Group.
- At the Barramine prospect a channel sample collected by Blatchford in 1925 assayed 25.32% copper, 279 g/t silver, and a trace of lead.
- At the Camel Hump prospect, rock chip samples were assayed up to 13.4% Copper, 6% Lead, 1.8% Zinc and 131 g/t Silver.
Geology
The Barramine Project covers the northern extension of the Fortescue and Hamersley Group Rocks (late Archaean) that lie within Rumble's Braeside Project. The Barramine Project hosts shales, siltstones, carbonates and mafic volcanics of the Lower Hamersley Group which in turn overlies andesites, basalts, volcaniclastics, sediments and porphyry of the Fortescue Group.
The north and northwest trending faults/structural zones, some with associated base metal mineralisation are hosted in Fortescue Group intermediate/mafic volcanics and volcaniclastics in association with the Koongaling Felsic Volcanics. The felsic volcanics are bimodal with the Fortescue Group basalts and are potentially the source of the poly-metallic mineralisation. Elsewhere within the project, numerous Mn prospects are hosted within the Carawine Dolomite and Pinjian Chert Brecia of the Hamersley Formation.


Image 2 – Barramine Project – Geology and Prospect Location Plan
Exploration Potential
Mineralisation Extending into the Barramine Project
Ongoing exploration (including reconnaissance RC drilling – Dec 2017) by Rumble at the Braeside Project has identified wide zones of alteration with strongly anomalous Pb and Zn. At the Barker Well Prospect (image 3 and 4), a single recent RC drill-hole intercepted up to 120m of silica – sericite - chlorite alteration with wide zones of Pb and Zn anomalism. A near surface intercept of 14m @ 0.75% Pb with 2m @ 3.6% Pb from 6m had targeted strongly mineralised surface alteration (4.23 % Pb). Small diggings nearby returned grades of 38.1% and 24.04% Pb.
The main structure, anomalous soil geochemistry and VTEM conductor trends associated with the Barker Well alteration and anomalism are interpolated to extend north into the Barramine Project.
Historic stream sediment sampling conducted during 1987 - 1991 in the southern portion of the Barramine Project highlighted a number of anomalous Au and Ag drainages. Elevated silver is strongly associated with the main mineralised structure (image 3) that extends north of the Barker Well prospect area (Braeside Project). Pb mineralisation within the Braeside Project is associated with silver (silver used as a proxy for Pb). Gold in stream anomalism is also associated with the main mineralised structure (image 4).




Image 4 - Southern Barramine Project – Extrapolation of Mineralised Structure from Braeside Project - Au in Stream Sediment Anomalism

Camel Hump Prospect (see image 2 for location)
High grade copper mineralisation with associated Pb, Zn and Ag lies within a northwest trending fault/shear structure in contact with felsic schists (felsic volcaniclastics) at the Camel Hump prospect. Limited grab sampling (12 rock chip samples) has defined multiple zones over a strike length of 1.5km (image 5). The zone of interest is completely open under shallow cover) and has not been explored by modern exploration (soil geochemistry, geophysics and drilling). Grab sampling results include:
- 13.4%, 1.78%, 1.4% Cu
- 3.08% Pb
- 1.79% Zn
- 131 g/t Ag
Rumble considers the potential for economic porphyry related style base metal mineralisation is high at the Camel Hump Prospect. No soil geochemistry or systematic grab sampling has been completed along the Camel Hump trend.

Image 5 – Camel Hump Prospect – Location of Grab Sample Base Metal Anomalism and Main Structure
Proposed Exploration – Barramine Project
Proposed exploration by Rumble includes the following for the 2018 field season.
- Soil Geochemistry (multi-element)
- o Extending the Braeside existing soil geochemistry north into the Barramine Project.
- o Detailed soil geochemistry along the Camel Hump Prospect trend.
- o Detailed soil geochemistry along the Barramine Cu prospect trend.
- Prospect geological mapping and rock chip geochemistry over soil geochemical anomalies.
- Ground geophysical surveys of geochemical/geological targets (if warranted)

Key Commercial Terms of the Barramine Binding Earn-In Agreement
RTR renegotiated the terms to acquire 70% of the title and interest in the Barramine Project and has provided notice to Great Sandy that it has exercised the option based on the below Terms:
a. RTR has to spend $750,000 on exploration over a period of 3 years from the execution of the agreement to earn 70% (renegotiated down from A$1,500,000)
b. RTR is required to spend $50,000 before it can withdraw from the definitive agreement (renegotiated down from $100,000
-
c. RTR to pay Great Sandy Pty Ltd $50,000 in RTR Shares
-
d. Great Sandy Pty Ltd is free carried to BFS
-
e. Following the completion of a BFS and decision to mine, Great Sandy Pty Ltd can either elect to contribute to ongoing project development or dilute to a 1.5% NSR
-
f. Great Sandy Pty Ltd will reserve and retain all rights relating to manganese and iron ore
-
ENDS –
About Rumble Resources Ltd
Rumble Resources Ltd is an Australian based exploration company, officially admitted to the ASX on the 1st July 2011. Rumble was established with the aim of adding significant value to its current gold and base metal assets and will continue to look at mineral acquisition opportunities both in Australia and abroad.
Forward Looking and Cautionary Statement
The information in this report that relates to historic exploration results was collected from DMP reports submitted by government agencies and previous explorers. Rumble has not completed the historical data or the verification process. As sufficient work has not yet been done to verify the historical exploration results, investors are cautioned against placing undue reliance on them.
Competent Persons Statement
The information in this report that relates to Exploration Results is based on information compiled by Mr Brett Keillor, who is a Member of the Australasian Institute of Mining & Metallurgy and the Australian Institute of Geoscientists. Mr Keillor is an employee of Rumble Resources Limited. Mr Keillor has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the "Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves". Mr Keillor consents to the inclusion in the report of the matters based on his information in the form and context in which it appears.

Section 2 Reporting of Exploration Results
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Mineraltenementandlandtenurestatus | •Type, reference name/number, location andownership including agreements or material issueswith third parties such as joint ventures,partnerships, overriding royalties, native titleinterests, historical sites, wilderness or nationalpark and environmental settings.•The security of the tenure held at the time ofreporting along with any known impediments toobtaining a licence to operate in the area. | •The project comprises of a singlegranted exploration license – E45/4368.•The license is currently owned by GreatSandy Pty Ltd. Rumble Resources hasexercised its option to earn 70% of theproject.•The license is granted, in a state ofgood standing and has no knownimpediments to operate in the area. |
| Explorationdone by otherparties | •Acknowledgment and appraisal of exploration byother parties. | •Exploration for base metals at CamelHump by Great Sandy Pty Ltd. SeeTable 1.•Historic stream sediment samplingcompleted by Carpentaria Exploration(CEC). The survey (245 samples) wascomplete for Au and Ag. Incomplete forbase metals. Summary of CEC Autargets Table 2. Results are Table 3. |
| Geology | •Deposit type, geological setting and style ofmineralisation. | •Target is Zn, Pb, Cu and preciousmetals. Deposit type is considered thesame as Rumbles Braeside Project –porphyry related base metal. |
| DrillholeInformation | •A summary of all information material to theunderstanding of the exploration results including atabulation of the following information for allMaterial drill holes:oeasting and northing of the drill hole collaroelevation or RL (Reduced Level – elevationabove sea level in metres) of the drill hole collarodip and azimuth of the holeodown hole length and interception depthohole length.•If the exclusion of this information is justified on thebasis that the information is not Material and thisexclusion does not detract from the understandingof the report, the Competent Person should clearlyexplain why this is the case. | •No drilling reported |
| Dataaggregationmethods | •In reporting Exploration Results, weightingaveraging techniques, maximum and/or minimumgrade truncations (e.g. cutting of high grades) andcut-off grades are usually Material and should bestated.•Where aggregate intercepts incorporate shortlengths of high grade results and longer lengths oflow grade results, the procedure used for suchaggregation should be stated and some typicalexamples of such aggregations should be shown indetail.•The assumptions used for any reporting of metalequivalent values should be clearly stated. | •No drilling completed |
| Relationshipbetweenmineralisationwidthsandintercept | •These relationships are particularly important in thereporting of Exploration Results.•If the geometry of the mineralisation with respect tothe drill hole angle is known, its nature should bereported. | •Not applicable – no drilling completed |
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| lengths | •If it is not known and only the down hole lengths arereported, there should be a clear statement to thiseffect (e.g. 'down hole length, true width notknown'). | |
| DiagramsBalancedreporting | •Appropriate maps and sections (with scales) andtabulations of intercepts should be included for anysignificant discovery being reported These shouldinclude, but not be limited to a plan view of drill holecollar locations and appropriate sectional views.•Where comprehensive reporting of all ExplorationResults is not practicable, representative reportingof both low and high grades and/or widths shouldbe practiced to avoid misleading reporting ofExploration Results. | •Image 1 presents the Barramine Projectin conjunction with Rumbles BraesideProject•Image 2 Barramine Project – ProjectLocation and Geology Plan.•Image 3. Southern Barramine Project –Extrapolation of Mineralised Structurefrom Braeside Project - Ag in StreamSediment Anomalism•Image 4. Southern Barramine Project –Extrapolation of Mineralised Structurefrom Braeside Project - Au in StreamSediment Anomalism•Image 5. Camel Hump Prospect –Location of Grab Sample Base MetalAnomalism and Main Structure•Table 1 presents the rock chip samples•Limited data for base metal exploration |
| Othersubstantiveexplorationdata | •Other exploration data, if meaningful and material,should be reported including (but not limited to):geological observations; geophysical surveyresults; geochemical survey results; bulk samples –size and method of treatment; metallurgical testresults; bulk density, groundwater, geotechnicaland rock characteristics; potential deleterious orcontaminating substances. | •No systematic soil sampling completed.•Selected stream sediment samplingwith the focus on Au and Ag |
| Further work | •The nature and scale of planned further work (e.g.tests for lateral extensions or depth extensions orlarge-scale step-out drilling).•Diagrams clearly highlighting the areas of possibleextensions, including the main geologicalinterpretations and future drilling areas, providedthis information is not commercially sensitive. | •Future work includes systematic soilsampling (same methodology ascompleted by Rumble in the BraesideProject) |

Table 1 – Barramine Project - Significant Historical Assays - Camel Hump prospect
| Sample ID | AU | Ag | Cu | Pb | Zn |
|---|---|---|---|---|---|
| Units | Ppb | Ppm | Ppm | Ppm | Ppm |
| CHMR1 | 34 | 27.5 | 1.40% | 6.04% | 1.80% |
| CHMR2 | 77 | 131 | 13.40% | 3.08% | 512 |
| CHMR3 | 2 | 6470 | 1380 | 1270 | |
| CHMR4 | 1 | 3690 | 438 | 32 | |
| CHMR5 | 1 | 1150 | 427 | 108 | |
| CHMR6 | 0.5 | 100 | 42 | 44 | |
| CHMR7 | -0.5 | 528 | 26 | 24 | |
| CHMR8 | -0.5 | 270 | 188 | 32 | |
| CHMR9 | -0.5 | 110 | 226 | 58 | |
| CHMR10 | -0.5 | 84 | 23 | 10 | |
| CHMR11 | -0.5 | 6650 | 20 | 24 | |
| CHMR12 | 15 | 3 | 1.78% | 419 | 250 |
Table 2. Stream Sediment Sampling by CEC (1988) – Result Summary
| Name | Sample | MGA East | MGANorth | Assayppb Au | Comments |
|---|---|---|---|---|---|
| Carters CkNorth | 89954 | 296,062 | 7,680,306 | 9.7 | 800m W of E45/838.Repeated 6.8ppb, upstreamsamples 0.3 & 0.1ppb indicate source outside JV EL sonot followed up. |
| Greek CkEast | 89956 | 298,867 | 7,679,037 | 6.4 | Upstream sample 92724 16.8ppb confirmed result butsource area looks small as creeks draining the west sideare low. No soil sampling. |
| Greek CkWest | 89679 | 297,774 | 7,678,698 | 3.0 | Confirmed by upstream sample 92734 4.7ppb, butsurrounding samples <1ppb. No soil sampling. |
| Viking I | 92623 | 292,213 | 7,686,528 | 28.7 | Other values of 23.6 & 18.1 over 1.2km in NW trendingzone in Maddina Basalt. Other creeks sampled in areadid not have elevated results. No soil sampling. |
| Viking III | 89882 | 295,261 | 7,685,311 | 6.4 | Not followed up.Located 700m NW of Camel Humpoccurrence.In faulted Jeerinah Formation sedimentsand Maddina Basalt. No soil sampling. |
| Londonderry | 92714 | 290,103 | 7,680,993 | 86.3 | Supported by 64.1 & 23.8ppb over 1.5km, NW trend.Underlain by Bamboo Creek Member felsic volcanics(Hardy Formation) with a band of Kylena Formationcarbonate (Fortescue Group) possible related to theanomalism. Best soil sample 22ppb Au. |
| Paddy'sFind | 89863 | 293,080 | 7,680,061 | 86.6 | Repeat sampled at 4.6ppb but supported by 19.7ppbin aparallel creek.Maddina Basalt cut by a NW trendingfault. Best soil sample 200ppb Au came from a zone ofcarbonate altered? basalt. |
| Carters Ck | 93376 | 295,986 | 7,678,186 | 142 | Supported by 49.6, 12.7ppb in adjacent creeks, defines aNNW zone ~500m long parallel stratigraphy in MaddinaBasalt. Mapped by CEC, best soil sample 147ppb Au. |
| Carters CkNorth | 89954 | 296,062 | 7,680,306 | 9.7 | No follow-up drainage sampling. In Kylena Basalt. Bestsoil sample 5ppb Au from 400x500m grid. |

Table 3. Stream Sediment Sampling Results – CEC 1988
| SAMPLE | MGA_E | MGA_N | AU_BLEG_PPB | AG_PPB | AS_PPM | CO_PPM | SAMPLE | MGA_E | MGA_N | AU_BLEG_PPB | AG_PPB | AS_PPM | CO_PPM |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 92710 | 289886.8 7680634 | 1.1 | 1.8 | 0 | 0 | 90883 | 292722.8 7684680.6 | 0.5 | 7 | 5 | 39 | ||
| 92709 | 290276.7 7680450 | 0.3 | 1.4 | 0 | 0 | 89967 | 290495 | 7684651.1 | 0 | 0 | 3 | 7 | |
| 92708 | 290384.3 7680457 | 64.1 | 18.6 | 0 | 0 | 90881 | 294546.9 7683961.1 | 19.2 | 5.2 | -2 | 31 | ||
| 89865 | 290475.7 7680192 | 6 | 1.9 | -2 | 36 | 90887 | 288058.7 7683946.8 | 0 | 0 | 0 | 0 | ||
| 89864 | 290611.7 7680236 | 1.7 | 4.1 | 15 | 40 | 90886 | 288882.9 7684904.8 | 0 | 0 | 0 | 0 | ||
| 92717 | 290753.4 7680737 | 1.6 | 3.1 | 0 | 0 | 89811 | 289272.5 7684674.8 | 0 | 0 | 0 | 0 | ||
| 93285 | 291032.8 7680197 | -0.1 | 11.3 | 4 | 19 | 90885 | 289167.3 7684932.9 | 0 | 0 | 0 | 0 | ||
| 93284? | 291171.8 7680152 | 0.6 | 5.2 | 2 | 81 | 89965 | 290291.8 7686822.1 | 0.3 | 4 | 0 | 30 | ||
| 93283 | 291425.6 7680141 | 0.2 | 6.7 | 3 | 24 | 89966 | 290459.6 7686774.7 | 0.7 | 3 | 0 | 42 | ||
| 89948 | 292918.8 7680698 | 1.1 | 9.9 | 3 | 0 | 92712 | 289459.2 | 7681193 | 2.1 | 0 | 0 | 0 | |
| 89946 | 293110.9 7680554 | 0.5 | 2.8 | 4 | 37 | 92713 | 289452.1 7681288.2 | 23.8 | 0 | 0 | 0 | ||
| 89947 | 292953.9 7680406 | 0.2 | 1.8 | 4 | 82 | 92714 | 289485.6 7681359.1 | 86.3 | 7.2 | 0 | 0 | ||
| 89863 | 292626.4 7680119 | 86.6 | 80.8 | -2 | 21 | 92711 | 289843.5 7681135.9 | 2.7 | 16.8 | 0 | 0 | ||
| 92704 | 292930.4 7680005 | 19.7 | 22.2 | 0 | 0 | 92715 | 290364.4 7681532.1 | 1.1 | 10 | 0 | 0 | ||
| 92706 | 293159.3 7679980 | 1.6 | 8 | 0 | 0 | 92716 | 290511.5 7681283.8 | 2.4 | 6 | 0 | 0 | ||
| 92705 | 293234.3 7680082 | 5.8 | 5.5 | 0 | 0 | 93286 | 291152.7 7681356.1 | -0.1 | 8.3 | 6 | 25 | ||
| 89676 | 290079.4 7678959 | 0.1 | 6.7 | 4 | 37 | 92707 | 293606.2 7679921.9 | 0.5 | 2.8 | 0 | 0 | ||
| 89997 | 289793 | 7678894 | 1 | 10.8 | 3 | 38 | 92640 | 295263.1 7677357.2 | 0 | 0 | 0 | 0 | |
| 89996 | 289632.4 7678820 | 2.6 | 7.7 | 6 | 15 | 92639 | 294976.8 7677658.8 | 0 | 0 | 0 | 0 | ||
| 89949? | 290395.2 7677749 | 0 | 0 | -2 | 38 | 92638 | 294955.2 7677863.9 | 0 | 0 | 0 | 0 | ||
| 98866 | 291060.1 7676868 | 0 | 0 | 0 | 0 | 92637 | 294984.5 7678142.9 | 0 | 0 | 0 | 0 | ||
| 89998 | 292485.2 7678081 | 0 | 0 | 0 | 0 | 92636 | 295005.9 7678150.8 | 0 | 0 | 0 | 0 | ||
| 89999 | 292559 | 7678244 | 0 | 0 | 0 | 0 | 90838 | 295021.7 | 7678260 | 0 | 0 | 0 | 0 |
| 89667 | 291708.9 7678258 | 0 | 0 | 0 | 0 | 90837 | 294977.1 7678308.7 | 0 | 0 | 0 | 0 | ||
| 89962 | 295833.6 7676955 | 0.1 | 1.2 | 4 | 26 | 93373 | 295023 | 7678362.9 | 0 | 0 | 0 | 0 | |
| 8996189951 | 295764.1 7676915295111.4 7677361 | 0.10.6 | 1.83 | 32 | 3634 | 9337298678 | 294968.6 7678510.4294799.5 7678552.7 | 00 | 00 | 06 | 039 | ||
| 89869 | 294905.7 7677808 | 0.2 | 3.9 | 2 | 34 | 90836 | 294816.3 7678488.7 | 0 | 0 | 0 | 0 | ||
| rs 93102 | 294794.1 7678560 | 0 | 0 | 0 | 0 | rs 93103 | 295439 | 7678832.1 | 1.2 | 3.9 | 0 | 0 | |
| 89871 | 295437.9 7678818 | 28.1 | 8.9 | -2 | 31 | 93104 | 295502.5 | 7678722 | 0.7 | 5.6 | 0 | 0 | |
| 93287 | 294416.8 7678675 | 0 | 0 | 5 | 23 | 92600 | 295807.5 7679204.3 | 3.5 | 12.9 | 0 | 0 | ||
| 93288 | 294384.9 7678636 | 0 | 0 | 4 | 34 | 92599 | 295799.7 | 7679181 | 4 | 16.4 | 0 | 0 | |
| 90000 | 294123.3 7679039 | 1.2 | 3.5 | 10 | 12 | 92598 | 295679.7 7679100.2 | 2.7 | 18.9 | 0 | 0 | ||
| 89950 | 293575.9 7678516 | 0 | 0 | 2 | 34 | 92601 | 296323.2 7679281.1 | 0.7 | 8.7 | 0 | 0 | ||
| 89867 | 293232 | 7679066 | 0.1 | 2.6 | 0 | 0 | 92602 | 296499.4 7679050.8 | 1.3 | 10.2 | 0 | 0 | |
| 89868? | 293060.8 7679130 | -0.1 | 2.5 | 0 | 0 | 92603 | 296672.2 7678842.7 | 0.6 | 9.4 | 0 | 0 | ||
| 93298 | 294527.3 7681216 | 0.5 | 5.9 | 7 | 31 | 92606 | 296655.6 7678378.5 | 1.1 | 10.2 | 0 | 0 | ||
| 89805 | 293530.3 7681379 | 0.2 | 1.6 | 4 | 37 | 92605 | 296657.3 7678334.9 | 1.1 | 3.8 | 0 | 0 | ||
| 89804 | 293306.5 7681382 | 0.1 | 9.5 | 6 | 25 | 92604 | 296715.7 7678318.3 | 0.8 | 7.2 | 0 | 0 | ||
| 89878 | 293862.2 7681736 | 0.5 | 3.6 | 3 | 22 | 92656 | 296768.5 7677658.5 | 0.7 | 8.6 | 0 | 0 | ||
| 89902 | 293957.4 7681993 | 2.7 | 9.2 | 3 | 22 | 92655 | 296553.8 7677679.4 | 2.6 | 16.9 | 0 | 0 | ||
| 93299 | 294445.7 7682157 | 0.5 | 6.1 | 2 | 28 | 92654 | 296550.1 7677801.9 | 2.4 | 9.7 | 0 | 0 | ||
| 89879 | 293905.1 7682305 | 0.2 | 2.4 | 9 | 21 | 92653 | 296565 | 7677837.1 | 4.9 | 38.7 | 0 | 0 | |
| 89807 | 293879.9 7682794 | 0 | 0 | 3 | 43 | 92612 | 296283.1 7678397.3 | 2 | 32.9 | 0 | 0 | ||
| 89064 | 293619.9 7683281 | 0.4 | 1.9 | 2 | 38 | 92610 | 296211 | 7678321.3 | 1.8 | 5.2 | 0 | 0 | |
| 92596 | 293306.3 7683640 | 0.2 | 2.8 | 0 | 0 | 92611 | 296232.2 7678312.7 | 9.2 | 11 | 0 | 0 | ||
| 89904 | 293145.8 7684099 | 0.2 | 5.1 | 3 | 28 | 92607 | 296321.1 7678200.5 | 4.8 | 9.8 | 0 | 0 | ||
| 89880 | 292914.9 7683270 | 0.2 | 4.7 | 5 | 21 | 92608 | 296348.9 7678215.2 | 5.6 | 19.8 | 0 | 0 | ||
| 93281 | 293409.3 7681353 | -0.1 | 3.6 | 2 | 32 | 92609 | 296370.3 7678273.3 | 1.9 | 16.7 | 0 | 0 | ||
| 89881 | 292654.4 7687871 | 0.1 | 7.6 | -2 | 85 | 92613 | 296141.6 7678603.9 | 9.7 | 45.7 | 0 | 0 | ||
| 89905 | 293175.2 7687783 | 5.3 | 4.7 | 2 | 25 | 92616 | 296152 | 7678654.4 | 4.8 | 23.1 | 0 | 0 | |
| 89812 | 293878.4 7686995 | 0.2 | 8.8 | 4 | 18 | 92615 | 296135.1 7678827.1 | 2.2 | 27.1 | 0 | 0 | ||
| 90884 | 291506.3 7686213 | 10.6 | 7.3 | 3 | 39 | 92614 | 296133.9 7678864.1 | 6.1 | 30 | 0 | 0 | ||
| 89810 | 290889.3 7685987 | 0 | 0 | 6 | 31 | 93379 | 295959.5 7678809.2 | 2.8 | 13 | 0 | 0 | ||
| 90882 | 292687.7 7684645 | 0.1 | 2.2 | 6 | 35 | 93380 | 295949.5 7678776.3 | 2.8 | 14.4 | 0 | 0 |

Table 3. Stream Sediment Sampling Results – CEC 1988
| SAMPLE | MGA_E | MGA_N | AU_BLEG_PPB | AG_PPB | AS_PPM | CO_PPM | SAMPLE | MGA_E | MGA_N | AU_BLEG_PPB | AG_PPB | AS_PPM | CO_PPM |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 93105 | 295810.6 7678701 | 4.7 | 15.8 | 0 | 0 | 89882 | 295248.5 7685841.4 | 6.4 | 7 | 3 | 16 | ||
| 9337693377 | 295868.7 7678293 | 295866.1 7678263 | 1422.7 | 13.97.6 | 00 | 00 | 8990689907 | 295866.9 7685644.7298585.9 7684856.2 | -0.10.1 | 72.3 | 20 | 90 | |
| 93378 | 295606.7 7678094 | 0.2 | 1.9 | 0 | 0 | 89813 | 297606.9 | 7684332 | -0.1 | 1.5 | 0 | 0 | |
| 93101 | 295623.6 7678058 | 1.8 | 4.7 | 0 | 0 | 89883 | 298070.9 7684053.2 | -0.1 | 2.4 | 0 | 0 | ||
| 92649 | 295790.1 7677904 | 3.7 | 18.1 | 0 | 0 | 93300 | 294595.9 7683934.9 | 0.3 | 3.6 | 3 | 27 | ||
| 9265092652 | 295804.3 7677917295956.6 7677926 | 8.749.6 | 12.412.9 | 00 | 00 | 8980693289 | 295514.7 7682119.3295540.1 7677197.2 | 0.10.2 | 1.81.8 | 24 | 2123 | ||
| 92651 | 295954.5 7677893 | 12.7 | 13.4 | 0 | 0 | 89963 | 295805.9 7676979.8 | 0.3 | 2.7 | 4 | 22 | ||
| 93374 | 295170 | 7678285 | 0 | 0 | 0 | 0 | 89952 | 296631 | 7675462.9 | 0 | 0 | 0 | 0 |
| 93375 | 295252.4 7678246 | 0.1 | 4.2 | 0 | 0 | 89953 | 295904.7 7679395.2 | 0.6 | 2.3 | 6 | 84 | ||
| 9083990840 | 295348.1 7677975295409.2 7677973 | 01.2 | 05.4 | 00 | 00 | 8995493290 | 295903.1 7679478.1296509.4 7679710.6 | 9.7-0.1 | 3.52.3 | 04 | 2415 | ||
| 92642 | 295517.6 7677628 | 0.3 | 5.4 | 0 | 0 | 92723 | 296385.4 7679619.5 | 0.3 | 3.4 | 0 | 0 | ||
| 92641 | 295543.5 7677614 | 0.7 | 7.8 | 0 | 0 | 89872 | 296673.4 7679480.1 | 0.3 | 5.1 | 4 | 16 | ||
| 9264392644 | 295663 | 295639.1 76775707677571 | 1.11 | 5.65.6 | 00 | 00 | 92291?92722 | 297218.5 | 297216.3 7680059.77679943 | -0.10.1 | 1.11.3 | 00 | 00 |
| 92645 | 295674.7 7677531 | 0.6 | 6.9 | 0 | 0 | 89955? | 297507 | 7680266.4 | 0.2 | 1.6 | 0 | 0 | |
| 92648 | 296130.4 7677533 | 4.1 | 15.8 | 0 | 0 | 89673? | 297662.2 7680455.4 | 0.1 | 1.7 | 0 | 0 | ||
| 92579 | 291960.1 7686870 | 23.6 | 14.7 | 0 | 0 | 89680 | 297391.1 7679439.4 | 0.2 | 4 | 0 | 0 | ||
| 92578 | 292005.3 7686857 | 0.5 | 5.7 | 0 | 0 | 89679 | 297302 | 7679339.3 | 3 | 21.5 | 0 | 0 | |
| 9262792626 | 292434.4 7686895292452.3 7686875 | 0.10.1 | 6.37.4 | 00 | 00 | 9273492733 | 297722.1 7678813.6297805.1 7678807.3 | 4.70.8 | 11.28.4 | 00 | 00 | ||
| 92629 | 292528.8 7686853 | 3.2 | 13.7 | 0 | 0 | 92732 | 297752.6 7678388.6 | 0.4 | 6.3 | 0 | 0 | ||
| 92628 | 292600.5 7686858 | 0.1 | 7.9 | 0 | 0 | 92730 | 298090.2 | 7678382 | 0.4 | 6.9 | 0 | 0 | |
| 92630 | 292696.8 7686735 | 0.3 | 12.9 | 0 | 0 | 92731 | 298052.3 | 7678277 | 0.4 | 6.7 | 0 | 0 | |
| 9263292631 | 292750 | 7686705292729.9 7686681 | 1.60.3 | 11.17.7 | 00 | 00 | 8980289958 | 298175.1 7678187.7299119.8 7677994.9 | 0.30.2 | 1.61.7 | 00 | 00 | |
| 92595 | 293208.4 7686694 | 32.2 | 18.3 | 0 | 0 | 93294 | 300424.6 7677578.9 | 0.3 | 3.1 | 0 | 0 | ||
| 92594 | 293109.8 7686469 | 0.9 | 12.7 | 0 | 0 | 93295 | 300622.6 | 7677563 | 0.1 | 2.2 | 0 | 0 | |
| 92593 | 293129.9 7686451 | 0.6 | 13.1 | 0 | 0 | 89877 | 301652.9 7676330.2 | 0 | 0 | 0 | 0 | ||
| 92580 | 291772 | 7686622 | 0.5 | 9.4 | 0 | 0 | 93297 | 301955 | 7677331.8 | 0 | 0 | 0 | 0 |
| 9262192623 | 291805.1 7686603291979.5 7686553 | 328.7 | 10.816.5 | 00 | 00 | 8987693296 | 301835.4 7677742.9301410.7 7677725.6 | 00 | 00 | 00 | 00 | ||
| 92622 | 291992.1 7686520 | 0.9 | 9.9 | 0 | 0 | 89857 | 300307.9 7678856.9 | 0.1 | 1.3 | 0 | 0 | ||
| 92625 | 292153.3 7686573 | 1.6 | 19.8 | 0 | 0 | 93293 | 299791.7 | 7679339 | 0.1 | 1.1 | 0 | 0 | |
| 92624 | 292137.1 7686545 | 3.9 | 19.3 | 0 | 0 | 89874 | 299573.5 7679284.1 | 0.1 | 1.9 | 0 | 0 | ||
| 9258892587 | 292476.5 7686441292463.5 7686387 | 0.40.8 | 4.77.9 | 00 | 00 | 9329289956 | 298941.3 7679660.7299074.3 7679410.2 | -0.16.4 | 1.86 | 00 | 00 | ||
| 92591 | 292784.3 7686217 | 0.5 | 16.1 | 0 | 0 | 92725 | 299132.2 7679297.2 | 0.2 | 2.7 | 0 | 0 | ||
| 92592 | 292813.6 7686195 | 3.9 | 11.2 | 0 | 0 | 92724 | 298966.2 7679296.4 | 16.8 | 13.8 | 0 | 0 | ||
| 92590 | 292670.5 7686074 | 18.1 | 13.2 | 0 | 0 | 92726 | 299291 | 7679025.2 | 0.9 | 8.1 | 0 | 0 | |
| 9258692585 | 292305 | 7686293292246.6 7686233 | 1.70.4 | 18.38.5 | 00 | 00 | 9272792728 | 299134.1 7679014.4299229.9 7678654.7 | 0.30.3 | 7.49.3 | 00 | 00 | |
| 92584 | 292271.8 7686211 | 2 | 21.1 | 0 | 0 | 92729 | 299066.4 7678656.7 | 0.1 | 2.1 | 0 | 0 | ||
| 89895 | 291822.9 7686400 | 8.7 | 18.7 | 0 | 0 | 89903 | 297351.1 7682045.9 | -0.1 | 8 | 0 | 0 | ||
| 89894 | 291815.4 7686461 | 0.6 | 17 | 0 | 0 | 89901 | 300804.8 7681756.5 | -0.1 | 2.7 | 0 | 0 | ||
| 8989390780 | 293000 | 291745.4 76864927684302 | 0.8-0.1 | 12.72.6 | 00 | 00 | 89722?92785 | 296719.9 7679641.9297362.3 7679274.1 | 00.5 | 2.77.1 | 00 | 00 | |
| 90860 | 292958.3 7684240 | -0.1 | 4.3 | 0 | 0 | 89959 | 298311.9 7675869.3 | 0 | 0 | 0 | 0 | ||
| 93371 | 293106.4 7684108 | 0.7 | 9.9 | 0 | 0 | 89885 | 293274.4 7689329.6 | 0 | 0 | 3 | 8 | ||
| 92634 | 293353.1 7684151 | 0.2 | 3.4 | 0 | 0 | 92581 | 292188.9 7685929.3 | 0.8 | 13.9 | 0 | 0 | ||
| 92635 | 293356.5 7683989 | 0.3 | 4.6 | 0 | 0 | 92582 | 292176.3 7685960.9 | 0.5 | 9.6 | 0 | 0 | ||
| 9259790859 | 293471.5 7683863293247.4 7683899 | 0.53.2 | 7.75.3 | 00 | 00 | 9258389897 | 292121.7 7685971.8291722.6 7685964.1 | 0.90.3 | 15.13 | 00 | 00 | ||
| 93370 | 293193.1 7683728 | 0 | 0 | 0 | 0 | 89898 | 291612.6 7686028.9 | 1.4 | 16.3 | 0 | 0 | ||
| 89809 | 293247.9 7683691 | 17.2 | 10.8 | 3 | 33 | 89899 | 291594.1 7686153.3 | 1.5 | 32.4 | 0 | 0 | ||
| 90398 | 294300.3 7684767 | 0.7 | 6.2 | 0 | 0 | rs 92633 | 293236.7 7683884.2 | 0.4 | 4 | 0 | 0 | ||
| 9039990400 | 294343.4 7684764294434.4 7684564 | 0.80.3 | 7.26.3 | 00 | 00 | 9270389814 | 292592.3 7680109.9301436.4 7691026.7 | 5.4-0.1 | 2.52 | 00 | 00 | ||
| 93107 | 294357 | 7684259 | 0.3 | 13.3 | 0 | 0 | UNKN01 | 296031.1 7677585.8 | 2.7 | 10.8 | 0 | 0 | |
| 89909 | 294573.5 7690419 | -0.1 | 1.2 | 0 | 0 | UNKN02 | 295929.3 7677571.9 | 0.7 | 9.4 | 0 | 0 | ||
| 89908 | 300447.6 7688510 | -0.1 | 1.1 | 0 | 0 | 89724 | 293153.1 7684126.2 | 0.2 | 5.1 | 0 | 0 | ||
| 89884 | 300519.1 7688385 | -0.1 | 1.7 | 0 | 0 | rs 93106 | 294544.3 7683975.9 | 0.7 | 14.9 | 0 | 0 |