European Metals Holdings Limited announced that the planned core drill hole programme was completed on time and budget, without time loss incidents. In total 17 drill holes were drilled to a summary depth of 6081 meters. Analytical results for the CIW-10 and CIW-23. Geomet holds the licenses for the company's 100% owned Cinovec Project in the Czech Republic. Drill Programme: The CIW-10 and CIW-23 were drilled at the western edge, and in the central part, respectively, of the Cinovec Main sector of the deposit. The current drill programme at Cinovec Main has been planned to confirm and delineate near surface lithium and tin mineralization that would provide initial feed to the mill. Other goals are the conversion of resources from the Inferred to Indicated category, and delivery of material for metallurgical testing. So far, ten diamond core holes have been completed, and three are underway. Visual inspection and logging indicates that the geology in these holes is as expected. After geological logging, drill core is cut in half with a diamond saw. Quarter core samples are selected and dispatched to ALS (Romania) for preparation and assay; the 3/4 of the core is returned to the core box and stored securely on site. Samples are being prepared and analyzed by ALS using ICP and XRF techniques following standard industry practice for lithium and tin deposits. Strict QAQC protocols are observed, including the insertion of a Li standard in random fashion for every 10 core samples, as well as the insertion of blank and duplicate samples. Mineralized Intercepts and Lithology: The drillhole CIW-10 was located near the granite-porphyry contact, testing lithium mineralization near the western termination of the deposit. In this location, at the W and NW part of the deposit, the contact is relatively steeply dipping. The CIW-10 drill hole was angled at 75 degrees to the W, and collared in the barren porphyry. At 213 m down the drill axis the porphyry-granite contact was intersected at a depth predicted by the Company's geologic model. The contact is marked by brecciated pegmatite, and immediately below it the granite is greisenized and mineralized in lithium. The interval from 213m to 429m is formed by variably greisenized granite containing 5 to 15% of zinnwaldite, the lithium-bearing mica. The footwall to the greisenized granite is a low-mica granite, in which the drill hole was terminated at 455m. The core angles of contacts are steeper than usually (about 20 to 40 degrees), and as the core was not oriented, it is impossible to ascertain with certainty the orientation of the mineralized zones. Therefore, the mineralized intercept may not represent true width. The drillhole CIW-23 was collared in the central part of the Cinovec-Main deposit where the Cinovec lithium granite daylights. First 119m of the core are formed by sericite-albite (locally hematized) granite. Between 116 and 119 the drill intersected a historic backfilled stope after mining high grade tin-tungsten quartz veins in the 1960's. The interval between 119m and 388.3m is formed by variably greisenized granite that carries zinnwaldite. Locally stopes, narrow quartz veins or massive greisens were intersected in this interval. The footwall to the greisenized granite is low-mica granite, in which the drill hole was terminated at 376.1m.