1884 Sectional Map

“I found it is the small everyday deeds of ordinary folk that keep the darkness at bay, small acts of kindness and love.”~ Gandalf

Department of the Interior Topographical surveys branch. Sectional Maps. Dominion Land Office April 25, 1884. Township 36 Range 6 West of the Third Meridian
Plan of Township No 36 Range 6 West of the Third Meridian. Dominion Land Office April 25, 1884.

Map Surveyed by the undersigned Frank L. Blake D.L.S. August 1883
Approved and confirmed E Deville for the Surveyor General

A map expresses a perspective {that of the cartographer}. But the map itself has not a perspective. As George Graham says, “the perspective is not in the map. It must be read into the map. The mind’s Intentionality or aboutness in underived. It inheres in it or is intrinsic to it.” He looked deeply forlorn needing to settle this  decision once and for all.

The wetlands which formed in the Pleistocene Yorath Island Spillway are very evident on the above map, and are part of what is now called the “West Swale” The West Swale extends from Yorath Island in the South Saskatchewan River through to Grandora, Rice Lake and the North Saskatchewan River [To get an overview of the West Swale check out the next Map 1915 Saskatoon Sheet which includes Grandora, etc…

“Humankind’s greatest sin is anthropocentrism – where human life is valued above all other sentient life. Msirtnecoporhtna – backwards or forwards it makes no sense. If Moses could spell it, he would have put in his top 10.” Philip Wollen founder of Winsome Kindness Trust

Blairmore Sector Afforestation Areas

Legend Additions in the colour Mauve:

How would the Blairmore Sector Afforestation Areas have featured on a map of 1883?

On the west side of Saskatoon a portion of the 660 acres preserved in perpetuity in 1972 are located at:

Richard St. Barbe Baker Afforestation Area (City of Saskatoon Urban Regional Park) Parts Section 22 and SW 23 township 36 range 6 west of the third meridian. (East of the CN overpass on SK Highway 7) SE 22 & SW 23-36-6 W3
S ½ 22-36-6 Richard St. Barbe Baker Afforestation Area (West of South West Off Leash Recreation Area) civic address 467 Township Road 362-A.  Only lands of SE 22 36 6 W3 under MVA conservation management
Part SE 23-36-6 – SW Off-Leash Recreation Area (Richard St. Barbe Baker Afforestation Area ) civic address 355 Township Road 362-A under MVA conservation
Un-named City of Saskatoon Afforestation Area. Part south of CN Chappell yards SE section 23-36-6-W3 preserved as afforestation area in perpetuity, under MVA conservation management- west of SW OLRA and east of COC.
Part SE 23-36-6 – Afforestation Area civic address 241 Township Road 362-A
In 1960, part of NE 21-36-6 W3 (West of the CN overpass on SK Highway 7) was purchased by the City, planted in 1972, preserved as an afforestation area. Named in 1978-1979 George Genereux Park (Urban Regional Park), this namesake was removed at this afforestation area for use at a different city pocket park.
NE 21-36-6 “George Genereux” Afforestation Area civic address 133 Range Road 3063

“Each person walks a journey unique to himself or herself. Live your own journey and run your own race.”  Winsome Campbell-Green

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 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
Membership with donation : $100.00 CAD

1./ Learn.

2./ Experience

3./ Do Something: ***

 

“St. Barbe’s unique capacity to pass on his enthusiasm to others. . . Many foresters all over the world found their vocations as a result of hearing ‘The Man of the Trees’ speak. I certainly did, but his impact has been much wider than that. Through his global lecture tours, St. Barbe has made millions of people aware of the importance of trees and forests to our planet.” Allan Grainger

“We forget that we owe our existence to the presence of Trees. As far as forest cover goes, we have never been in such a vulnerable position as we are today. The only answer is to plant more Trees – to Plant Trees for Our Lives.” ~ Richard St. Barbe Baker

“Act. Don’t react. See a need, fix it first. Worry about the details later. If you wait until you are asked you have just missed a golden opportunity. They are fleeting and rare.” Philip Wollen founder of Winsome Kindness Trust

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