On the Boards: Superflat
Mar 30, 2009 1:10 pm
[caption id=“attachment_1175” align=“aligncenter” width=“300” caption=“The southern tip of Governors Island in 1934. It’s flat.”]
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A few weeks back we blogged about the new hills West 8 is designing on the southern end of the Island. Those hills are part of a larger strategy that will use subtle shifts in topography to transform what are now acres of crabgrass and asphalt into an alluring, intriguing park that people will want to explore. This “transformative topography” is a key element of West 8’s design, but we’ve been struggling with how we communicate its importance to the future success of the park and the Island. Who wakes up in the morning and thinks, “I’d really like to go somewhere with awesome topography today”? But that’s partly what millions of people are doing each year when they decide to visit Central Park or Prospect Park. Before being transformed into parks, those areas were wide swaths of craggy, mostly flat, largely deforested land. Central Park had some schist outcroppings, but it wasn’t the winding, undulating, lush park we love today.
It’s also hard for people to visualize the extreme flatness of the Island, especially since most people have only experienced the lovely rolling landscape of the historic northern half of the Island (though this will change this summer when we open Picnic Point). We hope you come out this summer and see for yourself; in the meantime, check out some great historic photographs that really show off the Island’s flat southern half (see above and below).
[caption id=”” align=“aligncenter” width=“296” caption=“Governors Island in 1951. It’s still flat.”]
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