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EPM 16321 – PANDANNUS

COMBINED ANNUAL/ FINAL REPORT

For the Period

26 March 2008 to 31 March 2009

Author Paul Dwyer

April 2009

1:250,000 Sheet:Clarke River(SE 55-13)

GLENGARRY RESOURCES LIMITEDABN 40 009 468 099

EPM 16321 PandannusCombined Annual/ Final Report, 29 April 2009

SUMMARY

EPM 16321 (Pandannus) is located about 211 kilometres west of Townsville in north Queensland and 50 kilometres south west of the town of Greenvale. The Greenvale area is considered prospective for epigenetic structurally controlled copper mineralisation, volcanogenic massive sulphides as well as intrusive related disseminated gold mineralisation (Kidston style) and high-grade gold mesothermal vein style mineralisation.

The tenement, granted on 26th March 2008, is held 100% by Glengarry Resources Limited and forms part of the company’s Greenvale project.

Exploration undertaken by Glengarry Resources over the relinquished portion has consisted of open file data review, interpretation of publicly available aeromagnetic and radiometric data, limited rock chip sampling and geological traverses.

No anomalous target areas were identified hence the 4 sub-blocks of EPM16321 were recommended for relinquished on the 23rd of March 2009

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Table of Contents

1.0 INTRODUCTION..................................................................................................1

2.0 TENEMENT..........................................................................................................2

3.0 GEOLOGY AND MINERALISATION...................................................................4

4.0 WORK CARRIED OUT DURING THE REPORTING PERIOD...........................4

Data Compilation/Review 4

Aeromagnetic/Radiometric Interpretations 4

Geological Traverses/ Rock Chip Sampling 5

5.0 DISCUSSION OF EXPLORATION ACTIVITIES.................................................7

6.0 CONCLUSION/ RECOMMENDATION................................................................7

7.0 REFERENCES.....................................................................................................7

LIST OF FIGURES

Figure 1: Location Plan Greenvale Project and EPM16321 (Pandannus) Figure 2: Relinquished sub-blocks Pandannus EPM16321Figure 3: Glengarry Rock Chip Sampling over relinquished EPM16321 Figure 4: Open file >18ppb Au in soil anomalyFigure 5: Pandannus 100k Geology

LIST OF TABLES

Table 1: Glengarry’s tenement listing for EPM16321 Pandannus

LIST OF APPENDICESAppendix 1: Rock Chip/Float Sample Assays* Appendix 2: Geochemical Sample Results Appendix 3: Glengarry Rock Codes

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GREENVPROJECT

PANDANNEPM16

(Wando Vale

-19.7 °

° °

-18.6 ° -18.6 °

(Spring Creek (Gilldale

-18.7 ° -18.7 °

(Carpentaria Downs

(Wyandotte-18.8 ° -18.8 °

(Kidston-18.9 ° -18.9 °

(Lucky Do

-19 ° -19 °

-19.1 ° -19.1 °

-19.2 °(Lyndhurst -19.2 °

-19.3 °

GREENVALEPROJECT AREA

(Pandanus EPM1-6192.33°1

-19.4 ° -19.4 °

-19.5 ° -19.5 °

-19.6 ° -19.6 °

(Cheviot Hills

-19.7 °(Gregory Springs

(Clarke Hills

-19.8 °

PANDANNUS

Date:20/4/2009Pandannus Location MapAuthor: PAUL DWYERQueensland

Glengarry Resources LtdOffice: PERTH

Drawing: 1.1

Scale: 1:500000 Projection: Longitude / Latitude (AGD 84)

5 0kiillomettrres

5 10


1.0 Introduction

Exploration Permit for Minerals (EPM) 16321 is located about 211 kilometres west of Townsville in north Queensland and 48 kilometres south west of the town of Greenvale (Figure 1). The area is considered prospective for epigenetic structurally controlled disseminated copper mineralisation (Maitland style), volcanogenic massive sulphides as well as intrusive related disseminated gold mineralisation (Kidston style) and high- grade gold mesothermal vein style mineralisation.

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Figure 1: Location Plan Greenvale Project and EPM16321 (Pandannus)

2.0 Tenement

EPM 16321, granted for a five-year term on 26 th March 2008, is held 100% by Glengarry Resources Limited. The tenement was granted over 4 sub-blocks (Figure 2).

Details on the tenement sub-blocks are presented below:

BIM BLOCK Sub-blocksTOWN 2890 M,Q,R,W

Table 1 Glengarry’s tenement listing for EPM16321 Pandannus

2

-19.44 °

TOWN2962J

-19.45 °

°

°

-19.34 °-19.34 °TOWN2889ETOWN2890ATOWN2890BTOWN2890CTOWN2890DT

-19.35 ° -19.35 °

TOWN2889K TOWN2890F TOWN2890G TOWN2890H TOWN2890J T-19.36 °-19.36 °

-19.37 ° -19.37 °

TOWN2889P TOWN2890L TOWN2890M TOWN2890N TOWN2890O T

-19.38 ° -19.38 °

-19.39 ° -19.39 °

TOWN2889U TOWN2890Q TOWN2890R TOWN2890S TOWN2890T T

-19.4 ° -19.4 °

-19.41 °TOWN2889Z TOWN2890V T WN2890W TOWN2890X TOWN2890Y

-19.41 °T

-19.42 ° -19.42 °

TOWN2961E TOWN2962A TOWN2962B TOWN2962C TOWN2962D T

-19.43 ° -19.43 °

-19.44 °

TOWN2961K TOWN2962F TOWN2962G TOWN2962H

-19.45 °

50005001,000metres


EPM16231 BLOCK MAPDate:20/4/2009 PANDANNUSAuthor: PAUL DWYER QUEENSLAND

Office: PERTH GLENGARRY RESOURCES

Drawing: 1.2

Scale: 1:50000 Projection: Longitude / Latitude (AGD 84)

Figure 2: Relinquished sub-blocks Pandannus EPM16321

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3.0 Geology and Mineralisation

The geology of the EPM16321 is dominated by mid to late Devonian and early Carboniferous sedimentary sequences of the Broken River and Bundock Groups. The Mytton Formation and the Bulgeri formation are the two dominant formations from each group.

Mytton Formation: Part of the Broken River group and and consists of an arenite/ mudstone conglomerate.

Bugeri formation: In particular the Rockfields member, consists of well sorted, fine-medium-grained sandstones. This sequence is known to contain less lithic grains then the underlying Mytton Formation.

A number parallel north-westerly trending dolerite dykes have been mapped to the south of the current EPM. Some of these dykes have been mapped for up to 4km. The dykes appear to truncate all other stratigraphy allowing some constraints on age.

A series of north-easterly trending fault zones transect the stratigraphy within the EPM (Figure 5). These faults are believed to have been active during the Permian- Carboniferous and dominate the present day litho-structural assemblage. These NE trending fault sets are parallel to the main fold axis. The faults commonly truncate the limbs of folds. It is believed that the faults may be high angle thrust faults related to the NW dipping of overturned folds in that area. Other studies believe there may be a strike–slip movement on these fault sets that would explain the juxtaposition to the Dip Creek limestones.

The Rockfields Anticline is observed within the current EPM. This south-westerly plunging synformal-anticline is potentially a regional structural response from continent wide N-S compression in the Carboniferous.

The sediments of the Bundock Creek formation were once prospective for Uranium in the 1970’s. The Big Rush gold deposit consists of shear related quartz veins within the Mytton Formation of the Broken River Group. The deposit had a reserve of 880000t of ore with a grade of 2.06g/t gold at a cut off grade of 0.6g/t gold. No known mineralisation occurs within the EPM.

4.0 Work Carried Out During the Reporting

Period Data Compilation/Review

Historical rock chip sampling data was compiled and reviewed to assist with targetselection within the EPM. No anomalous target areas were defined within the relinquished portion.

Aeromagnetic/Radiometric Interpretations

Interpretation of available Government aeromagnetic and radiometric datasets was completed by Glengarry enabling the company to refine its 100,000 scale litho- structural interpretation of the project (Figure 5).

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Geological Traverses/ Rock Chip SamplingGlengarry’s ground exploration was limited to rock chip sampling and geological traverses. A total of 9 rock chip samples were collected over the Pandannus EPM. Rock chips were collected predominantly from narrow quartz veins. Complete assay sample results and sample descriptions are presented in Appendix 1.

Glengarry’s standard rock chip codes are presented in Appendix 2.

Sample AnalysisAll samples were analysed by ALS Chemex in Townsville for As, Ba, Bi, Co, Cu, Fe, Mn, Sb, Th, V, W, Pb, S, and Zn using ME-ICP41 and Ag, Mo and U using ME-MS42. Gold was assayed by method Au-AA21.

5

-19.42 °

°

°

-19.37 ° -19.37 °

-19.38 ° -19.38 °

-19.39 ° -19.39 °

-19.4 ° -19.4 °

-19.41 ° -19.41 °

-19.42 ° GLENGARRY RESOURCESDate:29/4/2009Author: P. Dwyer Office: PerthGGY Rock Chip sample locations Pandannus EPM16231 Queensland

Australia

Drawing:

Scale: 1:25000 Projection: Longitude / Latitude ( Australia GDA94)

2500250500

metres


Figure 3: Glengary Rock Chip Samples over relinquished EPM16321

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5.0 DISCUSSION OF EXPLORATION ACTIVITIES

Work completed by Glengarry Resources within the relinquished EPM16321 included research and interpretation of previous exploration companies’ data and field reconnaissance.

The review of previous exploration data allowed Glengarry to identify initial geochemical sampling targets. In the winter of 2008 Glengarry carried out a field reconnaissance programme that consisted of geological traverses together with selected rock chip/ rock float sampling.

Geological traverses identified a haematite stained quartz stockwork hosted within carbonate siltstone. Nine selective rock chip samples were taken over this stock work system, yielding a peak Au concentration of 1.59ppm. No evidence for a large scale Au bearing stockwork system was found and exploration over the tenement ceased.

6.0 CONCLUSION/ RECOMMENDATION

Given the reasonable data coverage, disappointing results returned from the selective rock chip sampling programme and the sudden global financial crisis hampering exploration efforts, it was decided to relinquish EPM16321.

7.0 REFERENCES

Geological Survey of Queensland, 1996: 1:250000 Geological series – Explanatory Notes, Clarke River (Second Edition)

7

-19.42 °

-19.37 ° -19.37 °

-19.38 ° -19.38 °

-19.39 ° -19.39 °

18ppbAu Soil Anomaly

-19.4 ° -19.4 °

-19.41 ° -19.41 °

222525505000 0000222525505000 5550500000

mmmeeetttrrrtttrrrttterrreesssmetr es

-19.42 °GLENGARRY RESOURCESDate:29/4/2009Author: P. Dwyer Office: PerthOpen file Au Soil Anomaly EPM16231 Pandannus Queensland

Australia

Drawing:

Scale: 1:25000 Projection: Longitude / Latitude ( Australia GDA94)


Figure 4: Open file stream sediment plus drill hole collar data summary over relinquished portion of EPM12510.

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-19.5 °

°5°2

-19.475 °

-19.5 °

° 7

-19.3 ° -19.3 °

-19.325 ° -19.325 °

-19.35 ° -19.35 °

-19.375 ° -19.375 °

-19.4 ° -19.4 °

-19.425 ° -19.425 °

-19.45 ° -19.45 °

Simplified Geology

RECENT TAILINGS ETC

QUATERNARY ALLUVIUM

QUATERNARY BASALT

-19.475 °

TERTIARYARENITE-MUDROCK

M. JURASSIC - E. CRETACEOUS ARENITECARBONIFEROUS FELSITES

L. DEVONIAN - E. CARBONIFEROUS ARENITE-MUDROCK

SILURIAN DIORITE

E. - M. DEVONIAN ARENITE

L. CAMBRIAN - E. ORDOVICIAN CHERT

100K Regional GeologyDate:20/4/2009EPM16231 PANDANNUS

CAMBRO- ORDOVICIANGRANITOIDAuthor: PAUL DWYER

E. PROTEROZOIC - CAMBRIAN CARBONATES

QUEENSLANDGLENGARRY RESOURCES

Office: PERTH

PALAEOPROTEROZOICMAFITES

NEO/EARLY. PROTEROZOIC GABBROID

Drawing: 1.2

Scale: 1:100000 Projection: Longitude / Latitude (Australia GDA94)MESOPROTEROZOIC111000111 222GRANITOID

kilometres

EPM16231Pa nda nnus


Figure 5: Pandannus 100K Geology

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APPENDIX 1

Rock Chip/Float Sample Data

APPENDIX 2

Geochemical Sample Results

APPENDIX 3

Glengarry Rock Codes

Appendix 1: Rock Chip/Float Sample Assays*

*all rock chip/ float sample assays forwarded as .csv files

Appendix 2: Geochemical Sample Results

Appendix 3: Glengarry Rock Code

SIMPLIFIED GEOLOGICAL TIMETABLEERA SYSTEM SERIES

CZ CENOZOIC QT

QUATERNARY HO PL

Holocene Pleistocene

TY TERTIARY PO

M

C

OL

EO

PA

Pliocene

Miocene

Oligocene

Eocene

Palaeocene

MZ MESOZOIC KT

JR

TR

CRETACEOUS

JURASSIC

TRIASSIC

PZ PALAEOZOIC P

M

CB

DV

SL

OV

CM

PERMIAN

CARBONIFEROUS

DEVONIAN

SILURIAN

ORDOVICIAN

CAMBRIAN

PC PRECAMBRIAN PR

PROTEROZOIC P3

P2

P1

Late

Middle

EarlyA ARCHAEAN A3

A2 A1

LateMiddle Early

SCHEMATIC REGOLITH PROFILE

PED

OLI

TH

SOIL / SCREEINDURATED HARDPANLATERITIC DURICRUST

MOTTLED ZONE

PLASMIC [amorphous clay]

or ARENOSE

ZONE CLA

YZO

NE

SAPR

OLI

TH SAPROLITE

SAPROCK

FRESH BEDROCK

2.0 WEATHERING + ROCK CODES2.1 Pedolith Weathering Codes 2.2 Sarpolith Rock Codes

Residual Rock1/Rock2

Lf

Lm Lc Lk Ls Lr Fr

Duricrust insitu over bedrock

Erosional

Mottled Zone Clay Zone Clay SaproliteSaprolite >20% weatheredSaprock <20% weathered Fresh Rock

Ca Cc Ccl Cco Cg Cl Cm Cw Cp CvCs

Alluvium Colluvium Colluvial LagColluvial Soil bGlacial deposit fLacustrine Deposits iMarine Deposits sAeolian Deposits

m Playa DepositsEvaporitic DepositsFluvial Sand Deposits

Suffixes calcareous ferruginousferruginous+silicified silicifiedmottled, ferruginous

LgLx

GossanRedox Front Xo Undifferentiated soil

Depositional Cx Contaminated, disturbed ground

Chc Chv ChfChs

Calcrete - pedogenic Calcrete - groundwater FerricreteSilcrete

El Eo Eof

Erosional Lag Erosional Soil Erosional Lateritic Soil

Eg Erosional GossanUndifferentiated

Xf Ferricrete - unknown origin

3.0 LITHOLOGY CODES3.1 FELSIC 3.1 FELSIC (lower grade) 3.1 FELSIC (high grade)F

F

v F

e Fi

Ft Fl

Fx

Ff

Felsic undifferentiated

Felsic coherent undivided Felsic extrusive

Felsic intrusive

Felsic tuff

Felsic lapilli tuff Felsic breccia

Felsic volcaniclastic, undivided

Fsc

Fqm

Fqb

Felsic schist, undivided

qtz-fpr-mus schist/rock qtz-fpr-bio schist/rock

Fsc

Fqm

Fqb Fn

Fr

Felsic Schist, undivided

qtz-fpr-mus schist/rock qtz-fpr-bio schist/rock

Felsic gneiss

felsic granulite

Fg Fg

a Fa

p Fg

g Fgt

Fgd

Fgy Fg

p Ffp

Fqz Ffq

Fqf Fvd

FvhFvr

Felsic granitoid, undivided

AdamelliteAplite

Syenogranite, monzogranite, alkali feldspar granite

Tonalite, trondhjemite

Granodiorite

Granophyre Pegmatite

Felspar porphyry Quartz porphyry

Felspar quartz porphyry

Quartz felspar porphyry

DaciteRhyodaciteRhyolite

Fgn Granitoid gneiss

3.2 SEDIMENTARY 3.2 SED (lower grade) 3.2 SED (high grade)S Sedimentary undifferentiated

Sx Sc

Sedimentary breccia Conglomerate

Sp Sl

Psammite, undivided Pelite, undivided

Sp Sl

Psammite, undivided Pelite, undivided

Sps Spt Sms Slc Sct Sif Sbl Sbd

Sandstone Siltstone Mudstone Claystone ChertBanded iron formation LimestoneDolomite

Ssh Ssy

Shale Phyllite

Ssq Sbm Sn

Quartzite MarbleSedimentary gneiss

Scs Sgw

Calc-silicate Greywacke

Spg Stl

Spongolite Tillite

3.3 INTERMEDIATE 3.3 INT. (lower grade) 3.3 INT. (high grade)I Intermediate undifferentiated

Iv I

Intermediate coherent undivided Intermediate extrusive Intermediate intrusive

Isc Ibc Im

Int. schist, undivided plg-cht-bio schist/rock plg-cht-mus schist/rock

Isc Iab

Int. schist, undivided plg-amp-bio schist/rock

e Ii

c

It Il Ix If

Intermediate tuff Intermediate lapilli tuff Intermediate brecciaIntermediate volcaniclastic, undivided

In Ir

Intermediate gneiss Intermediate granulite

Id Im

DioriteMonzodiorite, monzogabbro

3.4 MAFIC 3.4 MAFIC (lower grade) 3.4 MAFIC (high grade)M Mafic, undifferentiatedMb Basalt Msc Mafic schist, undivided Msc Mafic schist, undividedMbm High Mg basalt Mcc cht-crb schist/rock Msb Mafic schist - biotiteMt Mafic tuff Mac cht-amp schist/rock Mm AmphiboliteMf Mafic fragmental Mn Mafic gneissMx Mafic breccia Mr Mafic granuliteMd DoleriteMg GabbroMa AnorthositeMc TrocoliteMh Hornblendite

3.5 ULTRAMAFIC 3.5 U/M (lower grade) 3.5 U/M (high grade)U Ultramafic undifferentiated

Uf Ud Upd Uk UpxUs

Ultramafic fragmental DunitePeridotite Komatiite PyroxeniteSerpentinite

Usc Utc Utb Uts Uac Uta

Um schist, undivided tlc-cht-crb schist/rock tlc-crb schist/rocktlc-srp schist/rock trm-cht schist/rock tlc-trm schist/rock

Usc Uac Uta Utf Uaf Ufa

Um schist, undivided trm-cht schist/rocktlc-trm-crb schist/rock tlc-for schist/rocktrm-for rock tlc-for-ant rock

3.6 ALKALINEAc Ak Al AtAs

Carbonatite Kimberlite Lamprophyre TrachyteSyenite

3.7 TECTONIC + MISCELLANEOUS UNITSTc Cataclasite 2nd/3rd letter

qualifiersl leucoq quartzo oligomicticp polymictic

Tx Tectonic brecciaTm MyloniteVMSHx X

VeinMassive sulphidesHydrothermal breccia Unknown rock unit

4.0 STRUCTURAL & TEXTURAL CODESRegolith

bleached adccellular amyconcretionary aphearthy eqgfragmental glsfriable gpygossanous hylindurated ocllaminated ospmegamottled ophmottled orcnodular pgmoolitic plwpisolitic pphplastic psppoddy soppowdery sphstratiform sptsorted mscunsorted tufvermiform varvein-like vesvoided vfrcross-cutting xln

Sedimentary

bedded bndthinly bedded brxthickly bedded cokcross bedded colgraded bedded cmbsorted cruunsorted fib

lam mas

Colours(prefix l - light; d - dark, eg dbu = dark blue) blue gyblack khbrown mvcream orgreen pk

Igneous Metamorphic

ble adcumulate aci acicularcel amygdaloidal asb asbestiformcon aphanitic bld bladedear equigranular dcs decussatefrg glassy bnd bandedfri granophyre fib fibrousgos hyaloclastic gns gneissicind ocellar grn granoblasticlam olivine spinifex hnf hornfelsedmgm ophitic lpd lepidoblasticmot orthocumulate poc porphyroclastsnod pegmatitic pob porphyroblastsool pillowed sch schistosepis porhyyriticpla pyx spinifex Structuralpod subophiticpod spherulitic brx brecciatedstf spotted crn crenulatedsor mesocumulate fol foliateduns tuffaceous frc fracturedver variolitic lin lineatedvnl vesicular mas massivevoi volcanic fragments myl myloniticxct crystalline shr sheared

Veining (use for vein logging)

bdd banded rib ribbonbdn breccia sac saccharoidalbdk cockade spi spidercbd colloform sht sheetedgbd comb stk stockworksor crustiform str stringeruns fibrous sty stylolitic

laminated vug vuggymassive zon zoned

bu grey pp purplebk khaki rd redbr mauve wh whitecrgn

orangepink

ye yellow

5.0 MINERAL COMPONENTS & ALTERATIONRock Composition and Alteration Codes

act actinolite fer ferruginous phl phlogopiteadu adularia flt florite pis pisolitesaeg aegirine for forsterite plg plagioclasealb albite fuc fuchsite pre prehnitealu alunite gal galena ptl pentlanditeamp amphibole gnt garnet pyr pyritesbs antimony sulphides gib gibbsite pyx pyroxeneamo orthoamphibole goe goethite pyo pyrrhotiteand andalusite gld gold qtz quartzany anhydrite grp graphite ros roscoeliteank ankerite gvl gravel rbl rubbleant anthophyllite gru grunerite rut rutileapt apatite gyp gypsum snd sandapy arsenopyrite hal halite sau saussuriteazu azurite hed hedenbergite sca scapolitebar barite hem haematite sch scheelitebio biotite hbd hornblende ser sericitebis bismuth minerals jar jarosite srp serpentinecal calcareous kfp K feldspar sid sideritecct calcite kln kaolin sil silicacrb carbonate kyn kyanite slm sillimanitecas cassiterite pb2 lead minerals sme smectitechy chalcedony lep lepidolite spl sphaleritecha chalcocite lcx leucoxene spd spodumenecpy chalcopyrite lim limonite str staurolitecht chlorite mgm maghaemite slf sulphidesctd chloritoid mgs magnesite tlc talcchr chromite mnt magnetite tan tantalitecly cly minerals mal malachite tel telluridescps clinopyroxene mng manganese tit titanitecu2 copper oxides mcs marcasite tml tourmalinecrd cordierite mic mica trm tremolitecry chrysotile mol molybdenite tra tremolite-actinolitextl crystal mus muscovite wol wollastonitecum cummingtonite ni2 nickel clays vit vitricdps diopside non nontronite urn uraninitedol dolomite olv olivine cu1 native copperepd epidote opx orthopyroxene car carnotitefpr feldspar oxs oxide minerals

Alteration Summary Codes Alteration/Sulphide Styles

aa advanced argillic - sil, alu, pyr d disseminatedad adularia - kfp, sil, ser, fer, slf m massive, pervasiveag argillic - cly, kln, sid, ser, slf v veinsas aluminosilicate - and, ctd, crb, mus, cht, slf, qtz s stockworkap amphibole - amp, tlc, slf l lodesbi biotite - bio, cht, crb, amp, sil p pods, patchesbc biotite-chlorite - bio, cht, crb, slf f foliation controlledcs calc-silicate - dps, gnt, plg, amp, slf, crb b bands, bed controlledcb carbonate - crb, cht, tlc, slfct chlorite - cht, slf, ser, crbep epidote - epd, crb, qtz, slf Grain Sizefe ferruginous - mnt, cht, act, crb, qtz, slfgn greissen - ser, sil vfg very fine grainedhm haematisation - hem, alb, qtz, slf, crb fg fine grainedkp K-feldspar - kfp, qtz, sil mg medium grainedmg magnesian - crd, ant, plg, slf cg course grainedpg plagiocklase - plg, qtz, bio, slf vcg very course grainedkb potassic-biotite - bio, crb, qtz, cht, mus, slfkm potassic-muscovite - mus, bio, cht, crb, qtz, slf Intensity codeskc potassic-calcsilicate - bio, amp, plg, slf, crbkg potassic-magnesian - bio, crd, qtz, plg, cum, gnt, crb, slf T tracepp propylitic - sil, cht, epd, crb, slf W weakna sodic - alb, mus, crb, qtz, slf M moderatenc sodic-calcic - plg, amp, dps, qtz, slf, tit S strongse sericite - ser, crb, slf E extremesc sericite-chlorite - ser, cht, crb, qtz, slfsi silicification - qtz, crb, slfsf sulphidisation - slftl talc - tlc, amp, slftc talc-chlorite - tlc, cht

Sample Recovery + Sulphide Percentage

Record percentage estimate. Use -1 to define trace %

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