Euclid Green Integrated Planning
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Transcript of Euclid Green Integrated Planning
Restoring the Pulse
1) Streams into Sewers
City of Euclid boundary
Google Earth aerial viewer
© 2015 Bluestone Heights
Bluestone
Heightsbluestoneheights.org
2) Initial Green Solutions
4) Eco-Greenways
of Nature in Euclid
3) Integrated Planning
Bluestone HeightsRoy Larick
5) Euclid Ecology Unit
Overview
In five SlideShares, Restoring the Pulsepresents two goals for stormwater Integrated Planning in Euclid, Ohio:
• Revive the natural regulation of stormwater at relatively low cost and high community benefit.
• Reconnect fragmented natural habitat areas as a means to build local biodiversity and natural capital.
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Integrated Planning rationale
Integrated Planning
In 2015, Euclid may be able to revisit the EPA consent decree and its gray stormwater solution.
If so, we will want to pitch an Integrated Plan to EPA. Under such a plan, stormwater becomes a resource in potential benefit the sewer utility and the larger community.
Simply put, Integrated Planning encourages cities to work with nature, not against it.
Integrated Planning is the way we can restore the natural pulse of stormwater flow and also rejuvenate our urban watersheds.
Integrated Wastewater Planning ApproachEPA, May 2012
City of Euclid boundary
Google Earth aerial viewer
200th 222nd Babbitt 260th Lloyd
© 2015 Bluestone Heights
Restoring the Pulse
Euclid storm sewer catchments
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City of Euclid boundary
BioretentionManaging stormwater as a resource
Bioretention is the base means for slowing stormwater and for restoring the natural pulse in sewer catchments.
Bioretention helps reduce CSOoverflows and can help revive fragmented watershed features and ecological habitats.
Bioretention is the primary means to rebuild ‘natural capital’ under an Integrated Plan.
City of Euclid boundary
Google Earth aerial viewer
200th 222nd Babbitt 260th Lloyd
© 2015 Bluestone Heights
Integrated PlanningRestoring the Pulse Integrated Wastewater Planning Approach
EPA, May 2012
Euclid storm sewers
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Euclid watershed evolution
In addition to the priority CSOcatchments, Euclid has many places where bioretention can help restore the natural pulse of diminished watersheds.
Many such places involve ‘ghost water features’, stream course segments abandoned but still showing signs of life.
Ghost features offer good potential for greening under an Integrated Plan.
To understand the nature of ghosts and other ecologically sensitive places, let’s review how local watersheds have waxed and waned over the years.
City of Euclid boundary
Google Earth aerial viewer
200th 222nd Babbitt 260th Lloyd
© 2015 Bluestone Heights
Integrated PlanningRestoring the Pulse
Euclid storm sewers
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Euclid watershed evolution
The story begins with the retreat of the last glaciers and glacial lakes about 12,000 years ago.
To see the effects of time, we’ll observe a slice of the local landscape from the escarpment down to the lake. The slice long axis parallels Babbitt Rd.
Like Lloyd Rd, Babbitt follows the course of an escarpment run from Euclid Ave to Lake Erie. In this case, it is Babbitt Run.
City of Euclid boundary
Google Earth aerial viewer
200th 222nd Babbitt 260th Lloyd
© 2015 Bluestone Heights
Integrated PlanningRestoring the Pulse
Euclid storm sewers
Euclid bluestone
Cleveland Shale
Chagrin Shale
looking southeast
bluff
hills
face
plain
terrace
Integrated PlanningRestoring the Pulse
Euclid descends to Lake Erie in three steps.
The Portage Escarpment is a shale ‘massif’ capped with Euclid bluestone (fine, hard sandstone). The escarpment has two parts: face and hills.
The St Clair Terrace has a shale surface leveled by the surf of ancient glacial lakes.
The lake plain is covered with soft glacial debris and lake bottom clay.
Intensity of green represents the density of the local forestThe escarpment face is heavily forestedLake plain and hills have a typically urban forestSt Clair Terrace, highly industrialized, is the least forested
Euclid deep history
© 2015 Bluestone Heights
Euclid bluestone
Cleveland Shale
Chagrin Shale
hills
plain
terrace
12,000 BP
Stream headwaters had cut deeply into the escarpment face. ‘Escarpment ravines’ were the result.
Upon reaching the terrace and plain, the streams could cut shallow, shifting channels.
Along the lake bluff, streams dug deeper ravines in final descent.
About 12,000 years ago, with the retreat of the last glacier and associated lakes, Euclid’s watersheds had fully emerged.
The climate was still cool. There were few deciduous trees and lots of shrubbery and grassland. Euclid’s habitat suited mammoth (grazers) and, especially, mastodons (browsers).
Euclid deep history
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
surface stream
escarpment ravine
Euclid bluestone
Cleveland Shale
Chagrin Shale
hills
plain
terrace
10,000 BP
By 10,000 years ago, climate had warmed enough to support the emergence of the current deciduous forest.
Euclid deep history
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
surface stream
escarpment ravine
Euclid bluestone
Cleveland Shale
Chagrin Shale
hills
plain
terrace
1830 CE
By 1830 CE, Euclid’s early settlers were clearing the forest for agriculture, charcoal, and timber..
Forest clearing promoted erosion, especially on the escarpment face and the terrace. On the terrace, farmers began rerouting streams in ditches along roads and property lines.
After the Civil War, vineyards became Euclid primary agricultural endeavor, especially on the terrace. As vineyards did not require intensive plowing, agricultural erosion was minimal.
Euclid deep history
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
surface stream
escarpment ravine
Euclid bluestone
Cleveland Shale
Chagrin Shale
hills
plain
terrace
1890 CE
Trees flourished along property lines and abandoned farmland. Many of Euclid’s current large trees lie along old property lines.
By 1890, Euclid flat land became more valuable for building than for farming. A few vineyards held on to about 1920, but most farmland was abandoned to real estate speculation.
Euclid deep history
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
surface stream
escarpment ravine
Euclid bluestone
Cleveland Shale
Chagrin Shale
hills
plain
terrace
surface stream
buried stream
storm sewer
1950 CE
Euclid’s residential areas were still pretty bare in 1950. The urban forest ethic arrived in the 1960s.
With industrial and residential growth, Euclid’s streams became polluted and inconvenient for all forms of development.
The storm sewer system was established in the 1920s. On the plain and hills, almost all streams were buried by 1950.
Ghost features are to be found along buried stream courses.
Euclid deep history
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
escarpment ravine
Euclid bluestone
Cleveland Shale
Chagrin Shale
hills
plain
terrace
surface stream
buried stream
storm sewer
CSO catchment
2015 CE
Since the implementation of the US Clean Water Act in 1972, Euclid has made significant progress in upgrading its sanitary and storm sewer systems.
Storm events bring polluting overflows to 17 Combined Sewer Overflow (CSO) points. Eight CSOsare activated in even small ‘wet weather’ events. Each combined sewer system has a significant catchment.
Euclid Initial Green Solutions
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
escarpment ravine
Bioswales
Euclid bluestone
Cleveland Shale
Chagrin Shale
hills
plain
terrace
2025 CE
In devising an Integrated Stormwater Plan, we must first address the eight priority CSOs.
Strand’s ‘green sub-catchment’ designs are a good starting point (Initial Green Solutions).
Each would create new storm sewers to shunt pure stormwater to local bioretention facilities or ‘bioswales’.
Euclid green future
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
Control Runoff
Green Infrastructuresurface stream
buried stream
storm sewer
bioswale
CSO catchment
escarpment ravine
Bioswales
Rain gardens
Curbside bump-outs
Permeable pavement
Green roofs
Control Runoff
Euclid bluestone
Cleveland Shale
Chagrin Shale
Green Infrastructure
hills
plain
terrace
2025 CE
The second stage of an Integrated Plan would develop a range of bioretention facilities in non-priority areas.
We can benefit greatly by placing green infrastructure in relation to surviving surface streams and at ‘ghost’ stream locations. There are scores of ghost stream landscapes on the terrace and plain.
Euclid green future
face
© 2015 Bluestone Heights
bluff
Integrated PlanningRestoring the Pulse
surface stream
buried stream
storm sewer
bioswale
CSO catchment
escarpment ravine
Euclid bluestone
Cleveland Shale
Chagrin Shale
Eco-Greenways
Infiltrate stormwater
Increase habitat richness
Raise species diversity
Link public green spaces
Enhance connectivityPerform eco services
bluff
hills
Reforest
Extend wetlands
Restore streambeds
Stabilize slopes
Restore streambeds
Eradicate invasive species
Expand water bodies
Provide alternative transit channels
plain
terrace
2025 CE
As bioswales grow in number, individual sites can be linked within ‘eco-greenways’. Storm water infiltration can be maximized while greenspace is enhanced.
Eco-greenways regroup fragmented natural habitats. In linking habitat islands we can increase the natural capital of our city.
Greenways are all about restoring the natural pulse.
face
Greenway construction tasks
© 2015 Bluestone Heights
Eco-Greenways
Integrated PlanningRestoring the Pulse
Euclid Stormwater Integrated Plan
surface stream
buried stream
storm sewer
bioswale
CSO catchment
escarpment ravine
Public PresentationEuclid Public LibraryJune 10, 2015
City of Euclid boundary
© 2015 Bluestone Heights
Restoring the Pulse
1) Streams into Sewers
Bluestone
Heightsbluestoneheights.org
2) Initial Green Solutions
4) Eco-Greenways
of Nature in Euclid
3) Integrated Planning
5) Euclid Ecology Unit
Google Earth aerial viewer
Roy Larick
Walk back in time Look to the Future
Bluestone Heights
© 2015 Bluestone Heights
A production by
bluestoneheights.org
[email protected] bluestone outcropDoan Brook, Cleveland OHR. Larick