Radius Gold Inc. and joint venture partner, Volcanic Gold Mines Inc. announced that a first-pass drilling campaign has commenced on the Mila Gold Discovery located within the Motagua Norte Project. The Mila prospect to date is defined over a 250 m by 600 m area of quartz outcrop, subcrop and boulder float with abundant visible gold and bonanza grade assays discovered Volcanic geologists in Central Guatemala. A diamond core drilling rig has mobilized to commence exploration of the compelling gold targets developed at Mila.

Drill holes are designed to establish the width, grade and geometry of gold mineralization. Volcanic anticipates drilling between 1000 and 3000 m of diamond core in the first campaign. The Mila discovery presents an unusual challenge for exploration but an exceptional opportunity.

The abundance of gold-mineralized quartz boulders covering the surface makes it difficult to map-out, measure and model the gold mineralized structures. Of approximately 420 rock chip samples collected at surface across the area over one hundred returned assays exceeding 10 g/t gold, including twenty-one of over 100 g/t gold and a maximum of 692 g/t gold. With widely distributed gold-bearing quartz at surface it is difficult to distinguish the in situ quartz outcrop from the boulder piles that form at the base of collapsed vein outcrops and from boulder scree that has been locally transported downhill.

In addition to the obvious quartz vein mineralization, gold has also been observed hosted within sericite altered and micro-veined schist with samples returning assay results of up to 94 g/t gold, indicating potential for significant wall rock mineralization. The north-south striking quartz ridge which returned rock chip assays of up to 116 g/t gold is being tested in the first few drill holes. Sericite altered schist with quartz stockwork veinlets cropping-out on the eastern wall of the north-south quartz ridge returned assay results of up to 118 g/t gold is also being targeted in the first few drill holes.

Geological mapping of outcrops combined with interpretation of topographic features suggests that there are multiple quartz veins in at least two different orientations: north-south and northwest-southeast striking, with the best assay results concentrated in north-south trends. Continuous chip channel sampling across the best-defined north-south structure, a 250 m long ridge running through the centre of the prospect area, returned average grades of 95 g/t gold across a 10 m width of collapsed quartz vein boulders. This structure, and at least two more less well-defined parallel quartz boulder ridges are interpreted as north-south striking veins.

True thickness and dip direction of these veins is not yet understood and will be tested in the initial drilling. Drilling will also test a 100 m-wide dense quartz boulder field on the west side of the central north-south structure continuous lines of 2 m long chip channel samples of mixed outcrop, subcrop and colluvium returned average grades of 42 g/t gold along a 34 m line, and 54 g/t gold along a 24 m long line. The surficial quartz in this area is interpreted as the expression of multiple, close-spaced quartz veins.

The number of veins and their geometry are undefined. The initial drill programme is exploratory in nature and aims to establish the number of zones, width, grade and geometry of the gold bearing structures.