in the main lobby, glass vanities in the suite washrooms, heated floors, and a water wall in the spa. The Inn at the Forks project was the first Canadian application of the "Redi-Maid" system that links ensuite occupancy sensors, lighting and mechanical system controls to staff PDAs with the goal of maximizing energy efficiency. The hotel was completed with a construction cost of $16 million in May 2004. Winnipeg Rail Museum The Winnipeg Rail Museum is located at the historic Union Station adjacent to the Forks. It is home to the Countess of Dufferin steam locomotive, the first locomotive to enter western Canada. Outdoor features The Forks features numerous outdoor facilities, sculptures, and landscape features open to the public. Arctic Glacier Winter Park During winter, the following skating rinks, trails and snow park structures are erected at the Forks. The Plaza Skating Rink An Olympic-sized Skating Rink Rink under Scotiabank Stage 1.2 km of skating trails The Snowboard Fun Park The Toboggan Run In January 2008, the Guinness Book of World Records recognized The Forks as the home of the longest skating rink in the world. The 8.54-kilometre-long Assiniboine Credit Union River Trail on the Assiniboine River and the Red River is almost 1-kilometre longer than the previous record-holding rink. The 7.8-kilometre long rink on the Rideau Canal in Ottawa, Ontario had lost its World Record title which it had held since 1971. Then in 2008 the rivers beat their own record which made the longest rink go to about 9.3-kilometres. The Rideau Canal still held the record for the "world's largest naturally frozen ice rink" by the Guinness Book of World Records because "its entire length receives daily maintenance such as sweeping, ice thickness checks and there are toilet and recreational facilities along its entire length". In 2013, the Assiniboine Credit Union River Trail lost its record to the Lake Windermere Whiteway at Invermere, British Columbia. The length of the skating trail at The Forks changes each year, depending on river and ice conditions, although a concerted effort is made to make it as long as possible. In the winter of 2010/2011, conditions on The Assiniboine River made it impossible to safely create skating westward, so the path extended instead south on the Red River. Essentially, the water level and the weather at the time of freeze-up will impact the way the ice forms (see frazil ice, for example),