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Main Photo: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 1: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 2: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 3: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 4: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 5: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 6: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 7: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 8: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 9: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Photo 10: RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591
Status:
Active
Prop. Type:
Farm
MLS® Num:
SK986591
This half section of pasture land is all in native grass. The land has perimeter and cross fencing, allowing for ease of moving cattle. There is fresh water on the north quarter. There is road access on the south quarter.
Call Salesperson for directions
Listing Area:
Perdue Rm No. 346
Property Type:
Farm
Property Sub Type:
Hay
Property Offered:
Land Only
Lot Size:
319.18 acre(s)
Nearest Town:
Perdue
Date Listed:
Days on Mkt:
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Listed by RE/MAX Saskatoon
Data was last updated November 15, 2024 at 01:35 AM (UTC)
Steve LeBlanc
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RM346 Perdue Land in Perdue Rm No. 346: Farm for sale : MLS®# SK986591

Saskatchewan is a province in Western Canada, bordered on the west by Alberta, on the north by the Northwest Territories, on the east by Manitoba, to the northeast by Nunavut, and to the south by the United States (Montana and North Dakota). Saskatchewan and Alberta are the only landlocked provinces of Canada. In 2023, Saskatchewan’s population was estimated at 1,225,493.[8] Nearly 10% of Saskatchewan’s total area of 651,900 km2 (251,700 sq mi) is fresh water, mostly rivers, reservoirs, and lakes.

Residents primarily live in the southern prairie half of the province, while the northern half is mostly forested and sparsely populated. Roughly half live in the province’s largest city Saskatoon or the provincial capital Regina. Other notable cities include Prince Albert, Moose Jaw, Yorkton, Swift Current, North Battleford, Estevan, Weyburn, Melfort, and the border city Lloydminster.[9] English is the primary language of the province, with 82.4% of Saskatchewanians speaking English as their first language.[10]

Saskatchewan has been inhabited for thousands of years by indigenous groups. Europeans first explored the area in 1690 and first settled in the area in 1774. It became a province in 1905, carved out from the vast North-West Territories, which had until then included most of the Canadian Prairies. In the early 20th century, the province became known as a stronghold for Canadian social democracy; North America’s first social-democratic government was elected in 1944. The province’s economy is based on agriculture, mining, and energy

Saskatchewan is the only province without a natural border. As its borders follow geographic lines of longitude and latitude, the province is roughly a quadrilateral, or a shape with four sides. However, the southern border on the 49th parallel and the northern border on the 60th parallel curve to the left as one proceeds east, as do all parallels in the Northern Hemisphere. Additionally, the eastern boundary of the province follows range lines and correction lines of the Dominion Land Survey, laid out by surveyors prior to the Dominion Lands Act homestead program (1880–1928).

Saskatchewan is part of the western provinces and is bounded on the west by Alberta, on the north by the Northwest Territories, on the north-east by Nunavut, on the east by Manitoba, and on the south by the U.S. states of Montana and North Dakota. Saskatchewan has the distinction of being the only Canadian province for which no borders correspond to physical geographic features (i.e. they are all parallels and meridians). Along with Alberta, Saskatchewan is one of only two land-locked provinces.

The overwhelming majority of Saskatchewan’s population is in the southern third of the province, south of the 53rd parallel.

Saskatchewan contains two major natural regions: the boreal forest in the north and the prairies in the south. They are separated by an aspen parkland transition zone near the North Saskatchewan River on the western side of the province, and near to south of the Saskatchewan River on the eastern side.

Northern Saskatchewan is mostly covered by forest except for the Lake Athabasca Sand Dunes, the largest active sand dunes in the world north of 58°, and adjacent to the southern shore of Lake Athabasca. Southern Saskatchewan contains another area with sand dunes known as the “Great Sand Hills” covering over 300 km2 (120 sq mi). The Cypress Hills, in the southwestern corner of Saskatchewan and Killdeer Badlands (Grasslands National Park), are areas of the province that were unglaciated during the last glaciation period, the Wisconsin glaciation.

The province’s highest point, at 1,392 m (4,567 ft), is in the Cypress Hills less than 2 km (1.2 mi) from the provincial boundary with Alberta.[14] The lowest point is the shore of Lake Athabasca, at 213 m (699 ft). The province has 14 major drainage basins made up of various rivers and watersheds draining into the Arctic Ocean, Hudson Bay and the Gulf of Mexico.[15]

Climate

climate types of Saskatchewan
Saskatchewan receives more hours of sunshine than any other Canadian province.[16] The province lies far from any significant body of water. This fact, combined with its northerly latitude, gives it a warm summer, corresponding to its humid continental climate (Köppen type Dfb) in the central and most of the eastern parts of the province, as well as the Cypress Hills; drying off to a semi-arid steppe climate (Köppen type BSk) in the southwestern part of the province. Drought can affect agricultural areas during long periods with little or no precipitation at all.

The northern parts of Saskatchewan – from about La Ronge northward – have a subarctic climate (Köppen Dfc) with a shorter summer season. Summers can get very hot, sometimes above 38 °C (100 °F) during the day, and with humidity decreasing from northeast to southwest.

Warm southern winds blow from the plains and intermontane regions of the Western United States during much of July and August, very cool or hot but changeable air masses often occur during spring and in September. Winters are usually bitterly cold, with frequent Arctic air descending from the north.[17] with high temperatures not breaking ?17 °C (1 °F) for weeks at a time. Warm chinook winds often blow from the west, bringing periods of mild weather. Annual precipitation averages 30 to 45 centimetres (12 to 18 inches) across the province, with the bulk of rain falling in June, July, and August.[18]

Saskatchewan is one of the most tornado-active parts of Canada, averaging roughly 12 to 18 tornadoes per year, some violent. In 2012, 33 tornadoes were reported in the province. The Regina Cyclone took place in June 1912 when 28 people died in an F4 Fujita scale tornado. Severe and non-severe thunderstorm events occur in Saskatchewan, usually from early spring to late summer. Hail, strong winds and isolated tornadoes are a common occurrence.

The hottest temperature ever recorded in Saskatchewan was in July 1937 when the temperature rose to 45 °C (113 °F) in Midale and Yellow Grass. The coldest ever recorded in the province was ?56.7 °C (?70.1 °F) in Prince Albert, north of Saskatoon, in February 1893.

The first known European to enter Saskatchewan was Henry Kelsey from England in 1690, who travelled up the Saskatchewan River in hopes of trading fur with the region’s indigenous peoples. Fort La Jonquière and Fort de la Corne were first established in 1751 and 1753 by early French explorers and traders. The first permanent European settlement was a Hudson’s Bay Company post at Cumberland House, founded in 1774 by Samuel Hearne.[23] The southern part of the province was part of Spanish Louisiana from 1762 until 1802.[24]

19th century
In 1803, the Louisiana Purchase transferred from France to the United States part of what is now Alberta and Saskatchewan. In 1818, the U.S. ceded the area to Britain. Most of what is now Saskatchewan was part of Rupert’s Land and controlled by the Hudson’s Bay Company, which claimed rights to all watersheds flowing into Hudson Bay, including the Saskatchewan River, Churchill, Assiniboine, Souris, and Qu’Appelle River systems.

In the late 1850s and early 1860s, scientific expeditions led by John Palliser and Henry Youle Hind explored the prairie region of the province.

In 1870, Canada acquired the Hudson’s Bay Company’s territories and formed the North-West Territories to administer the vast territory between British Columbia and Manitoba. The Crown also entered into a series of numbered treaties with the indigenous peoples of the area, which serve as the basis of the relationship between First Nations, as they are called today, and the Crown. Since the late twentieth century, land losses and inequities as a result of those treaties have been subject to negotiation for settlement between the First Nations in Saskatchewan and the federal government, in collaboration with provincial governments.

In 1876, following their defeat of United States Army forces at the Battle of the Little Bighorn in Montana Territory in the United States, the Lakota Chief Sitting Bull led several thousand of his people to Wood Mountain. Survivors and descendants founded Wood Mountain Reserve in 1914.

The North-West Mounted Police set up several posts and forts across Saskatchewan, including Fort Walsh in the Cypress Hills, and Wood Mountain Post in south-central Saskatchewan near the United States border.

The 1885 Battle of Batoche was a battle during the North-West Rebellion. 1885 illustration by Sergeant Grundy
Many Métis people, who had not been signatories to a treaty, had moved to the Southbranch Settlement and Prince Albert district north of present-day Saskatoon following the Red River Rebellion in Manitoba in 1870. In the early 1880s, the Canadian government refused to hear the Métis’ grievances, which stemmed from land-use issues.

Finally, in 1885, the Métis, led by Louis Riel, staged the North-West Rebellion and declared a provisional government. They were defeated by a Canadian militia brought to the Canadian prairies by the new Canadian Pacific Railway. Riel, who surrendered and was convicted of treason in a packed Regina courtroom, was hanged on November 16, 1885. Since then, the government has recognized the Métis as an aboriginal people with status rights and provided them with various benefits.

European settlements
The national policy set by the federal government, the Canadian Pacific Railway, the Hudson’s Bay Company and associated land companies encouraged immigration. The Dominion Lands Act of 1872 permitted settlers to acquire one-quarter of a square mile of land to homestead and offered an additional quarter upon establishing a homestead. In 1874, the North-West Mounted Police began providing police services. In 1876, the North-West Territories Act provided for appointment, by the Ottawa, of a Lieutenant Governor and a Council to assist him.[25]


Highly optimistic advertising campaigns promoted the benefits of prairie living. Potential immigrants read leaflets that described Canada as a favourable place to live and downplayed the need for agricultural expertise. Ads in The Nor’-West Farmer by the Commissioner of Immigration implied that western land held water, wood, gold, silver, iron, copper, and cheap coal for fuel, all of which were readily at hand. The reality was far harsher, especially for the first arrivals who lived in sod houses. However eastern money poured in and by 1913, long term mortgage loans to Saskatchewan farmers had reached $65 million.[26]

The dominant groups comprised British settlers from eastern Canada and Britain, who comprised about half of the population during the late 19th and early 20th centuries. They played the leading role in establishing the basic institutions of plains society, economy and government.[27]

Source https://en.wikipedia.org/wiki/Saskatchewan

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mobile back ground john deere combine Alberta and Saskatchewan Commercial & Industrial
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topsoil Depth (in) Alberta Source aafc slc version 3.2

Understanding Topsoil Depth in Alberta: Insights from AAFC SLC Version 3.2 Data

Topsoil depth is a critical factor for agricultural productivity, influencing water retention, nutrient availability, and root growth. The provided map of Alberta illustrates the topsoil depth in inches, highlighting significant regional variations. This analysis is based on data from the Agriculture and Agri-Food Canada (AAFC) Soil Landscapes of Canada (SLC) Version 3.2.

Key Observations

The topsoil depth in Western Alberta and the Rockies is generally shallow, ranging from 0 to 6 inches. This is due to the rugged terrain and erosional processes associated with mountainous regions. The shallow topsoil in these areas supports forests and natural vegetation rather than extensive agriculture.

Central Alberta, including areas around Edmonton and Red Deer, exhibits moderate to deep topsoil depths, generally between 8 to 14 inches. These depths are conducive to productive agriculture, supporting a variety of crops. The deeper topsoil in central regions contributes to higher agricultural yields and sustainable farming practices.

In Southern and Eastern Alberta, regions such as Calgary and areas towards the Saskatchewan border show variable topsoil depths ranging from 6 to 10 inches. While suitable for agriculture, these areas may require careful soil management to maintain productivity. Areas with shallower topsoil are more drought-resistant and may need irrigation and soil conservation practices.

Regional Analysis

The Rocky Mountain Influence is evident in the shallow topsoil of the Rocky Mountain foothills, resulting from the rocky and rugged terrain, limiting soil accumulation. These areas are more suited to forest growth and natural vegetation rather than intensive agriculture.

In contrast, the Prairie Conditions in central Alberta benefit from moderate to deep topsoil, which is ideal for crop production and supports Alberta’s agricultural economy. Maintaining topsoil depth through conservation practices is essential for sustaining long-term agrarian productivity in these areas.

Implications for Agriculture

Understanding topsoil depth is crucial for effective soil management practices, including crop selection, irrigation, and fertilization. Farmers can use this data to optimize their farming practices, choosing crops suited to the available topsoil depth and implementing appropriate soil conservation measures. Deeper topsoil improves water retention and nutrient availability, which is essential for healthy crop growth and high yields.

Conclusion

The topsoil depth map of Alberta reveals significant regional variations influenced by geographical features such as the Rocky Mountains and the fertile plains of central Alberta. Understanding these variations is crucial for optimizing agricultural practices and ensuring sustainable farming. By leveraging this data, farmers can improve crop yields, manage soil health, and enhance overall agrarian productivity in Alberta.

Sources

  • Agriculture and Agri-Food Canada (AAFC) Soil Landscapes of Canada (SLC) Version 3.2 Data
  • Alberta Agriculture and Forestry






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