Green Network Study Area

What in the world is the P4G Green Network Study Area?

Well to start out with , the Saskatoon North Partnership for Growth (P4G) is a collaborative which includes political and administrative representation from the following partnering municipalities: City of Saskatoon, Rural Municipality of Corman Park, City of Martensville, Town of Osler, City of Warman, Saskatoon Regional Economic Development Authority(SREDA) (Advisory Role)

Now then where is the Green Network Study Area located?

Green Network Study Area, south of Saskatoon, Saskatchewan in the Rural Municipality of Corman Park, part of the Saskatoon North Partnership for Growth P4G planning area (partial map) adapted from the Saskatoon North Partnership for Growth Regional Plan map on page 26
Green Network Study Area, south of Saskatoon, Saskatchewan in the Rural Municipality of Corman Park, part of the Saskatoon North Partnership for Growth P4G planning area (partial map) adapted from the Saskatoon North Partnership for Growth Regional Plan map on page 26

Page 45 of the Saskatoon North Partnership for Growth Regional Plan explores the concept of this green space, and the discussion is supplied in the aforementioned report explaining those aspects which are under additional review.

Basically the report states that, “the Green Network Study Area includes connected areas of wetlands, swales, natural areas, the South Saskatchewan River corridor, and other areas providing stormwater storage and conveyance, and recharge of groundwater supplies.”

This area will support the native flora and fauna of the area, thus encouraging wildlife to thrive and move about from the West Swale wetland areas through to the South Saskatchewan River.

According to the P4G report, there will be consideration given to both environmental and recreational activities in multi-functional green spaces.  This inter-connected open space system will supply opportunities for hiking, cycling, bird-watching, and other passive recreation activities within parks, open space, and protected areas.

Across the river, the green natural space marked on the map, as well, is Diefenbaker park.

Meewasin Valley Authority’s Maple Grove Conservation Area/ Leisureland and Yorath Island are both found within the Green Network Study Area on the west side of the South Saskatchewan River.  More about these areas follows.

Wikimapia reports on Maple Grove Conservation Area/ Leisureland as follows; ”

Maple Grove originally did not have a channel running through it. The quarter section of which Maple Grove is part of was intact when surveyed in 1903; however, the river channel meandered into the quarter section then deposited on the west edge forming Yorath island. This natural accretion allowed the owner of Maple Grove to retain title of the remainer of the quarter section on the island (very rare).

In the 1960s, Mr. Mike Egnatoff and his wife developed the area into an amusement park with a ferris wheel, trampolines, miniature golf, playground, train, playfields, and picnic facilities. In addition, they developed a dance hall with kitchen and concession. A campsite for trailers was developed which turned into a permanent mobile trailer park with 18 trailer units. The amusement park was known as Leisureland. It was very active for 20 years, then except for the group picnics, hall and trailer court, the area became inactive due to amusement competition in town. The Egnatoffs built a new house on the site close to the river and near the hall in the 1980s. In addition to the trailers and the one new house, there is a shack that is located south of the hall at the base of the west bank. This building is the only building site on the lower terrace that is above the 1:500 year flood line. A root cellar mini hall was built to service the catering hall near the entrance to the property. This building is currently being leased to a group of artists.”

Wikipedia has an article about Yorath Island, the confluence of the West Swale;
“Yorath is a small island, 151 acres (61 ha) in size, in the South Saskatchewan River just outside the southern boundaries of the city of Saskatoon, Saskatchewan, Canada. The island is relatively new, and did not exist when the land was first surveyed in 1903. This island is managed by the Meewasin Valley Authority; it is not accessible by road (although some maps of the area plot a non-existent north-south grid road on the island), but can be seen from the Maple Grove (formally Leisureland) area. The island is named after Christopher J. Yorath, who in 1913 became the commissioner of Saskatoon.Yorath is best known for an extensive, forward-thinking planning document published in 1913 that proposed future residential and road layout for Saskatoon, and he originated the idea of the City developing an “Encircling Boulevard”; in 2013 this proposal came to fruition with the completion of the Circle Drive freeway project. Ironically, Yorath’s document proposed the Encircling Boulevard cross through what would later be named Yorath Island; the final Circle Drive passes to the north of the island, which is undeveloped save for a set of power lines that cross the river and the northern tip of the island.Within North America the Island is one of the farthest northern examples of a cottonwood forest. The island also support 23 different types of shrubs and a mixture of wildlife (including the Cooper’s Hawk, coyotes, red foxes, river otter, porcupine, beaver and deer)”

“The Meewasin Valley Authority entered to an agreement with the Leisureland  Community Co-operative Ltd. whereby the public use of certain lands (Maple Grove) owned by Meewasin is limited. The agreement was a condition of the purchase of the property by Meewasin and will expire December 31, 2022.” City of Saskatoon

For more information:

Blairmore Sector Plan Report; planning for the Richard St. Barbe Baker Afforestation Area,  George Genereux Urban Regional Park and West Swale and areas around them inside of Saskatoon city limits

P4G Saskatoon North Partnership for Growth The P4G consists of the Cities of Saskatoon, Warman, and Martensville, the Town of Osler and the Rural Municipality of Corman Park; planning for areas around the afforestation area and West Swale outside of Saskatoon city limits

Richard St. Barbe Baker Afforestation Area is located in Saskatoon, Saskatchewan, Canada north of Cedar Villa Road, within city limits, in the furthest south west area of the city. 52° 06′ 106° 45′
Addresses:
Part SE 23-36-6 – Afforestation Area – 241 Township Road 362-A
Part SE 23-36-6 – SW Off-Leash Recreation Area (Richard St. Barbe Baker Afforestation Area ) – 355 Township Road 362-A
S ½ 22-36-6 Richard St. Barbe Baker Afforestation Area (West of SW OLRA) – 467 Township Road 362-A
NE 21-36-6 “George Genereux” Afforestation Area – 133 Range Road 3063
Wikimapia Map: type in Richard St. Barbe Baker Afforestation Area
Google Maps South West Off Leash area location pin at parking lot
Web page: https://stbarbebaker.wordpress.com
Where is the Richard St. Barbe Baker Afforestation Area? with map
Where is the George Genereux Urban Regional Park (Afforestation Area)? with map

Pinterest richardstbarbeb

Facebook Group Page: Users of the George Genereux Urban Regional Park

Facebook: StBarbeBaker

Facebook group page : Users of the St Barbe Baker Afforestation Area

Facebook: South West OLRA

Twitter: StBarbeBaker

Please help protect / enhance your afforestation areas, please contact the Friends of the Saskatoon Afforestation Areas Inc. (e-mail)

Support the afforestation areas with your donation or membership ($20.00/year).  Please donate by paypal using the e-mail friendsafforestation AT gmail.com, or by using e-transfers  Please and thank you!  Your donation and membership is greatly appreciated.  Members e-mail your contact information to be kept up to date!

QR Code FOR PAYPAL DONATIONS to the Friends of the Saskatoon Afforestation Areas Inc.
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Membership : $20.00 CAD – yearly
Membership with donation : $50.00 CAD
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1./ Learn.

2./ Experience

3./ Do Something: ***

The Province of Saskatchewan Motto:

Multis e gentibus vires (From Many Peoples Strength)

Has any one of us ever really seen a Tree? When we become aware of trees we may each glimpse of them to moments of spiritual vision and, identifying ourselves with the trees, become conscious of the rising of the sap; the upward thrust of life, leaf burgeoning, their consciousness of the changing seasons; we may share their passionately boisterous exuberance of life in the height of the storm, and their tranquility when at rest; with them we will enjoy the glad murmur of the ripening seed clusters when after weeks of drought the steady warm rain brings relief to thirst; and we will know that these creatures, our elder brethern, are intimately related to us in their love and hunger for life. We may even catch their enthusiasm and aspire heavenwards while still rooted in our Mother Earth and in communion with our fellow man and, tree-wise, strive to make the Earth more fruitful again.~Richard St. Barbe Baker

 

 

What is the West Swale?

Geological formation during The Pleistocene Era

Geology of the Yorath Island Spillway After the Flood.

The geological formation of the West Swale occurred during the Pleistocene era from waters cascading out of the glacial l North Saskatchewan River valley, which is quite different from the formation of the North East Swale, which was formed from glacial ice waters in the South Saskatchewan River Valley subsidence.

The West Swale earth science features include glaciofluvial Iandforms created by meltwater channels during Pleistocene glacial drainage. The afforestation area formerly known as George Genereux Urban Regional Park, Richard St. Barbe Baker Afforestation Area, the Chappell Marsh Conservation Area and Maple Grove at the West Swale Confluence are all provincially significant examples of a landscape typifying fluvioglacial erosion.

Meltwater channels are unique and significant as they possess characteristics which distinguish them from conventional river valleys. The low lying area of the West Swale does, indeed, display a fascinating geological record of the last stages of the Great Ice Age. On a walk in the Richard St. Barb Baker Afforestation Area, or the Urban Regional Park formerly named George Genereux park, and spend an absolutely unforgettable day 2.6 million years in the making.

The West Swale lands are of imperative value to surrounding rural agricultural lands at the present moment, but the lands also provide flood relief in the South West sector in Saskatoon. There are notable and significant geological features providing scientific, educational, historical and aesthetic landscape importance to the city of Saskatoon, the province of Saskatchewan, the nation of Canada.

What happened during the Pleistocene era?

2,588,000 to 11,700 years ago

“During the Quaternary period, between 2 and 3 million years ago, the prairies were covered by a glacier, the Laurentide ice sheet.

Northern hemisphere glaciation during the last ice ages. The accumulation of 3 to 4 kilometers (1.9 to 2.5 mi) thick ice sheets caused a sea level lowering of about 120 meters (390 ft)
Northern hemisphere glaciation during the last ice ages. The accumulation of 3 to 4 kilometers (1.9 to 2.5 mi) thick ice sheets caused a sea level lowering of about 120 meters (390 ft)

It was 3 kilometers (1.9 mi) thick which advanced and receded several times across the prairies. There were multiple glaciations affecting the Saskatchewan area during the Pre-Illinoian, Illinioan, and Wisconsin stages of the last Ice Age.” Geology These were the major glaciations, there were other glaciations summarized as follows.

Glacial Lake Agassiz A glacial lake is a lake with origins in a melted glacier. They are formed when a glacier erodes the land, and then melts, filling the hole or space that it has created. Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes.
Glacial Lake Agassiz A glacial lake is a lake with origins in a melted glacier. They are formed when a glacier erodes the land, and then melts, filling the hole or space that it has created. Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes.

Ice retreated, and drainage occurred to the north, creating Glacial lakes in low lying areas. Glacial Lake Saskatoon I situated in the northern Saskatoon Lowland and lower areas of the Elstow Basin. When the northern outlet of Lake Saskatoon lowered, the South Saskatchewan River Valley began replacing Glacial Lake Saskatoon I. A broad plain called the Cory Plain was created in the area south west of Saskatoon. Cory Plain features cut off meander loops, ox-bow lakes and geological features showing the historic river braiding and travels.

The northern flow of water in the Glacial North Saskatchewan River Valley was halted by ice, creating Glacial Rice Lake settling into the lowlands west of Grandora. Glacial Rice Lake drained by channels into the South Saskatchewan Valley “The Moon Lake Channel, a major spillway connecting the North Saskatchewan River basin with the South Saskatchewan, and a smaller parallel channel, Yorath Island Channel, also cross the Cory plain….but they are clearly not South Saskatchewan channels.”

Yorath Island Channel, Moon Lake Channel, Sutherland Channel and Cory Plain Channel Pleistocene Era South Sk River Valley 2588000 to 117000 years ago Adapted from Larry Edwin Hodges
Yorath Island Channel, Moon Lake Channel, Sutherland Channel and Cory Plain Channel Pleistocene Era South Sk River Valley 2588000 to 117000 years ago Adapted from Larry Edwin Hodges

Then there was another advance of ice ~ Patience Lake Ice ~ creating a kame and moraine ridge near Grandora 10 miles west of Saskatoon. The ice blocked the northern flow of water creating another glacial lake; Lake Saskatoon II. As the ice wasted away, & Lake returned to river valley, there were remnants of the lake in and south of Saskatoon. Lacustrine silts and clays were deposited south and west of the city area forming the Cory Plain surface. Paraphrase from Hodges

How is it best to preserve our nation’s geologic heritage which contain evidence some of the earth’s greatest examples of geologic phenomena. From glaciers to swales, it is a true inspiration to be immersed in your personal geologic experience here in the West Swale which envelopes the Chappell Marsh Conservation Area, Richard St. Barbe Baker Afforestation Area and the Afforestation Area formerly known as George Genereux urban regional park. Yorath Island, an “end moraine” and a natural landmark in the South Saskatchewan River locates the confluence of the Yorath Island spillway with the glacial South Saskatchewan River Valley. The West Swale is a low-lying depression created by repeated glaciations and the melting of the last bit of glacial ice.

The West Swale, a major meltwater drainage channel, a glacial spillway and a prairie valley is a classical example of glacial spillway topography. In the West Swale are several areas and features that budding geologists can discover and study the results left behind as the “catastrophic floods of glacial meltwater and sediment washed through these valleys”, typifying the Yorath Island glacial spillway, now known as the West Swale.James S. Aber Pleistocene deposits and geology show “erosional features of the underlying bedrock surface such as buried valleys, which are filled and concealed by drift, and which result in a hickening of Pleistocene deposits; erosional features of the surface of the drift, such as stream valleys, which cause a thinning of the Pleistocene deposits; and depositional features such as end moraines, drumlins, and outwash plains of glacial origin, which result in a thickening of the Pleistocene deposits.P.F. Karrow

The preservation of the afforestation areas in 1972, therefore, has also preserved a segment of the invaluable historic geological landmark of the West Swale, and its Pleistocene heritage and history.  Next time you are out at the Richard St. Barb Baker Afforestation Area, or the Urban Regional Park formerly named George Genereux park, know you are spending an absolutely unforgettable day 2.6 million years in the making.

The 1884 Sectional Map and the 1915 Saskatoon Sheet both do a brilliant job showing the West Swale around the Blairmore Afforestation Areas.

Now it is time to zip on over to an adventure amid the Pleistocene Megafauna – with an online virtual tour to meet the mammoths, sabre-tooth cats, and tapirs.

BIBLIOGRAPHY:
Hodges, Larry Edwin: Morphology of the South Saskatchewan River Valley Outlook to Saskatoon PhD Thesis. Department of Geography. McGill University. Montreal, Quebec. July 1971.
Theberge, John B., (1989) The Wholeness of Nature. Legacy, The Natural History of Ontario. McClelland and Stewart Inc. ISBN 0-7710-8398-X

For directions as to how to drive to “George Genereux” Urban Regional Park

For directions on how to drive to Richard St. Barbe Baker Afforestation Area

For more information:

Blairmore Sector Plan Report; planning for the Richard St. Barbe Baker Afforestation Area,  George Genereux Urban Regional Park and West Swale and areas around them inside of Saskatoon city limits

P4G Saskatoon North Partnership for Growth The P4G consists of the Cities of Saskatoon, Warman, and Martensville, the Town of Osler and the Rural Municipality of Corman Park; planning for areas around the afforestation area and West Swale outside of Saskatoon city limits

Richard St. Barbe Baker Afforestation Area is located in Saskatoon, Saskatchewan, Canada north of Cedar Villa Road, within city limits, in the furthest south west area of the city. 52° 06′ 106° 45′
Addresses:
Part SE 23-36-6 – Afforestation Area – 241 Township Road 362-A
Part SW 23-36-6 – SW Off-Leash Recreation Area (Richard St. Barbe Baker Afforestation Area ) – 355 Township Road 362-A
S ½ 22-36-6 Richard St. Barbe Baker Afforestation Area (West of SW OLRA) – 467 Township Road 362-A
NE 21-36-6 “George Genereux” Afforestation Area – 133 Range Road 3063
Wikimapia Map: type in Richard St. Barbe Baker Afforestation Area
Google Maps South West Off Leash area location pin at parking lot
Web page: https://stbarbebaker.wordpress.com
Where is the Richard St. Barbe Baker Afforestation Area? with map
Where is the George Genereux Urban Regional Park (Afforestation Area)? with map

Pinterest richardstbarbeb

Facebook Group Page: Users of the George Genereux Urban Regional Park

Facebook: StBarbeBaker

Facebook group page : Users of the St Barbe Baker Afforestation Area

Facebook: South West OLRA

Twitter: StBarbeBaker

Please help protect / enhance /commemorate your afforestation areas, please contact the Friends of the Saskatoon Afforestation Areas Inc. (e-mail)

Support the afforestation areas with your donation or membership ($20.00/year).  Please donate by paypal using the e-mail friendsafforestation AT gmail.com, or by using e-transfers  Please and thank you!  Your donation and membership is greatly appreciated.  Members e-mail your contact information to be kept up to date!

QR Code FOR PAYPAL DONATIONS to the Friends of the Saskatoon Afforestation Areas Inc.
Paypal
Payment Options
Membership : $20.00 CAD – yearly
Membership with donation : $50.00 CAD
Membership with donation : $100.00 CAD

1./ Learn.

2./ Experience

3./ Do Something: ***

You Tube Video Richard St. Barbe Baker Afforestation Area

You Tube Video Richard St Barbe Baker presented by Paul Hanley

You Tube Video Richard St Barbe Baker Afforestation Area and West Swale wetlands

You Tube Video Richard St. Barbe Baker Afforestation Area – Saskatoon’s best kept secret.

 

The trees and vegetation, which cover the land surface of the Earth and delight the eye, are performing vital tasks incumbent upon the vegetable world in nature. Its presence is essential to earth as an organism. It is the first condition of all life; it it the ‘skin’ of the earth, for without it there can be no water, and therefore, no life.~Richard St. Barbe Baker

 

It is not a farce.…”To be whole. To be complete. Wildness reminds us what it means to be human, what we are connected to rather than what we are separate from.” ~Terry Tempest Williams

 

“Clearly, human pressure is exerting a sudden and cataclysmic impact on much of this province, if viewed in the time-frame of evolution and geology to which the rhythms of ecosystems are tuned. The groundswell of environmental concern taking shape among us, its citizens, results in public pressure for new and stronger strictures on human exploitation and desecration…Such action is needed as the embodiment of an ethical responsibility to the land and living things, for our own well-being as well as for that of all other species.” Theberge, 1989. P.376

 

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