Spacing Toronto's Daniel Rotsztain describes, with photos and maps, the aftermath of a recent walk in downtown Toronto's underground path system reveals the still-lasting geological influence of the area. Even after all the construction and channelling, remnants of lost streams like west-end Toronto's Garrison Creek still endure.
Thinking about the sheer volume of stone mined from the earth, shipped across the planet and reconstituted as Torontonian skyscrapers, it’s easy to appreciate that our modern city is a geologic force as strong as those that created the Scarborough Bluffs and carved the ravines.
Sometimes, the geologic forces of urbanization are more subtle. When the initial construction of the Bay-Adelaide centre was delayed indefinitely in the early 1990s, the city was left with a 6-storey stump and an unfulfilled order of 35,000 tons of Norwegian granite. Without the 44-storey tower to be clad, the city was awash in free flowing Scandinavian stone that has since settled into hundreds of tables and floors in downtown Toronto.
Beneath the city covered in layers of stone from elsewhere, there are indeed remnants of historical watercourses. Though most of the waterways in downtown Toronto have been eradicated due to extreme excavation for infrastructure and subterranean parking levels, a proxy for one of the Market Streams that used to flow south east through the city does exist.
In the corridor between the Royal Bank Building and Brookfield Place, the stone below our feet was showing signs of water absorption. This would have been where Newgate Creek emptied into Lake Ontario.
Though dry to the touch, the off-coloured stone might be a sign of the groundwater that would have replaced the creek. Standing underground, surrounded by concrete, it’s powerful to feel this rare assertion of the landscape beneath Toronto — a sign of the city before the glass, steel and international stone of today’s internationally constituted metropolis.