Galway Metals Inc. reported drill results that expand the SW Deposit to the east at the George Murphy Zone (GMZ), and outside of the resource, at the Clarence Stream gold project in southwest New Brunswick, Canada. Assay results for metallurgical holes drilled at the SW Deposit have been received as well. Drill results from the SW deposit west end will be released in the coming weeks.

Results Indicate the SW Deposit is Open East and NE: The Adrian north drill intersections are important because they illustrate there are significant gold intersections located 475 metres from the existing block model. These drill intersections are well north and east of the Triangle area where Galway is attempting to fill in the area between the new Stewart Zone discovery and the existing resource area. Drilling in the Triangle area has returned intersections such as 8.0 g/t gold over 9.5 metres, 3.9 g/t gold over 6.0 metres, 4.1 g/t gold over 10.25 metres, and 8.6 g/t gold over 2.0 metres along 1,380 metres.

These intersections are not included in the existing resource and are interpreted to dip towards veins in the SW Deposit that are dipping the same way; the Sawyer Brook fault (the main accretionary structure on the property that controls most mineralization) is located there; the area of the triangle is 180% larger than the SW Deposit. The intersection of 0.6g/t gold over 12.0 metres in hole CL-155 is located well into the Triangle area. The drill results east of GMZ include 19.1 g/t gold over 1.05 metres, and 0.5 g/t gold over 17.0 metres.

These results indicate that the deposit is open in that direction. Previously released results of 0.6 g/t gold over 41.0 metres (CL-166), and 2.0 g/t gold over 14.0 metres (CL-164) were returned after the resource was completed and would also widen and extend the GMZ resource east. Drilling for Metallurgical Testing and Ore Sorting: Diamond drilling was undertaken to retrieve PQ-sized core (i.e. big core - 85 mm diameter) at Clarence Stream for use in studies to determine the amenability of the mineralization for pre-concentration on site via ore sorting and for metallurgical testing.

The first assay results from the new SW Deposit have been received from the metallurgical core holes. No MET work has been conducted on this new deposit. The Clarence Stream work is designed to check five different areas to confirm if conventional cyanide will liberate good recoveries and if gravity recoveries are adequate.

Intersections from the PQ core include: 12.6 g/t gold over 18.0 metres (Richard Zone) and 8.6 gold Au over 24.3 metres (GMZ west). Other intersections are 1.3 g/t gold over 16.0 metres plus 0.6 g/t gold over 15.0 metres (Richard Zone), 1.4 g/t gold over 14.0 metres (GMZ), 1.0 g/t gold over 11.0 metres plus 24.8 g/t gold over 1.0 metres (GMZ), and 1.5 g/t gold over 42.9 metres (Adrian Zone). Drill holes were drilled in the vicinity of specific existing drill holes that provided a range of assays from low-grade to high-grade.

New Brunswick Junior Mining Assistance Program: Galway would like to acknowledge financial support from the New Brunswick Junior Mining Assistance Program, which partially funded drilling of the SW Deposit. Clarence Stream Geology and Mineralization: Clarence Stream deposits can be characterized as intrusion-related, quartz-vein hosted gold deposits. They contain elevated levels of bismuth and arsenopyrite in multiple quartz veins, with significant antimony in the South and North Zones and tungsten in the vicinity.

The Zones contain multiple zones of quartz veining with sulfides and sericite alteration. In general, mineralization at Clarence Stream consists of 10-70% quartz stockworks and veins with 1-5% fine pyrite plus pyrrhotite plus arsenopyrite in sericite altered sediments. The South and North Zones also contain stibnite.

Locally there is up to 10% sphalerite and semi-massive galena veinlets. The 3.1 km trend that hosts the SW Deposit is associated with a mineralized mafic intrusive locally - similar to the South Zone. The Stewart Zone intersections are located in sediments between two intrusions and mineralization is controlled by fault structures.

It was originally drilled to test a modest 61 ppb soil anomaly that coincided with a strong linear magnetic low, and is in quartz veining with associated 1-3% pyrite, pyrrhotite, and arsenopyrite, very similar to other mineralization in the area. It is located close to the contact with a granite and appears to parallel the contact with multiple veins, at 15 degrees along strike (horizontally - almost north-south) - following a line of soil anomalies, and dipping 40 degrees east toward Adrian. There is also evidence that a second set of veins are in a different orientation, running NE-SW along magnetic lows with corresponding soil anomalies.

This is a similar setting, and with similar geochemical/geophysical signatures, as all the other intrusion-related gold deposits and discoveries at Clarence Stream.