Cypress Completes Phase 1 Drill Program at Gunman Zinc-Silver Project in Nevada

VANCOUVER, BRITISH COLUMBIA--(Marketwired - May 27, 2014) - Cypress Development Corp. (TSX VENTURE:CYP)(PINKSHEETS:CYDVF)(FRANKFURT:C1Z) ("Cypress" or the "Company") is pleased to announce that the Phase 1 2014 drill program at its wholly owned Gunman zinc-silver oxide project, Nevada, has been completed with all assays pending. The 1140 acre Gunman zinc-silver-gold project is located directly west of Barrick's Bald Mountain gold mine complex on the southern Carlin mineral trend in White Pine County, Nevada.

Three previous Reverse Circulation (RC) drill programs totaling approximately 38,000 feet have been completed by Cypress on the Gunman project with significant grades between 5% to 33% zinc and 0.5 to 15.0 oz per ton silver encountered in the RH Zone.

Gunman Project Southern Carlin Trend location map: www.cypressdevelopmentcorp.com/s/Image.asp?i=Maps/Gunman-43-101.jpg

Cypress carried out a thirteen hole 2014 Phase 1 RC drill program at its Gunman poly metallic property in White Pine County, Nevada. The thirteen holes totaled 3,540 feet and were targeted at three areas of the central portion of the property. Additional work completed during Phase 1 includes the initiation of a detailed stratigraphic study in the central portion of the property and prospecting in the far north exploration area, located 5000 feet north of the central portion of the property.

2014 Gunman RC Drill Hole Location Map: www.cypressdevelopmentcorp.com/s/Image.asp?i=Maps/Gunman-May-2014-RC-Plan-Map.jpg

Main RH Zone Area

Seven holes were drilled into the known, well developed oxide zinc and silver mineralization at the RH Zone. These holes were completed to provide confirmation assays in order to complete an independent NI 43-101 Compliant Resource Estimate and for the opportunity to collect additional data on the style of mineralization at the RH Zone. The holes drilled into the western portion of the RH Zone intersected the distinctive poly lithic, rounded grain sandstone which is known from outcrop along the western margin of the RH Zone. Below this clastic marker unit, a well fractured, brecciated and stock work veined dolomite unit is encountered. Well-developed gossanous zones were logged from near surface to an approximate depth of 220 feet. Carbonaceous dolomite was intersected at depth in all the RH Zone area holes.

Bedrock exposures created during construction of the RH Zone area drill pads have provided valuable, detailed data on the style of mineralization in the near surface portion of the RH Zone. Gossanous boxworks form irregular bands through the exposed, highly brecciated dolomite. These gossan zones are associated with quartz veinlet swarms and quartz, carbonate, iron oxide breccia matrix in fills. These textures and observed veining zone associated with the gossanous boxworks suggest that the mineralization in the near surface portion of the RH Zone has a strong component of quartz and poly-metallic sulfide veining.