Wednesday, Nov 12, 2008

Geoinformatics Exploration Inc. (TSX-V: GXL) (""Geoinformatics"", ""GXL"" or the ""Company"") is pleased to announce that it has intersected widespread mineralization in the first hole drilled on a regional prospect called Raintree West, located approximately 1.5 km east of the Whistler Zone which hosts a NI 43-101 compliant mineral resource estimate.

Highlights

First hole ever drilled at Raintree West intersected:

160 metres grading 0.59 g/t gold, 6.02 g/t silver, 0.10% copper,

0.20% lead, 0.46% zinc (or 1.26 g/t gold equivalent) including:

24 metres grading 1.37 g/t gold, 6.32 g/t silver, 0.13% copper,

0.36% lead, 0.80% zinc (or 2.42 g/t gold equivalent).

Raintree West is one of several regional concealed targets drilled byGeoinformatics during the 2008 summer field season. Assays are pending onthree remaining regional prospects and two holes from the Whistler Zoneitself.

We are extremely pleased with the discovery of a new mineralized systemon the Whistler Project as it confirms the exploration potential and validatesthe Companys innovative exploration techniques,"" said Mr. Darren Holden,Chief Operating Officer of Geoinformatics. ""We have long suspected that themineralization defined at the Whistler Zone is one of many related porphyrysystems on the project. This discovery of widespread porphyry hosted goldmineralization at Raintree, with comparable grades to those of Whistlers MainZone, confirms this theory and bodes well for other similar discoveries tofurther enhance the value of the overall Whistler Project.""

Raintree West Prospect

The Raintree West prospect lies in a cluster of prospects identified by the Company using proprietary targeting techniques. Raintree West exhibits acomparable magnetic signature to that of the Whistler Zone with a coincidentinduced polarization (IP) anomaly that extends over 800 metres in length.Raintree West is a blind target, concealed by a thin veneer (5 metres) ofgravels in relatively flat ground.

Drill hole RN-08-06 was angled west to east and intersected diorite porphyry rocks immediately below gravel overburden. The first 22 metres of the diorite porphyry contained low-grade mineralization, below which visible alteration and veining increased and was accompanied by visible copper, leadand zinc sulphides over the next 190 metres. The hole remained in dioriteporphyry to the total depth of the hole at 300 metres