Avala Resources Ltd. (TSX VENTURE: AVZ) (the "Company" or "Avala") is pleased to present an update on the Korkan target area, part of the sediment hosted gold belt within the Cretaceous magmatic arc bordering the Timok Magmatic Complex ("TMC") in Eastern Serbia.

1.  HIGHLIGHTS

--  Surface trenches on the Korkan target area have outlined an erosional
    window into the strongly gold mineralised target stratigraphy.
--  The Korkan target area, as currently defined by gold surface
    geochemistry, is approximately 4.5 km in length and up to 1 km wide and
    is underlain by Jurassic limestone, conglomerates and sandstone with
    varying carbonate content.
--  Trench sampling of the Korkan target area returned the following wide,
    high-grade gold intercept (0.4g/t cut-off grade):

    --  140m @ 2.67g/t
        --  Including: 74m @ 4.27g/t
--  The trench sampling follows up and confirms the initial 'discovery'
    trench (JASTR009), excavated in 2008 which returned the following
    intersections:
    --  59m at 2.50g/t and
    --  58m at 2.61g/t.

--  Avala controls 100% of the newly identified sediment hosted gold belt
    which totals approximately 250 sq km.
--  Gold deposits in the Republic of Serbia are subject to a 3% NSR.
--  Avala intends to systematically drill test all currently defined
    priority target areas. See Figures 1 and 2 at the end of this release
    for additional detail.

GEOLOGY AND MINERALIZATION STYLE

Sediment hosted gold, located along the western margin of the Timok Magmatic Complex, represents a previously unrecognized style of gold mineralization within the Timok region.

Geological mapping of the sediment hosted gold belt suggests mineralization is associated with a complex lithological and structural sequence of limestone/marble, calc-silicate hornfels, biotite-magnetite hornfels, monzonite (pre-ore Potoj Cuka stock), diorite dykes, andesitic volcanic and volcaniclastic rocks, schists, conglomerates, sandstones and tuffaceous sedimentary rocks.

The belt is extensively faulted and intruded by numerous diorite and monzonite complexes with associated thermal metamorphic aureoles, indicating the potential for sufficient permeability and rheologic contrast for fluid movement and hydrothermal deposition.

The Korkan target area is underlain by massive Jurassic limestone, overlain by a quartz pebble conglomerate and sandstone sequence with a carbonate matrix component which is the host to the strongly mineralised interval intersected by the surface trenches. The quartz pebble conglomerate is overlain by a carbonate-clast conglomerate which is not mineralized. Avala currently believes that this 'cover sequence' may postdate the gold mineralising event (a similar 'cover sequence' unit is present between the Umka and Strnjak target areas; see Figure 1). The quartz pebble conglomerate and sandstone unit appears to dip moderately (approx.40 degrees ) towards the south-south west under the 'cover sequence' and towards the Bigar target area.

The Korkan target area represents possible stratabound sediment hosted gold mineralization within a favourable sedimentary unit; the quartz pebble conglomerate.

The strongly mineralised interval cut in surface trench KOTR033 is generally oxidised and the effects of supergene processes are currently not known.

Figure 1 shows the Korkan target area within the larger sediment hosted gold belt together with the locations of the newly defined 'cover sequence'.


3.  TRENCH

--  The recently completed trench program at Korkan consisted of 1,658
    meters for 829 samples and was designed to follow up a previous high
    grade trench (JASTR009) defined during the initial wide spaced (nominal
    800m spacing) trench program and to help refine geological contact
    relationships due to the poor exposure in the area.
--  KOTR033 was designed orthogonal to the high-grade (JASTR009) trench due
    to the recognition that the initial trench was not favourably located to
    be representative of the true width of the quartz pebble conglomerate
    unit.
--  Table 1 details trench intercepts at a range of cut-off grades for the
    Korkan sediment hosted gold target area.
--  Figure 2 displays the location of trench sampling to date and shows the
    recently completed program together with the geology in the Korkan
    target area.
--  Highlights from the Korkan target area include the following trench
    intercepts (0.4g/t Au cut-off grade):

--  KOTR033: 140m @ 2.67g/t

--  Including:
    --  74m @ 4.27g/t
    --  18m @ 1.19g/t
    --  6m @ 2.10g/t
    --  6m @ 1.38g/t

4.  DISCUSSION

--  A major sediment hosted gold belt bordering the western boundary of the
    Timok Magmatic Complex identified by soil and trench samples extends
    over 20 km along strike and is approximately 8 km wide.
--  The geology, geochemistry and available drill intersections suggest a
    strong similarity to the style of gold mineralization typified by the
    North Carlin Trend, Nevada, USA.
--  At Korkan, recently completed trenches have outlined significant gold
    associated with quartz pebble conglomerates and sandstone with a
    carbonate matrix component. The outcropping area of gold mineralisation
    is a small (170 meter x 120 meter) erosional window into the target
    stratigraphy.
--  The recognition that the Korkan and Bigar target areas are separated by
    a 'cover sequence', which appears to be post-mineral has significant
    implications for the gold potential of the sediment hosted gold belt.
--  Initial drill testing of the Korkan stratabound sediment hosted gold
    target area should commence in the first week of November 2010.
--  Trenching programs will continue on multiple target areas within the
    sediment hosted gold belt in order to define the extents of the
    anomalous gold and to further define priority target areas to be drilled
    as soon as the results of the current trench programs are received and
    interpreted.
--  Further geophysical modelling along with detailed geological mapping are
    underway.

SAMPLING AND ANALYSIS

The majority of soil samples have been assayed at the ALS Chemex laboratory, Perth, Australia. More recent programs have been assayed at the SGS managed laboratory at Chelopech in Bulgaria using a combination of ICP-OES and ICP-MS whereas gold has been assayed by low level detection fire assay method with an AAS finish. Trench samples were prepared at the SGS managed laboratory facility at Bor, Eastern Serbia and the samples have been assayed at the SGS managed laboratory at Chelopech in Bulgaria or the SGS managed laboratory facility at Bor, Eastern Serbia. Following Avala standard procedures, a full suite of field and laboratory duplicates and replicates along with internationally accredited standards have been submitted with each batch of samples.

Trench sampling was carried out as channels in the wall just above the trench floor on 2m intervals. Except where extensive soil cover is encountered, trenches were sampled in their entirety. The samples were routinely weighed prior to final bagging to maintain an even sample size and to avoid sampling bias in harder rock types. An average channel sample weight was maintained at 3kg/m, which produces a consistent sample weight approximating half HQ core samples. Field duplicate samples were taken every 20 samples and known standards were inserted into the sample stream after every 20th sample. A geological and structural log was completed as for diamond drilling. All data collected in the field was routinely entered into geology and structural geology spread sheets using Field Marshal software for subsequent entry to an acQuire database and validation.

Dr. Julian F. H. Barnes, a qualified person under National Instrument 43-101, a Director and the Company's Special Consultant, has supervised the preparation of the technical data in this press release.

Previously released data refers to data included in the "Potoj Cuka Gold Project, Serbia National Instrument 43-101 Technical Report" by Paul Mazzoni dated March 10, 2010 (the "Technical Report"), filed on SEDAR at www.sedar.com. Further information in respect of results, investigations, interpretations, quality assurance and quality control measures, along with geology, mineralogy, sampling, and analytical procedures is included in the Technical Report."

About Avala Resources Ltd.

Avala is a recently-formed company focused on the exploration and development of the Potoj Cuka sediment hosted gold project and the Timok gold-copper project in Serbia. The common shares of Avala trade on the TSX Venture Exchange under the symbol AVZ.

Avala is well-capitalized, with approximately $19.6 million in its treasury at July 30, 2010, which it plans to use for the exploration and development of its mineral projects in Serbia. Avala's issued and outstanding share capital totals 146,284,237 common shares, of which approximately 50.2% is held by Dundee Precious Metals Inc. (TSX: DPM).

This press release contains forward-looking information. Although the Company believes in light of the experience of its officers and directors, current conditions and expected future developments and other factors that have been considered appropriate that the expectations reflected in this forward-looking information are reasonable, undue reliance should not be placed on them because the Company can give no assurance that they will prove to be correct. Forward looking information in this news release includes statements regarding the nature of the mineralization of the project, the results of the exploration activities and interpretation of such results, and timing and location of future work programs. Forward-looking information involves known and unknown risks, uncertainties, assumptions and other factors that may cause actual results or events to differ materially from those anticipated in such forward-looking information. The forward-looking statements contained in this press release are made as of the date hereof and the Company undertakes no obligations to update publicly or revise any forward-looking statements or information, whether as a result of new information, future events or otherwise, unless so required by applicable securities laws.

Maps and table are available at the following address: http://media3.marketwire.com/docs/avala.pdf

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this press release.

Contacts: Avala Resources Ltd. James Crombie President and Chief Executive Officer 450-640-0810 jcrombie@avalaresources.com www.avalaresources.com