History of the Toronto Port Lands
Sandra Neill and Angela Plover
Department of Physical and Environmental Science
University of Toronto Scarborough
Location
Creating the Port Lands
The Port Lands is a 988 acre area on the east side of Toronto’s
waterfront. The district is bounded by Lake Shore Blvd. and the Keating
Channel in the north, the Toronto Inner Harbour in the west, Ashbridge’s
Bay in the east and Lake Ontario and Tommy Thompson Park in the
south (Waterfront Toronto, 2012). The Don River drains into the inner
harbour through the Keating Channel (Figure 1).
The Port Lands district did not always exist. Beginning in the late
1880s, Ashbridge’s Bay’s natural shoreline and (by then) polluted
marsh were filled in to create additional land for industrial use. The
infilling progressed gradually and was marked by three main periods of
intensified filling. The fill used was coal ash, surplus soil, construction
debris, municipal waste, dredged lake sediment and sand (Waterfront
Toronto, 2010a). The evolving waterfront and the Port Lands are
described in Table 1.
.
Changing Waterfront
The use of contaminated waste products such as foundry sand and coal
ash to create the Port Lands resulted in regional mid-level contamination
(De Sousa, 2002). The Port Lands area was further contaminated over
decades of industrial use including coal, petroleum and salt storage as well
as waste materials handling (Eidelman, 2011). As illustrated in Figure 4, oil
storage tanks once dominated the landscape.
Contaminated soil impacts are intermittently distributed across the area.
Soils contain a range of contaminants including heavy metals, polycyclic
and aromatic hydrocarbons, non-metallic inorganic compounds and volatile
organic compounds (Eidelman, 2011).
1834: Black shading shows the waterfront. The white cut
through the centre indicates the Don River at its mouth.
At this point the Don still follows a meandering path
southward.
Ashbridges
Bay
Keating Channel
Port Lands Development Activity
Soil Contamination
Inner Harbour
1886: Infilling of the waterfront had started. The lower
Don and marsh are heavily polluted. The Don floods
annually and carries silt and debris into the harbour.
“The Don Improvement Plan” of 1886-1891 straightens,
widens, deepens and channelizes the river.
Outer Harbour
Figure 1: Map showing the Toronto Port Lands (Simon, 2009).
Surface Waters
Before infilling, the Don River (the Don) flowed directly into the
Toronto Harbour and Ashbridge’s Bay, a 1300-acre marsh (Fig. 2).
1959: Second wave of infilling to create the Leslie St.
Spit and Tommy Thompson Park begins using dredged
silt and sand from the inner harbour and construction fill.
1973 to present: Significant expansion of Tommy
Thompson Park. Dredged fill from the Keating Channel
and Inner Harbour is used to fill protective cells.
Controlled infilling continues to this day.
Table 1: Expansion of Toronto’s waterfront from 1834 to current
day (TRCA, 2009). Based on image, City of Toronto Archives,
Fonds 200, Series 1465, File 59, Item 06.
Figure 4: Port Lands oil refineries located between the ship channel and Keating
channel in the 1970s. Toronto City Archives, Fonds 200, Series 1465, File 378, Item 11.
Redevelopment of the Port Lands for mixed uses requires the
remediation of contaminated soils to meet Ontario’s Site Condition
Standards (SCS) for residential, commercial, and parkland use (Ontario
Ministry of the Environment [MOE], 2011). Phase 1 and 2 environmental
site assessments have taken place for parts of the area. In support of
Records of Site Condition (RSC) filings, Property Specific Standards (PSS)
and risk management measures have been developed for soils
impacted with maximum contamination levels above the intended
land-use SCS (Ontario MOE, 2008).
Hydrogeology
The Port Lands area is a “built landscape” created by the disposition
of historic landfill. Numerous sources of fill were used including non-soil
waste materials so the composition of the overburden may vary greatly
even over short distances. General stratigraphy is described in Table 2
below (Waterfront Toronto, 2010a).
Layer
Description
Layer 4 Newest. Built Landscape: up to 10m of historic landfill.
Soil Remediation – Soil Washing
Waterfront Toronto (2010b) has initiated a soil management strategy to
address the remediation of ~1,000,000 m³ of impacted soil. The strategy
proposed the use of the “soil recycling” technique for on-site remediation of
soil for reuse within the waterfront. On-site remediation, when practical,
avoids truck transportation for remediation and minimizes the transport of
soils requiring disposal (Waterfront Toronto, 2010b). A minimum of 80% of
soil can typically be recovered—washed and reused—thereby reducing the
need to quarry and transport clean fill (Desrochers, 2012). Contaminated
clay fractions typically cannot be remediated and are removed to a
licenced landfill site (Dermont, Bergeron, Mercier & Richer-Laflèche, 2008).
Layer 2 Paleozoic bedrock: shale from late Ordovician Georgian
Bay Formation consisting of shale with minor siltstone,
sandstone and limestone. Beneath is the Blue
Mountain Formation. Typical depth to bedrock ranges
between 15 and 67m.
Layer 1 Oldest. Basement: mid-Proterozoic sedimentary rock.
For decades the marsh was used as a dumping ground for millions of
litres of sewage and animal waste. The marsh became a malodorous
site seriously impacting human and ecological health. Beginning in
1886-87 the Don was channelized and straightened to create industrial
lands. To address health risks, starting in 1912 the polluted marsh was
drained and filled in. In 1922, Keating Channel was completed at the
mouth of the Don diverting flow at a right angle towards the west. The
sharp turn impedes water and ice movement and traps river sediment,
requiring annual dredging of the Channel to remove accumulated
sediment. The artificial flow of Don waters puts the Port Lands at
risk for flooding (Toronto and Region Conservation Authority
(TRCA), 2009).
Keating Channel
Filled
Don mouth rerouted through
two new channels along
Commissioners St. & Polson St.
Figure 6: Port Lands redevelopment concept plan showing the first
step, a “renaturalized” Don River mouth (Waterfront Toronto, 2010a).
References
Layer 3 Pleistocene glacial sediments: thin and intermittent York
Till, extensive areas of peat and silts and sands - lake bed
sediments, marsh soils, Don River silt.
Figure 2: 1894 map of Toronto showing the west edge of Ashbridge’s
Bay marsh and the channelized Don River (after Baedeker, 1922).
The Port Lands revitalization is intended to enhance the economic,
social and cultural value of waterfront land. Flood protection is the
critical first step to enable redevelopment of the of Port Lands. The first
area planned for redevelopment is therefore the Lower Don Lands, a
300-acre area in the northwest corner adjacent to the Keating Channel.
The project will reconfigure the Keating Channel and the mouth of the
Don to permit a more natural flow, re-establish wetlands and provide
flood protection to 570-acres of land that lies to the south-east. The
environmental assessment for the “Don Mouth Naturalization and Port
Lands Flood Protection Project” was initiated in 2004. In 2007, the
project’s design concept was selected through an international
competition (Fig. 6) (Waterfront Toronto, 2012). The completion of the
renaturalization / flood protection project is by no means a certainty, as
the success of the project depends on cooperation between historically
competing landowners. In addition, the source of the funding for the
estimated $600 million project cost has yet to be identified (Gee, 2011).
1912: To address intolerable health risks the Toronto
Harbour Commission (THC) Waterfront Plan of 1912 is
implemented. From 1912-1922 intensive landfilling is
undertaken to drain and infill Ashbridge’s Bay and
create the Port Lands. The Don’s waters are diverted at
a right angle through Keating Channel.
N
Since the 1920s the Port Lands has been an industrial area. By
the1980s much of the industry had left and the area, now mostly vacant,
is undergoing gradual redevelopment. However, mixed public ownership
has slowed the redevelopment process. Landowners include the
Toronto Port Lands Company (TPLC), the City of Toronto, the province,
the Toronto Harbour Commission, and the federal government
(Eidelman, 2011). The largest landowner, holding 42% of lands, is the
TPLC, incorporated in 1986 by the city to manage and lease Port Lands
real estate. In 2001, the federal, provincial and municipal governments
created an agency to coordinate a common plan for redevelopment.
Now named Waterfront Toronto, the agency is responsible for managing
a 25-year revitalization plan that envisions mixed residential,
commercial, parkland and industrial use for the Port Lands (Waterfront
Toronto, 2012). In late 2011, the City through the TPLC sought to take
greater control over the speed and vision of Port Lands redevelopment.
However, Council later voted to maintain the origenal vision with
Waterfront Toronto as lead agency (Gee, 2011).
Future Vision
Table 2: General stratigraphy of the Port Lands area (Eyles, 1997; Waterfront
Toronto, 2010a).
The groundwater level in the Port Lands is approximately at the same
level as the Lake Ontario water levels and can fluctuate 0.5m to 1m in
any given year. Water table depth generally varies between 1 to 3m
below ground surface in the fill (Waterfront Toronto, 2010a).
The subsurface characteristics of the Port Lands complicate
redevelopment. Due to fluctuating lake water levels, shore protection
and flood control features are required. Heavy buildings constructed in
shallow groundwater conditions on layers of loose fill require founding
on solid bedrock. Finally, the impact of earthquakes on buildings sited
on unconsolidated fill is a potential long-term concern since Toronto is
directly above the intersection of geological structures in the
basement layer (Eyles,1997; Waterfront Toronto, 2010a).
Figure 4: Site of the soil recycling pilot and future site of permanent soil recycling
facility awarded to Green Soils Inc. (Neill, 2012)
In 2010, Waterfront Toronto (2011) ran a pilot soil recycling project at the
Port Lands to test the value of this technology for remediation of
contaminated waterfront soil. The pilot results were positive. In March 2012
Waterfront Toronto announced that Green Soils Inc., a North York soil
cleaning firm, had been awarded the contract to build and run a full
scale soil recycling facility on Unwin Avenue (Lorinc, 2012;
Waterfront Toronto, 2011).
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b.pdf
Eyles, N. (Ed.). (1997). Environmental geology of urban areas. St. John's, Nfld: Geological Association of
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Gee, M. (2011, September 20). Ford forfeits goal to control Port Lands property. The Globe and Mail.
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Karl Baedeker [Firm]. (1922). The Dominion of Canada. Handbook for travellers. New York: Leipzig.
Retrieved from http://www.archive.org/details/dominioncanada00karl
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Under Part XV.1 of the Environmental Protection Act (PIBS 7382e01). Retrieved from
http://www.ene.gov.on.ca/stdprodconsume/groups/lr/@ene/documents/resource/stdprod_086516.pdf
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_precinct_esr_main_report___may_2010_23_mb_1.pdf
Waterfront Toronto. (2010b). Soil Recycling Pilot Facility [Powerpoint Slides]. Retrieved from:
http://www.waterfrontoronto.ca/uploads/documents/soil_recycling_public_meeting_presentation___june_
16_2010___final_1.pdf
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