Stanley Park has significantly changed since its opening to the public in the year 1888. The change is mainly contributed to the landscape transformation of the small peninsula that is situated adjacent to the downtown Vancouver. Moreover, the greatest landscape alterations have taken place to the underlying public park (Schultz, 2007). Peninsula is mainly forested with diverse conifers whilst the shoreline is still intact. The underlying boundary amidst the prevailing park and the corresponding city is similar. Nevertheless, numerous substantial landscape changes depict that complicated environmental history of the existing urban park. Prospect Point Two of the underlying conspicuous landscape alteration within the Stanley Park since the year 1888 is mainly situated on the farthest west end of the peninsula at the Prospect Point. This is depicted to be the highest elevation point within the park and mainly overlooks the underlying entrance to the city’s harbour (Schultz, 2007). Moreover, it depicts the change in the southern shore of the First Narrows on the Burrard Inlet. At the end of the nineteenth and subsequent early twentieth centuries Vancouver city council supervised the change of the section of the Stanley Park in order to facilitate the building of the dual fundamental pieces of the urban infrastructure, Lions Gate Bridge and corresponding water reservoir. In the year 1889, the prevailing Vancouver Waterworks Company finished the building of the freshwater pipeline from the underlying Capilano River, which ran below the First Narrows via Stanley Park (Schultz, 2007). Subsequent to the shipping accident severed the underlying submerged pipeline at the prevailing First Narrows constructed an emergency reservoir at the existing Prospect Point (Schultz, 2007). In the year 1905, the city enlarged and subsequently upgraded the initial reservoir. It replaced the Prospect Point reservoir after the Greater Vancouver Water Board with the renowned Little Mountain in the year 1946. Moreover, the underlying park board filled and correspondingly covered the original reservoir thus changing it into to the baseball diamond.
ReferenceSchultz, P. (2007). 1,000 places to see in the USA and Canada before you die. New York: Workman Pub.
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