Highest-Grade Lithium Intersection to Date at Red Mountain
Released
Released
Announcement PDF
ASX / Media Release
16 December 2025
Suite 116 Level 1, 165-167 Phillip St Sydney, NSW 2000
GPO Box 2733, Sydney NSW 2001
P. +61 (0) 2 8046 2799 | E. admin@venariminerals.com
venariminerals.com
Exceptional wide, high-grade lithium intersection reinforces
quality and scale of the Red Mountain lithium discovery
109.7m of lithium mineralisation includes the highest-grade intercept to date,
confirming the strong tenor of the Northern Area of the deposit
Highlights
• Highest-grade lithium intersection received to date from the Red Mountain Project
returned from the October drilling campaign.
• Drill-hole RMRC013 intersected a combined 109.7m of lithium mineralisation (combined
estimated true width ‘ETW’ of 87.8m), including:
o 77.7m (ETW 62.2m) @ 2,440ppm Li from 76.2m, including:
▪ 24.4m (ETW 19.5m) @ 4,270ppm Li from 97.5m; and
▪ 7.6m (ETW 6.1m) @ 3,080ppm Li from 132.6m; and
o 4.6m (ETW 3.7m) @ 2,610ppm Li from 59.4m; and
o 7.6m (ETW 6.1m) @ 1,460ppm Li from 170.7m.
• Result firms up the tenor of mineralisation down-dip from high-grade hole RMDD003, which
intersected 32.4m @ 3,260ppm Li from 57.2m, 13.8m @ 1,330ppm Li from 39.6m and 23.3m
@ 1,610ppm from 94.4m to end-of-hole.
• Assay results remain outstanding for three holes, expected in the coming fortnight, which will
pave the way for a maiden Mineral Resource Estimate (MRE) for Red Mountain in early 2026.
Venari Minerals NL (ASX: VMS) (“Venari”, “the Company” or “VMS”) is pleased to report assay results
for RMRC013, which was drilled in the northern area of the 100%-owned Red Mountain Project in
Nevada, USA, as part of a 13-hole Reverse Circulation (RC) drilling campaign completed in October
2025.
Drill-hole RMRC013 was designed to test for mineralisation down-dip of the high-grade lithium
intersected in previous hole RMDD003 (Figures 2 and 3). RMRC013 was highly successful, intersecting
the highest-grade mineralisation to date at the Project and extending the drill-defined extent of
mineralisation to a depth of approximately 150 metres below surface.
The exceptionally high-grade mineralisation in the hole, which includes 12individual 1.5m (5ft) samples
grading in excess of 4,000ppm Li, is expected to firm up a high-grade core to the northern part of the
Project, which includes several other holes that intersected high-grade mineralisation – RMDD003,
RMDD002, RMRC014 and RMRC015.
Assays remain outstanding for three holes from the campaign.
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Venari Chairman, Tony Leibowitz, said:
“The results from hole RMRC013 are quite exceptional and show the Tier-1 scale and quality of the Red
Mountain Project. Importantly, this hole has strengthened and expanded the strategically important
high-grade core in the Northern Area of the deposit. The October drilling campaign has been very
successful, and we are looking forward to seeing the results of the final three holes, which are expected
in the coming fortnight. As a result of the delays experienced with assay laboratories in North America,
the maiden MRE for Red Mountain will now be delivered in Q1 2026. Against the backdrop of rapidly
improving sentiment in the lithium market, we are looking forward to achieving this milestone and
illustrating the enormous value in this project to our shareholders.”
Results
Intersections for RMRC013 are as follows:
• 10.7m down-hole (estimated true width ‘ETW’ 8.6m) @ 1,690ppm Li / 0.90% Lithium Carbonate
Equivalent (LCE) from 57.9m, including:
o 4.6m (ETW 3.7m) @ 2,610ppm Li / 1.39% LCE from 59.4m;
• 77.7m down-hole (ETW 62.2m) @ 2,440ppm Li / 1.3% LCE from 76.2m, including:
o 24.4m (ETW 19.5m) @ 4,270ppm Li / 2.27% LCE from 97.5m, and
o 7.6m (ETW 6.1m) @ 3,080ppm Li / 1.64% LCE from 132.6m;
• 21.3m downhole (ETW 17m) @ 966ppm Li / 0.51% LCE from 170.7m, including:
o 7.6m (ETW 6.1m) @ 1,460ppm Li / 0.78% LCE from 170.7m;
Figure 1. RMRC013-RMDD003 preliminary interpretative cross-section with down-hole lithium geochemistry.
Hole ID
Easting
(NAD83)
Northing
(NAD83)
RL (m)
Azimuth
(°)
Dip
(°)
Depth
(m)
RMRC013 637122 4291198.1 1707.7 90.5 -70 210.3
Table 1. Drill collar details
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Background
Located in central-eastern Nevada (Figure 3), adjacent to the Grand Army of the Republic Highway (Route
6), the Red Mountain Project was staked by Venari in August 2023.
Figure 2. Red Mountain north and central (down-hole) drill intersections over gridded soil geochemistry image.
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The Project area has broad mapped tertiary lacustrine (lake) sedimentary rocks known locally as the Horse
Camp Formation. Elsewhere in Nevada, equivalent rocks host large lithium deposits (see Figure 3) such as
Lithium Americas’ (NYSE: LAC) 62.1Mt LCE Thacker Pass Project3
and American Battery Technology
Corporation’s (NASDAQ: ABAT) 15.8Mt LCE Tonopah Flats deposit4
.
Prior to the most recent campaign, a total of 19 drill holes had been completed at the project to date for a
combined 3,336m of drilling across three campaigns. These campaigns have been highly successful,
intersecting strong lithium mineralisation in almost every hole6
.
Scoping leachability testwork on mineralised material from Red Mountain indicates high leachability of
lithium of up to 98%, varying with temperature, acid strength and leaching duration5
, and beneficiation test-
work has indicated the potential to upgrade the Red Mountain mineralisation1,2,7
.
Figure 3. Location of Red Mountain and other Nevada Lithium projects.
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References
1 – ASX: ASE, 22 April 2025, Beneficiation testwork successfully upgrades mineralisation at Red Mountain
2 - ASX: ASE, 10 June 2025, Beneficiation Delivers 4,480ppm Lithium Clay Concentrate at Red Mountain
3 - NYSE: LAC, 31 December 2024, Updated NI 43-101 Technical Report for the Thacker Pass Project
4 - OTCMKTS: ABML, 26 February 2023, Technical Report Summary for The Tonopah Flats Lithium Project, Esmeralda
5 - ASX: ASE, 9 December 2024, Positive initial metallurgical results from Red Mountain
6 - ASX: ASE, 25 June 2025, Exceptional Drill-hole Intersects combined 170m of Lithium Mineralisation at Red Mountain
7 - ASX: ASE, 3 September 2025, Outstanding lithium anomalism in surface sampling at Red Mountain Extension
8 – ASX: VMS, 15 October 2025, Metallurgical test-work delivers 132% upgrade to lithium mineralisation at Red Mountain, Nevada
9 – ASX: VMS, 17 November 2025, Initial Red Mountain Assays confirm High-grade Lithium
10 – Lithium Carbonate Equivalent wt%(LCE) has been calculated from Lithium parts-per-million (ppm) by the formula LCE = Li (ppm)
x 5.323 /10,000
11 – ASX: ASE, 15 May 2025, Exceptional lithium intercept extends Red Mountain discovery further to the North
Authorisation
This announcement has been authorised for release by the Board of Venari Minerals NL.
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For further information, please contact:
Matthew Healy Nicholas Read
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T: +61 (0) 431 683 952 T: +61 (0) 419 929 046
E: matt@venariminerals.com E: nicholas@readcorporate.com.au
Competent Persons
The information in this report that relates to Sampling Techniques and Data (Section 1) is based on
information compiled by Mr. Matthew Healy, a Competent Person who is a Member of The Australasian
Institute of Mining and Metallurgy (AusIMM Member number 303597). Mr Healy is a full-time employee
of Venari Minerals NL and is eligible to participate in share-based incentive schemes of the Company.
Mr Healy has sufficient experience that is relevant to the style of mineralisation and type of deposit
under consideration and to the activity being undertaken 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 Healy consents to the inclusion in the report of the matters based on his
information in the form and context in which it appears.
The information in this report that relates to Reporting of Exploration Results (Section 2) is based on
information compiled by Mr. Richard Newport, principal partner of Richard Newport & Associates –
Consultant Geoscientists. Mr. Newport is a member of the Australian Institute of Geoscientists and
has sufficient experience which is relevant to the style of mineralisation and type of deposit under
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consideration and to the activity which he is undertaking to qualify as a Competent Person under the
2012 Edition of the ’Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore
Reserves‘. Mr. Newport consents to the inclusion in this announcement of the matters based on his
information in the form and context in which it appears.
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APPENDIX 1 - JORC Code, 2012 Edition – Table 1
SECTION 1 - SAMPLING TECHNIQUES AND DATA
Criteria JORC Code explanation Commentary
Sampling
techniques
Nature and quality of sampling (e.g.
cut channels, random chips, or
specific specialised industry
standard measurement tools
appropriate to the minerals under
investigation, such as down hole
gamma sondes, or handheld XRF
instruments, etc.). These examples
should not be taken as limiting the
broad meaning of sampling.
Include reference to measures
taken to ensure sample
representivity and the appropriate
calibration of any measurement
tools or systems used.
Aspects of the determination of
mineralisation that are Material to
the Public Report.
In cases where ‘industry standard’
work has been done this would be
relatively simple (e.g. ‘reverse
circulation drilling was used to obtain 1
m samples from which 3 kg was
pulverised to produce a 30 g charge
for fire assay’). In other cases, more
explanation may be required, such
as where there is coarse gold that
has inherent sampling problems.
Unusual commodities or
mineralisation types (e.g. submarine
nodules) may warrant disclosure of
detailed information.
5.5” reverse circulation drilling was
undertaken for drill sample
collection. Samples were collected
on a 5-foot basis in calico bags,
with approximate 30% split
retained from a rotary cone splitter
for lab assay. Water was injected
throughout the hole.
Nominal small drill sample was
collected for chip tray records
Samples were air dried on elevated
grid mesh until practical to
transport
Claystone hosted lithium deposits
are thought to form as a result of
the weathering of lithium-bearing
volcanic glass within tertiary-aged
tuffaceous lacustrine sediments of
the mapped Ts3 unit. Inputs of
lithium from geothermal sources
have also been proposed.
Drilling
techniques
Drill type (e.g. core, reverse circulation,
open-hole hammer, rotary air blast,
auger, Bangka, sonic, etc.) and details
(e.g. core diameter, triple or standard
tube, depth of diamond tails, face-
sampling bit or other type, whether core
is oriented and if so, by what method,
etc.).
5.5” Reverse Circulation drilling
methods employed using a cross-
over sub immediately behind the
hammer.
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Drill sample
recovery
Method of recording and assessing
core and chip sample recoveries
and results assessed.
Measures taken to maximise
sample recovery and ensure
representative nature of the
samples.
Whether a relationship exists between
sample recovery and grade and
whether sample bias may have
occurred due to preferential loss/gain
of fine/coarse material.
Sample recoveries to be measured by
dry sample weight at the laboratory
prior to assay.
Some instances of poor recovery
noted.
Instances of poor recovery are not
expected to materially impact
interpretation of results
Logging Whether core and chip samples
have been geologically and
geotechnically logged to a level of
detail to support appropriate Mineral
Resource estimation, mining studies
and metallurgical studies.
Whether logging is qualitative or
quantitative in nature. Core (or
costean, channel, etc.) photography.
The total length and percentage of
the relevant intersections logged.
Drill cuttings of entire hole logged
for lithology by consultant
geologist
Logging is qualitative with selective
quantitative logging (e.g. quartz
veining)
Chip tray photography undertaken
on all full drill holes
Sub-
sampling
techniques
and sample
preparation
If core, whether cut or sawn and whether
quarter, half or all core taken.
If non-core, whether riffled, tube sampled,
rotarysplit, etc. and whether sampled wet
or dry.
For all sample types, the nature, quality
and appropriateness of the sample
preparationtechnique.
Quality control procedures adopted for all
sub-sampling stages to maximise
representivityof samples.
Measures taken to ensure that the
sampling isrepresentative of the in-situ
material collected,including for instance
results for field duplicate/second-half
sampling.
Samples 30% split using a rotary cone
splitter and submitted to ALS
Laboratories in Reno for preparation
and analysis.
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Quality of
assay data
and
laboratory
tests
Whether sample sizes are appropriate to
thegrain size of thematerial being
sampled.
The nature, quality and appropriateness of
the assaying and laboratory procedures
used andwhether the technique is
considered partial ortotal.
For geophysical tools, spectrometers,
handheldXRF instruments, etc., the
parameters used in determining the
analysis including instrument make and
model, reading times, calibrations
factors applied and theirderivation, etc.
Nature of quality control procedures
adopted (e.g. standards, blanks,
duplicates, external laboratory checks)
and whether acceptable levels of
accuracy (i.e. lack of bias) and precision
have been established.
Samples analysed by method ME-
MS61 which is an ICP-MS method
employing a 4-acid digest.
A comparison of aqua-regia and 4-
acid digests was undertaken for Red
Mountain mineralisation, with no
material difference in lithium results
identified.
Assay quality was monitored using
pulp blanks, as well as certified
reference materials (CRMs) at a range
of lithium grades. Pulp blank results
indicated no material contamination
of samples from sample preparation
or during the analytical process. CRM
results were within 3 standard
deviations of certified values. No
material systematic bias nor other
accuracy related issues were
identified.
Verification
of sampling
and
assaying
The verification of significant intersections
byeither independent or alternative
company personnel.
The use of twinned holes.
Documentation of primary data, data
entryprocedures, data verification, data
storage(physical and electronic)
protocols.
Discuss any adjustment to assay data.
Sample intervals assigned a unique
sample identification number
prior to sample despatch
Lithium-mineralised claystone
Certified Reference Materials
(standards), pulp blanks and coarse
blanks inserted into the sample
stream at regular intervals to monitor
lab accuracy and potential
contamination during sample prep
and analysis.
Location of
data points
Accuracy and quality of surveys used to
locatedrill holes (collar and down-hole
surveys), trenches, mine workings and
other locations used in Mineral Resource
estimation.
Specification of the grid system used.
Quality and adequacy of topographic
control.
Drill collar locations determined using
hand held GPS with location reported
in NAD83 UTM Zone 11 with expected
accuracy of +/- 10m
Downhole surveys conducted on drill
holes at nominal 100ft intervals, with
drill rigs lined up by compass and
clino at start of hole.
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APPENDIX 1 - JORC Code, 2012 Edition – Table 1
Criteria JORC Code explanation Commentary
Data
spacing and
distribution
Data spacing for reporting of Exploration
Results.
Whether the data spacing and distribution
is sufficient to establish the degree of
geological and grade continuity
appropriate for the Mineral Resource and
Ore Reserve estimation procedure(s) and
classifications applied.
Whether sample compositing has been
applied.
Drill spacing appropriate for early
stage exploration
Orientation
of data in
relation to
geological
structure
Whether the orientation of sampling
achieves unbiased sampling of possible
structures and the extent to which this is
known, considering the deposit type.
If the relationship between the drilling
orientation and the orientation of key
mineralised structures is considered to
have introduced a sampling bias, this
should be assessed and reported if
material.
Claystone beds are regionally
shallow-dipping at ~20°-45° to the
east and varying locally across the
Project with some evidence of faulting
and potential folding. Most holes are
drilled approximately perpendicular
to bedding, with some having a down-
dip component due to drill pad
location and allowable disturbance
limitations. These holes have
estimated true width intersections
included in the body release as well
as down hole intersections.
Sample
security
The measures taken to ensure sample
security.
Samples stored at secured yard and
shed located in township of Currant
until delivered by staff or contractors to
the ALS labs
Audits or
reviews
The results of any audits or reviews of
sampling techniques and data.
Not applicable
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APPENDIX 1 - JORC Code, 2012 Edition – Table 1
SECTION 2 - REPORTING OF EXPLORATION RESULTS
Criteria JORC Code explanation Commentary
Mineral
tenement
and land
tenure
status
Type, reference name/number, location
and ownership including agreements or
material issues with third parties such as
joint ventures, partnerships, overriding
royalties, native title interests, historical
sites, wilderness or national park and
environmental settings.
The security of the tenure held at the time
of reporting along with any known
impediments to obtaining a licence to
operate in the area.
Red Mountain Claims held in 100%
subsidiary Needles Holdings Inc.
Claims located on Federal (BLM) Land
Drilling conducted on claims certified
by the Bureau of Land Management
(BLM)
Exploration
done by
other parties
Acknowledgment and appraisal of
exploration by other parties.
No known previous lithium exploration
conducted at Red Mountain.
Exploration conducted elsewhere in
Nevada by other explorers referenced in
body text.
Geology Deposit type, geological setting and style
of mineralisation.
The principal target deposit style is
claystone hosted lithium
mineralisation. Claystone hosted
lithium deposits are thought to form as
a result of the weathering of lithium-
bearing volcanic glass within tertiary-
aged tuffaceous lacustrine sediments
of the mapped Ts3 unit.
Lacustrine environments formed as a
result of extensional tectonic regime
that produced ‘basin and range’
topography observed across the state
of Nevada. Inputs of lithium from
geothermal sources have also been
proposed.
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Drill hole
Information
A summary of all information material to
the understanding of the exploration
results including a tabulation of the
following information for all Material drill
holes:
• easting and northing of the drill
hole collar
• elevation or RL (Reduced Level –
elevation above sea level in
metres) of the drill hole collar
• dip and azimuth of the hole
• down hole length and interception
depth
• hole length.
If the exclusion of this information is
justified on the basis that the information
is not Material and this exclusion does not
detract from the understanding of the
report, the Competent Person should
clearly explain why this is the case.
Drill hole information is tabulated in
body text and/or shown in relevant
maps.
Data
Aggregation
Methods
In reporting Exploration Results, weighting
averaging techniques, maximum and/or
minimum grade truncations (e.g. cutting of
high grades) and cut-off grades are usually
Material and should be stated.
Where aggregate intercepts incorporate
short lengths of high-grade results and
longer lengths of low-grade results, the
procedure used for such aggregation
should be stated and some typical
examples of such aggregations should be
shown in detail.
The assumptions used for any reporting of
metal equivalent values should be clearly
stated
Intersections, where quoted are
weighted by length. Lengths originally
recorded in feet are quoted to the
nearest 10cm.
Estimates of ‘true width’ intersections
given where drilling is interpreted to
have a significant down-dip component.
Rounding is conducted to 3 significant
figures
A 500ppm Li cut-off was used to quote
headline intersections, with allowance
for 10ft of internal dilution by lower
grade material.
Low grade mineralisation (300-500ppm
Li) is present outside of the quoted
intersections
Intersections are quoted in both lithium
ppm and as wt% Lithium Carbonate
Equivalent (LCE). LCE is calculated as
LCE = Li (ppm) x 5.323 / 10,000, as per
industry conventions
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Section 2 Reporting of Exploration Results
Criteria JORC Code explanation Commentary
Relationship
between
mineralisatio
n widths and
intercept
lengths
These relationships are particularly
important in the reporting of Exploration
Results.
If the geometry of the mineralisation with
respect to the drill hole angle is known, its
nature should be reported.
If it is not known and only the down hole
lengths are reported, there should be a
clear statement to this effect (e.g. ‘down
hole length, true width not known’).
Insufficient information available due to
early exploration status, although
interpretation to date is that
intersections in this hole approximate
true width unless otherwise indicated.
Diagrams Appropriate maps and sections (with
scales) and tabulations of intercepts
should be included for any significant
discovery being reported These should
include, but not be limited to a plan view of
drill hole collar locations and appropriate
sectional views.
Included in ASX announcement.
Balanced
reporting
Where comprehensive reporting of all
Exploration Results is not practicable,
representative reporting of both low and
high grades and/or widths should be
practiced to avoid misleading reporting of
Exploration Results.
This release describes all relevant
information
Other
substantive
exploration
data
Other exploration data, if meaningful and
material, should be reported including (but
not limited to): geological observations;
geophysical survey results; geochemical
survey results; bulk samples – size and
method of treatment; metallurgical test
results; bulk density, groundwater,
geotechnical and rock characteristics;
potential deleterious or contaminating
substances.
This release describes all relevant
information
Further work The nature and scale of planned further
work (e.g. tests for lateral extensions or
depth extensions or large-scale step-out
drilling).
The Red Mountain lithium project is
emerging as a significant lithium
discovery in Nevada and is being
advanced toward a maiden Mineral
Resource Estimate later this year. It is
the Company’s intent to advance the
project beyond this to technical
studies.
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APPENDIX 2 – Red Mountain Drilling Sample Assay Table
Hole ID
From
(ft)
To (ft)
Li
(ppm)
LCE (%) Hole ID
From
(ft)
To (ft)
Li
(ppm)
LCE (%)
RMRC013 0 5 10.6 0.01 RMRC013 210 215 1010 0.54
RMRC013 5 10 22.8 0.01 RMRC013 215 220 830 0.44
RMRC013 10 15 102 0.05 RMRC013 220 225 809 0.43
RMRC013 15 20 286 0.15 RMRC013 225 230 174 0.09
RMRC013 20 25 969 0.52 RMRC013 230 235 67.5 0.04
RMRC013 25 30 523 0.28 RMRC013 235 240 45.1 0.02
RMRC013 30 35 347 0.18 RMRC013 240 245 242 0.13
RMRC013 35 40 264 0.14 RMRC013 245 250 300 0.16
RMRC013 40 45 163 0.09 RMRC013 250 255 1100 0.59
RMRC013 45 50 77.5 0.04 RMRC013 255 260 1150 0.61
RMRC013 50 55 98.7 0.05 RMRC013 260 265 1725 0.92
RMRC013 55 60 87.6 0.05 RMRC013 265 270 2160 1.15
RMRC013 60 65 86.6 0.05 RMRC013 270 275 2630 1.40
RMRC013 65 70 74 0.04 RMRC013 275 280 2500 1.33
RMRC013 70 75 106 0.06 RMRC013 280 285 1865 0.99
RMRC013 75 80 86.7 0.05 RMRC013 285 290 1980 1.05
RMRC013 80 85 46.3 0.02 RMRC013 290 295 1010 0.54
RMRC013 85 90 54.1 0.03 RMRC013 295 300 127.5 0.07
RMRC013 90 95 35.9 0.02 RMRC013 300 305 388 0.21
RMRC013 95 100 29.6 0.02 RMRC013 305 310 2750 1.46
RMRC013 100 105 40.7 0.02 RMRC013 310 315 1475 0.79
RMRC013 105 110 78.9 0.04 RMRC013 315 320 2130 1.13
RMRC013 110 115 61.2 0.03 RMRC013 320 325 4170 2.22
RMRC013 115 120 55.1 0.03 RMRC013 325 330 5240 2.79
RMRC013 120 125 84.9 0.05 RMRC013 330 335 5550 2.95
RMRC013 125 130 53.2 0.03 RMRC013 335 340 4900 2.61
RMRC013 130 135 84.2 0.04 RMRC013 340 345 4520 2.41
RMRC013 135 140 98.1 0.05 RMRC013 345 350 4750 2.53
RMRC013 140 145 88.7 0.05 RMRC013 350 355 5090 2.71
RMRC013 145 150 99.7 0.05 RMRC013 355 360 3960 2.11
RMRC013 150 155 204 0.11 RMRC013 360 365 5250 2.79
RMRC013 155 160 179.5 0.10 RMRC013 365 370 4670 2.49
RMRC013 160 165 211 0.11 RMRC013 370 375 2240 1.19
RMRC013 165 170 422 0.22 RMRC013 375 380 2130 1.13
RMRC013 170 175 531 0.28 RMRC013 380 385 4030 2.15
RMRC013 175 180 142 0.08 RMRC013 385 390 4560 2.43
RMRC013 180 185 107 0.06 RMRC013 390 395 3270 1.74
RMRC013 185 190 69.5 0.04 RMRC013 395 400 4010 2.13
RMRC013 190 195 1310 0.70 RMRC013 400 405 1295 0.69
RMRC013 195 200 3010 1.60 RMRC013 405 410 581 0.31
RMRC013 200 205 2600 1.38 RMRC013 410 415 695 0.37
RMRC013 205 210 2230 1.19 RMRC013 415 420 550 0.29
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Hole ID
From
(ft)
To (ft)
Li
(ppm)
LCE (%) Hole ID
From
(ft)
To (ft)
Li
(ppm)
LCE (%)
RMRC013 420 425 247 0.13 RMRC013 630 635 370 0.20
RMRC013 425 430 702 0.37 RMRC013 635 640 254 0.14
RMRC013 430 435 1010 0.54 RMRC013 640 645 405 0.22
RMRC013 435 440 3070 1.63 RMRC013 645 650 296 0.16
RMRC013 440 445 3730 1.99 RMRC013 650 655 163 0.09
RMRC013 445 450 3170 1.69 RMRC013 655 660 139.5 0.07
RMRC013 450 455 3010 1.60 RMRC013 660 665 592 0.32
RMRC013 455 460 2420 1.29 RMRC013 665 670 374 0.20
RMRC013 460 465 1385 0.74 RMRC013 670 675 216 0.11
RMRC013 465 470 2180 1.16 RMRC013 675 680 288 0.15
RMRC013 470 475 1140 0.61 RMRC013 680 685 1075 0.57
RMRC013 475 480 1400 0.75 RMRC013 685 690 447 0.24
RMRC013 480 485 1250 0.67
RMRC013 485 490 818 0.44
RMRC013 490 495 2900 1.54
RMRC013 495 500 907 0.48
RMRC013 500 505 703 0.37
RMRC013 505 510 313 0.17
RMRC013 510 515 366 0.19
RMRC013 515 520 424 0.23
RMRC013 520 525 678 0.36
RMRC013 525 530 508 0.27
RMRC013 530 535 411 0.22
RMRC013 535 540 345 0.18
RMRC013 540 545 868 0.46
RMRC013 545 550 267 0.14
RMRC013 550 555 200 0.11
RMRC013 555 560 262 0.14
RMRC013 560 565 1035 0.55
RMRC013 565 570 2100 1.12
RMRC013 570 575 1825 0.97
RMRC013 575 580 1235 0.66
RMRC013 580 585 1085 0.58
RMRC013 585 590 865 0.46
RMRC013 590 595 589 0.31
RMRC013 595 600 375 0.20
RMRC013 600 605 1155 0.61
RMRC013 605 610 603 0.32
RMRC013 610 615 390 0.21
RMRC013 615 620 305 0.16
RMRC013 620 625 1090 0.58
RMRC013 625 630 870 0.46
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