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Message: Gold World Resources Discovers Six Highly Anomalous Zones Indicating a Potential
Gold World Resources Discovers Six Highly Anomalous Zones Indicating a Potential for Bulk Mining

TORONTO, Oct. 27, 2011 /CNW/ - Gold World Resources Inc. (TSXV:GDW) or ("the "Company") is pleased to report that it has located six anomalous zones on its Mount Anderson, Yukon property with exceptionally high MMI™ ("mobile metal ion") response levels for precious and base metals (see note on chart below). The anomalies have been located by plotting the results of all 4,625 Mount Anderson soil sample. The results indicate a major zoned area of mineralization extending from the Rob Skarn to the Fleming Skarn that is more than 6,000 meters across with a gold-enriched core approximately1,750m by 400m wide (see attached map or website www.goldworldresources.com). There is no record or evidence of any past exploration at three of the six strong anomalies within the zoned area.

Anomaly A, a strong 1250m by 750m NW-trending Au-Ag-As anomaly located on the west slope of Mt. Anderson merges with Anomaly B, an equally prominent 500m by 250m Au-Ag-Zn-Pb anomaly with high MMI values and is surrounded further out by areas of moderately anomalous Zn and Cu creating a pattern of zoning that appears to fit the model described by Hart et al* for bulk mineable intrusion-related deposits such as at Fort Knox Mine, Alaska (operated by Kinross). Soil survey lines 35 and 36 (see news release dated August 11, 2011) fortuitously crossed the central portion of these two clusters showing very anomalous values and extending northwest for 1,750 meters (1*).

1) Anomaly A (²*): Au-Ag-As cluster of high anomalous values 1 250m by 750m is untested by past trenching, adit mining or drilling;
2) Anomaly B: Au-Ag-Zn-Pb cluster of high anomalous values 500m by 250m continuing eastward from Anomaly A and encompassing the area of former adit mining;
3) Anomaly C: A narrow E-W Au-Ag anomaly with high Pb and locally high Cu extends east for 1,200 meter from Anomaly B;
4) Anomaly D: Strong Au-Ag-Pb-As anomaly 400 by 800 m in the north central portion of the property; No record or evidence of past exploration has been found at this site.
5) Anomaly E: High Sb-Ag-As in the general area of the Fleming Skarn and extending E-W for 800 m and for as much as 250 m N-S. No record or evidence of past exploration has been found at this site.
6) Anomaly F: Strong Au-Ag-Pb anomaly fringed by moderately high Sb, Zn and Cu values

(²*)Exploration in the late 1980's found significant (not NI43 101 compliant) anomalous gold and silver in soil and bedrock along the north margin of the Anomaly A. In a 1987 assessment report (091948, H. Keyser, 1987) it is stated that "Mineralization has only been found as float at or near the outcrop on the ridge-top west of Mt. Anderson. It is believed to be a new discovery. Selected samples of this float have returned up to 6.273 oz/t gold and 15.21 oz/t silver." NOTE: Additional analyses results are awaited on nine randomly chosen rock chip samples collected from this area in August by Dallas Davis and will be available a.s.a.p.

(1*)The Au-Ag-As portion of the 1,750-m A & B Anomalies extends along the slope of Mt. Anderson from the portals of the easterly-driven adits from which ore was extracted in the 1906-15 period and processed in a mill discovered this summer by the Company's field team. This anomalous area is underlain by an altered and fractured granodiorite and is cut by numerous E-W and NW-trending dikes and a prominent NE-trending rhyolitic dike-like body which, at the north end of Anomaly A, has been mapped by past explorers as terminating in a plug-like rhyolitic body. Early Eocene Rhyolite dikes of the Skukum Group were mapped in this area by Hart and Radloff**. The association of the rhyolite with epithermal gold veins of the Mt. Skukum deposits and elsewhere in the Wheaton District was noted.

Mr. Dallas Davis, P.Eng., FEC - Interim Consulting VP Exploration states: "There may exist significant tonnage and many more high-grade veins. The tentative conclusion, subject to reviewing the airborne survey (only preliminary map received to date) is that the Company's 2012 exploration program should be designed to test the potential for large scale bulk mining by diamond drilling."

The soil sampling program covered slightly more than half of the recently enlarged Mount Anderson, Yukon gold/silver, polymetallic property.

The soil analyses were carried out by SGS Toronto Laboratory and the following table shows statistics and the methodology employed to process and depict the Mount Anderson Yukon soil survey results:

Quartile Value in parts per billion (ppb) for 4625 Mt. Anderson Soil Analyses by SGS Toronto Lab MMI-M Method
Ag (ppb) As (ppb) Au (ppb) Cu (ppb) Mn (ppb) Pb (ppb) Sb (ppb) Zn (ppb)
25% quartile(using Excel spreadsheet formula) 21 5 0.1 220 1230 190 0.5 110
50% quartile 38 5 0.2 460 2970 420 0.5 260
75% quartile 72 20 0.6 1200 6380 880 1 630
Highest ppb in the 4625 sample analyses 6850 1560 49.1 29900 155048 63100 160 41600
of which 5 >3000ppb 8>500ppb 3>30ppb 3>20000 3>100000 9>50000 4>100 5>14000
8 >2000ppb 20>300ppb 11>20ppb 28>9999 11>49999 22>24999 11>49 41>6999
23>1000ppb 48>200ppb 30>10ppb 123>4999 88>24999 57>12499 30>24 153>3499
78 > 500ppb 92>150ppb 79>5ppb 533>2499 418>12499 118>6249 67>11 400>1749
714 > 99ppb 143>99ppb 194>2.4ppb 1357>999 1195>6249 263>3124 147>5 902>874
Lower detection limit by SGS Toronto Lab 1 ppb 10 ppb 0.1 ppb 10 ppb 10 ppb 10 ppb 1 ppb 20 ppb
In order to present MMI™ ppb results in a way that is comparable from element to element and indicative of degree to which values are anomalous, the approach presented by SGS (http://www.geochem.sgs.com/mmi-response-ratios.htm) has been followed by Gold World Resources Inc.. This approach is to determine for each element and soil sample the ratio of the ppb result to the 25% quartile background for the particular element. The result is referred to as the "RESPONSE RATIO" ("RR"). The RR also can be described as the number of times that the sample analysis is above background. In the case of samples which contain less than the lower detection limit for a particular element, a value equal to half the detection limit is used for calculating the background.

About the Company:

The Company is a precious- and base-metals exploration company focusing on the Mount Anderson Yukon gold/silver, polymetallic Project.

ON BEHALF OF THE BOARD
"Hermann Derbuch",
Chairman & CEO
Gold World Resources Inc.

*(see Hart, C.J.R., McCoy, D.T., Goldfarb, R.J., Smith, Moira, Roberts, Paul, Hulstein, Roger, Bakke, A.A., and Bundtzen, T.K., 2002, Geology, exploration, and discovery in the Tintina gold province, Alaska and Yukon: Society of Economic Geologists, Special Publication 9, p. 241-274).
** Hart and Radloff (see pages 50 & 77 in INAC, Yukon Region, Open File 1990-4)

Certain of the statements made and information contained herein is "forward-looking information" within the meaning of the Securities Act (Alberta), including statements concerning Gold World Resources' plans for the Property, which involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of Gold World Resources, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking information. Such information contained herein represents management's best judgment as of the date hereof based on information currently available. The TSX Venture Exchange has not reviewed and does not accept responsibility for the adequacy or accuracy of this release.

Source: Canada Newswire (October 27, 2011 - 1:26 PM EDT)

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