Alberta Ranch For Sale on MLS®
731072 Rang Road 124
Rural Grande Prairie County
Rural Grande Prairie No. 1, County of
T0H 2C0
$575,000
Agri-Business
beds: 5
baths: 3.0
- Status:
- Active
- Prop. Type:
- Agri-Business
- MLS® Num:
- A2175206
- Bedrooms:
- 5
- Bathrooms:
- 3
- Photos (49)
- Schedule / Email
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- Mortgage calculator
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Schedule a viewing:
- Property Type:
- Agri-Business
- Property Sub Type:
- Agriculture
- Transaction Type:
- For Sale
- Possession:
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- Possession Date:
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- Major Use Description:
- Hobby Farm
- Lower Level Finished Area:
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- Above Grade Finished Area:
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- Taxes:
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- Tax Assessed Value:
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- HOA Fee Includes:
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- Lot Area:
- 19.01 acre(s)7.69 hectare(s)
- Acres Cleared:
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- Acres Cultivated:
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- Acres Irrigated:
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- Acres Leasehold:
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- Acres Not Cultivated:
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- Acres Freehold:
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- Acres Seeded:
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- Acres Tame Hay:
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- Acres Treed:
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- Acres Waste:
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- Acres Water Rights:
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- Reg. Size:
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- Reg. Size Includes:
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- Total Rooms Above Grade:
- 3
- Bedrooms:
- 5 (Above Grd: 3)
- Bedrooms Above Grade:
- 3
- Bedrooms Below Grade:
- 2
- Bathrooms:
- 3.0 (Full:2, Half:1)
- Plan:
- 0624877
- Ensuite:
- No
- Garage:
- 0
- NONE
- Fridge, stove, dishwasher, washer, dryer, window coverings, generator, stock waterer
- None Known
- Floor
- Type
- Size
- Other
- Main Floor
- Bedroom
- 11'6"3.51 m × 10'10"3.30 m
- Upper Level
- Bedroom
- 9'10"3.00 m × 9'10"3.00 m
- Upper Level
- Bedroom
- 9'10"3.00 m × 9'10"3.00 m
- Basement
- Bedroom
- 10'6"3.20 m × 9'2.74 m
- Bedroom - Primary
- 14'3"4.34 m × 13'7"4.14 m
- Floor
- Ensuite
- Pieces
- Other
- Main Floor
- No
- 2
- 0' x 0'
- Upper Level
- No
- 5
- 0' x 0'
- Basement
- No
- 4
- 0' x 0'
- Title to Land:
- Fee Simple
- Num. of Parcels:
- 0
- Nearest Town:
- Hythe
- Region:
- Grande Prairie No. 1, County of
- Zoning:
- AG
- Listed Date:
- Oct 24, 2024
- Days on Mkt:
- Signup
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- Steve LeBlanc
- Marcel LeBlanc Real Estate Inc.
- 403-391-6447
- Contact by Email
Alberta Ranch For Sale
Alberta is one of the thirteen provinces and territories of Canada. It is a part of Western Canada and is one of the three prairie provinces. Alberta borders British Columbia to the west, Saskatchewan to the east, the Northwest Territories to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada, with Saskatchewan being the other.
The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds.[9]
Alberta is the fourth largest province by area at 661,848 square kilometres (255,541 square miles),[10] and the fourth most populous, being home to 4,262,635 people.[2] Alberta’s capital is Edmonton, while Calgary is its largest city.[11] The two are Alberta’s largest census metropolitan areas.[12] More than half of Albertans live in either Edmonton or Calgary, which contributes to continuing the rivalry between the two cities. English is the official language of the province. In 2016, 76.0% of Albertans were anglophone, 1.8% were francophone and 22.2% were allophone.[13]
Alberta’s economy is based on hydrocarbons, petrochemical industries, livestock and agriculture.[14] The oil and gas industry has been a pillar of Alberta’s economy since 1947, when substantial oil deposits were discovered at Leduc No. 1 well.[15] It has also become a part of the province’s identity. Since Alberta is the province most rich in hydrocarbons, it provides 70% of the oil and natural gas produced on Canadian soil. In 2018, Alberta’s output was CA$338.2 billion, 15.27% of Canada’s GDP.[16][17]
Alberta is renowned for its natural beauty, richness in fossils and for housing important nature reserves. Alberta is home to six UNESCO designated World Heritage Sites: the Canadian Rocky Mountain Parks, Dinosaur Provincial Park, Head-Smashed-In Buffalo Jump, Waterton-Glacier International Peace Park, Wood Buffalo National Park and Writing-on-Stone Provincial Park.[20] Other popular sites include Banff National Park, Elk Island National Park, Jasper National Park, Waterton Lakes National Park, and Drumheller.
Main article: Geography of Alberta
Alberta, with an area of 661,848 square kilometres (255,541 square miles), is the fourth-largest province after Quebec, Ontario, and British Columbia.[26]
Alberta’s southern border is the 49th parallel north, which separates it from the U.S. state of Montana. The 60th parallel north divides Alberta from the Northwest Territories. The 110th meridian west separates it from the province of Saskatchewan; while on the west its boundary with British Columbia follows the 120th meridian west south from the Northwest Territories at 60°N until it reaches the Continental Divide at the Rocky Mountains, and from that point follows the line of peaks marking the Continental Divide in a generally southeasterly direction until it reaches the Montana border at 49°N.[27]
The province extends 1,223 kilometres (760 miles) north to south and 660 kilometres (410 miles) east to west at its maximum width. Its highest point is 3,747 metres (12,293 feet) at the summit of Mount Columbia in the Rocky Mountains along the southwest border while its lowest point is 152 metres (499 feet) on the Slave River in Wood Buffalo National Park in the northeast.[28]
With the exception of the semi-arid climate of the steppe in the south-eastern section, the province has adequate water resources. There are numerous rivers and lakes in Alberta used for swimming, fishing and a range of water sports. There are three large lakes, Lake Claire (1,436 km2 [554 sq mi]) in Wood Buffalo National Park, Lesser Slave Lake (1,168 km2 [451 sq mi]), and Lake Athabasca (7,898 km2 [3,049 sq mi]), which lies in both Alberta and Saskatchewan. The longest river in the province is the Athabasca River, which travels 1,538 km (956 mi) from the Columbia Icefield in the Rocky Mountains to Lake Athabasca.[29]
The largest river is the Peace River with an average flow of 2,100 m3/s (74,000 cu ft/s).[30] The Peace River originates in the Rocky Mountains of northern British Columbia and flows through northern Alberta and into the Slave River, a tributary of the Mackenzie River.
Alberta’s capital city, Edmonton, is located at about the geographic centre of the province. It is the most northerly major city in Canada and serves as a gateway and hub for resource development in northern Canada. With its proximity to Canada’s largest oil fields, the region has most of western Canada’s oil refinery capacity. Calgary is about 280 km (170 mi) south of Edmonton and 240 km (150 mi) north of Montana, surrounded by extensive ranching country. Almost 75% of the province’s population lives in the Calgary–Edmonton Corridor. The land grant policy to the railways served as a means to populate the province in its early years.[31]
Most of the northern half of the province is boreal forest, while the Rocky Mountains along the southwestern boundary are largely temperate coniferous forests of the Alberta Mountain forests and Alberta–British Columbia foothills forests. The southern quarter of the province is prairie, ranging from shortgrass prairie in the southeastern corner to mixed grass prairie in an arc to the west and north of it.
The central aspen parkland region extending in a broad arc between the prairies and the forests, from Calgary, north to Edmonton, and then east to Lloydminster, contains the most fertile soil in the province and most of the population. Much of the unforested part of Alberta is given over either to grain or to dairy farming, with mixed farming more common in the north and centre, while ranching and irrigated agriculture predominate in the south.[32]
The Alberta badlands are located in southeastern Alberta, where the Red Deer River crosses the flat prairie and farmland, and features deep canyons and striking landforms. Dinosaur Provincial Park, near Brooks, showcases the badlands terrain, desert flora, and remnants from Alberta’s past when dinosaurs roamed the then lush landscape.
Climate
Alberta extends for over 1,200 km (750 mi) from north to south; its climate, therefore, varies considerably. Average high temperatures in January range from 0 °C (32 °F) in the southwest to ?24 °C (?11 °F) in the far north. The presence of the Rocky Mountains also influences the climate to the southwest, which disrupts the flow of the prevailing westerly winds and causes them to drop most of their moisture on the western slopes of the mountain ranges before reaching the province, casting a rain shadow over much of Alberta.
The northerly location and isolation from the weather systems of the Pacific Ocean cause Alberta to have a dry climate with little moderation from the ocean. Annual precipitation ranges from 300 mm (12 in) in the southeast to 450 mm (18 in) in the north, except in the foothills of the Rocky Mountains where total precipitation including snowfall can reach 600 mm (24 in) annually.[28][33]
Northern Alberta is mostly covered by boreal forest and has a subarctic climate. The agricultural area of southern Alberta has a semi-arid steppe climate because the annual precipitation is less than the water that evaporates or is used by plants.
The southeastern corner of Alberta, part of the Palliser Triangle, experiences greater summer heat and lower rainfall than the rest of the province, and as a result, suffers frequent crop yield problems and occasional severe droughts.
Western Alberta is protected by the mountains and enjoys the mild temperatures brought by winter Chinook winds. Central and parts of northwestern Alberta in the Peace River region are largely aspen parkland, a biome transitional between prairie to the south and boreal forest to the north.
Alberta has a humid continental climate with warm summers and cold winters. The province is open to cold Arctic weather systems from the north, which often produce cold winter conditions. As the fronts between the air masses shift north and south across Alberta, the temperature can change rapidly. Arctic air masses in the winter produce extreme minimum temperatures varying from ?54 °C (?65 °F) in northern Alberta to ?46 °C (?51 °F) in southern Alberta, although temperatures at these extremes are rare.
In the summer, continental air masses have produced record maximum temperatures from 32 °C (90 °F) in the mountains to over 40 °C (104 °F) in southeastern Alberta.[34] Alberta is a sunny province. Annual bright sunshine totals range between 1,900 up to just under 2,600 hours per year. Northern Alberta gets about 18 hours of daylight in the summer.[34] The average daytime temperatures range from around 21 °C (70 °F) in the Rocky Mountain valleys and far north, up to around 28 °C (82 °F) in the dry prairie of the southeast.
The northern and western parts of the province experience higher rainfall and lower evaporation rates caused by cooler summer temperatures. The south and east-central portions are prone to drought-like conditions sometimes persisting for several years, although even these areas can receive heavy precipitation, sometimes resulting in flooding.
In the winter, the Alberta clipper, a type of intense, fast-moving winter storm that generally forms over or near the province and, pushed with great speed by the continental polar jetstream, descends over the rest of southern Canada and the northern tier of the United States.[35] In southwestern Alberta, the cold winters are frequently interrupted by warm, dry Chinook winds blowing from the mountains, which can propel temperatures upward from frigid conditions to well above the freezing point in a very short period.
During one Chinook recorded at Pincher Creek, temperatures soared from ?19 to 22 °C (?2 to 72 °F) in just one hour.[28] The region around Lethbridge has the most Chinooks, averaging 30 to 35 Chinook days per year. Calgary has a 56% chance of a white Christmas, while Edmonton has an 86% chance.[36]
After Saskatchewan, Alberta experiences the most tornadoes in Canada with an average of 15 verified per year.[37] Thunderstorms, some of them severe, are frequent in the summer, especially in central and southern Alberta. The region surrounding the Calgary–Edmonton Corridor is notable for having the highest frequency of hail in Canada, which is caused by orographic lifting from the nearby Rocky Mountains, enhancing the updraft/downdraft cycle necessary for the formation of hail.
History
Main article: History of Alberta
See also: Timeline of Alberta history
Paleo-Indians arrived in Alberta at least 10,000 years ago, toward the end of the last ice age. They are thought to have migrated from Siberia to Alaska on a land bridge across the Bering Strait and then possibly moved down the east side of the Rocky Mountains through Alberta to settle the Americas. Others may have migrated down the coast of British Columbia and then moved inland.[49] Over time they differentiated into various First Nations peoples, including the Plains Indians of southern Alberta such as those of the Blackfoot Confederacy and the Plains Cree, who generally lived by hunting buffalo, and the more northerly tribes such as the Woodland Cree and Chipewyan who hunted, trapped, and fished for a living.[28]
The first Europeans to visit Alberta were French Canadians during the late 18th century, working as fur traders. French was the predominant language used in some early fur trading forts in the region, such as the first Fort Edmonton (in present-day Fort Saskatchewan). After the British arrival in Canada, approximately half of the province of Alberta, south of the Athabasca River drainage, became part of Rupert’s Land which consisted of all land drained by rivers flowing into Hudson Bay. This area was granted by Charles II of England to the Hudson’s Bay Company (HBC) in 1670, and rival fur trading companies were not allowed to trade in it.
The Athabasca River and the rivers north of it were not in HBC territory because they drained into the Arctic Ocean instead of Hudson Bay, and they were prime habitats for fur-bearing animals. The first European explorer of the Athabasca region was Peter Pond, who learned of the Methye Portage, which allowed travel from southern rivers into the rivers north of Rupert’s Land.
Other North American fur traders formed the North West Company (NWC) of Montreal to compete with the HBC in 1779. The NWC occupied the northern part of Alberta territory. Peter Pond built Fort Athabasca on Lac la Biche in 1778. Roderick Mackenzie built Fort Chipewyan on Lake Athabasca ten years later in 1788. His cousin, Sir Alexander Mackenzie, followed the North Saskatchewan River to its northernmost point near Edmonton, then setting northward on foot, trekked to the Athabasca River, which he followed to Lake Athabasca.
It was there he discovered the mighty outflow river which bears his name—the Mackenzie River—which he followed to its outlet in the Arctic Ocean. Returning to Lake Athabasca, he followed the Peace River upstream, eventually reaching the Pacific Ocean, and so he became the first European to cross the North American continent north of Mexico.[50]
The extreme southernmost portion of Alberta was part of the French (and Spanish) territory of Louisiana and was sold to the United States in 1803. In the Treaty of 1818, the portion of Louisiana north of the Forty-Ninth Parallel was ceded to Great Britain.[51]
Fur trade expanded in the north, but bloody battles occurred between the rival HBC and NWC, and in 1821 the British government forced them to merge to stop the hostilities.[52] The amalgamated Hudson’s Bay Company dominated trade in Alberta until 1870 when the newly formed Canadian Government purchased Rupert’s Land. Northern Alberta was included in the North-Western Territory until 1870, when it and Rupert’s land became Canada’s North-West Territories.
First Nations negotiated the Numbered Treaties with the Crown in which the Crown gained title to the land that would later become Alberta, and the Crown committed to the ongoing support of the First Nations and guaranteed their hunting and fishing rights. The most significant treaties for Alberta are Treaty 6 (1876), Treaty 7 (1877) and Treaty 8 (1899).
The District of Alberta was created as part of the North-West Territories in 1882. As settlement increased, local representatives to the North-West Legislative Assembly were added. After a long campaign for autonomy, in 1905, the District of Alberta was enlarged and given provincial status, with the election of Alexander Cameron Rutherford as the first premier. Less than a decade later, the First World War presented special challenges to the new province as an extraordinary number of volunteers left relatively few workers to maintain services and production. Over 50% of Alberta’s doctors volunteered for service overseas.[53]
Demographics of Alberta
The 2021 Canadian census reported Alberta had a population of 4,262,635 living in 1,633,220 of its 1,772,670 total dwellings, an 4.8% change from its 2016 population of 4,067,175. With a land area of 634,658.27 km2 (245,042.93 sq mi), it had a population density of 6.7/km2 in 2021.[2] Statistics Canada estimated the province to have a population of 4,800,768 in Q1 of 2024.[58]
Since 2000, Alberta’s population has experienced a relatively high rate of growth, mainly because of its burgeoning economy. Between 2003 and 2004, the province had high birthrates (on par with some larger provinces such as British Columbia), relatively high immigration, and a high rate of interprovincial migration compared to other provinces.[59]
In 2016, Alberta continued to have the youngest population among the provinces with a median age of 36.7 years, compared with the national median of 41.2 years. Also in 2016, Alberta had the smallest proportion of seniors (12.3%) among the provinces and one of the highest population shares of children (19.2%), further contributing to Alberta’s young and growing population.[60]
About 81% of the population lives in urban areas and only about 19% in rural areas. The Calgary–Edmonton Corridor is the most urbanized area in the province and is one of the most densely populated areas of Canada.[61] Many of Alberta’s cities and towns have experienced very high rates of growth in recent history.[when?] Alberta’s population rose from 73,022 in 1901[62] to 3,290,350 according to the 2006 census.[63]
According to the 2016 census Alberta has 779,155 residents (19.2%) between the ages of 0–14, 2,787,805 residents (68.5%) between the ages of 15–64, and 500,215 residents (12.3%) aged 65 and over.[64]
Additionally, as per the 2016 census, 1,769,500 residents hold a postsecondary certificate, diploma or degree, 895,885 residents have obtained a secondary (high) school diploma or equivalency certificate, and 540,665 residents do not have any certificate, diploma or degree.[64]
Information source: https://en.wikipedia.org/wiki/Alberta
731072 Rang Road 124 in Rural Grande Prairie No. 1, County of: Rural Grande Prairie County Agriculture for sale : MLS®# A2175206
Welcome to our Alberta Ranch MLS® Search page
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Whether looking for Farms, Ranch, Land, Commercial or Residential, you will find valuable information about the local community, amenities, and market trends. Our advanced search filters allow you to easily refine your search by location, property type, price range, and more, while interactive maps help you visualize property locations and explore surrounding areas.
Each listing includes comprehensive details, high-quality photos, and key features to assist you in making informed decisions. Additionally, Steve LeBlanc offers insights into the Alberta area real estate market, community highlights, and essential amenities, helping you understand each property’s unique characteristics.
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Maps | Data | Information
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
Saskatchewan Rm’s SCIC Average Soil Rating
Soil Class Average for Each RM in Saskatchewan: A-P Rating System
The map showing the soil class average for each Rural Municipality (RM) in Saskatchewan uses the A-P rating system, where A represents the best soil quality and P represents the lowest. This classification helps understand the agricultural potential and soil health across the province.
Key Features of the Map
A-P Rating System:
A Rating: Soils with the highest agricultural productivity potential. These soils are rich in nutrients, have good structure, and have excellent moisture retention.
P Rating: Soils with the lowest agricultural productivity potential. These may have poor fertility, high salinity, or drainage issues.
Geographical Distribution:
The map highlights the variability in soil quality across Saskatchewan. Areas with higher ratings (A, B, C) are often more suitable for intensive agriculture.
Agricultural Zones: High-quality soils predominantly support major agricultural activities in the central and southern regions of the province.
Implications for Agriculture:
Crop Selection: Farmers can use this information to select appropriate crops for their land, ensuring optimal yields.
Soil Management: Identifying lower-quality soils (rated P, O, N) can help implement targeted soil improvement practices.
Applications of the Soil Class Map
Agricultural Planning:
Optimizing Crop Yields: Farmers can determine the best areas for different types of crops based on soil quality. High-rated soils (A, B) can support more demanding crops.
Sustainable Practices: Implementing crop rotation, cover cropping, and conservation tillage can help maintain soil health.
Land Management:
Resource Allocation: Land managers can allocate resources more effectively by focusing efforts on areas with high agricultural potential.
Policy Development: Policymakers can use the map to develop strategies for soil conservation and sustainable agricultural practices.
Conclusion
Using the A-P rating system, the soil class average map for each RM in Saskatchewan is a valuable tool for farmers, land managers, and policymakers. It provides essential insights into soil quality, helping to enhance agricultural productivity, implement sustainable practices, and conserve environmental resources.
Sources
Saskatchewan Crop Insurance Corporation (SCIC)
Agriculture and Agri-Food Canada (AAFC)
Canadian Soil Information Service (CanSIS)
For more detailed information and to view the full map, you can visit the Saskatchewan Crop Insurance Corporation (SCIC) and Canadian Soil Information Service (CanSIS).
7 Saskatchewan Rm’s that contain SCIC Soil rating A
Class A Soil in Saskatchewan
Class A soil is considered premium agricultural land, offering optimal conditions for crop production due to its superior fertility, structure, and moisture retention. In Saskatchewan, seven Rural Municipalities (RMs) are renowned for having Class A soil. These regions are pivotal to the province’s agricultural success.
The 7 RMs with Class A Soil in Saskatchewan
Star City (RM 428)
It is known for its rich, loamy soil, which supports a variety of crops, including wheat, canola, and barley.
Flett’s Springs (RM 429)
The fertile soil in this RM is ideal for grain and oilseed crops, which contribute significantly to the local economy.
Invergordon (RM 430)
The Class A soil supports diverse farming operations, including mixed grain farming and livestock production.
St. Louis (RM 431)
This area is known for its productive soil, which is well-suited for high-yield crop farming.
Kinistino (RM 459)
The fertile soil in Kinistino supports a robust agricultural sector, mainly cereal and oilseed production.
Birch Hills (RM 460)
Known for its excellent soil quality, Birch Hills is a prime location for high-value crop production.
Prince Albert (RM 461)
This RM benefits from rich, fertile soil that supports a wide range of agricultural activities, making it a vital area for the province’s farming industry.
Conclusion
The seven RMs in Saskatchewan with Class A soil are crucial to the province’s agricultural success. These regions provide optimal crop growth conditions, contributing significantly to the local economy and supporting sustainable farming practices. Recognizing and preserving the value of Class A soil is essential for the continued prosperity of Saskatchewan’s farming industry.
Sources
Saskatchewan Crop Insurance Corporation (SCIC)
CP Rail 1910 Land for sale in Central Alberta
The map titled “CP Rail Lands for Sale 1910 Central Alberta” is a historical document showcasing the lands offered for sale by the Canadian Pacific Railway Company (CPR) in Central Alberta around the year 1910. Here’s a detailed analysis of the historical context, significance, and features of this map:
Historical Context
- Canadian Pacific Railway (CPR): Established in the late 19th century, the CPR played a pivotal role in the development and settlement of Western Canada. The railway facilitated transportation, trade, and migration, contributing significantly to the region’s economic growth.
- Land Sales: The CPR was granted extensive land holdings by the Canadian government as part of the incentives to build the transcontinental railway. These lands were then sold to settlers, immigrants, and investors to finance railway construction and operations.
Features of the Map - Geographical Coverage: The map covers Central Alberta, indicating the sections of land available for purchase. This region includes a mix of agricultural land and potential settlement areas.
- Land Parcels: The red shading on the map indicates the specific parcels of land that were for sale. Each parcel is meticulously plotted, showing the systematic approach to land distribution.
- Sectional Grid: The map uses a sectional grid system common in land surveying, dividing the area into manageable units for sale and development. This grid system was essential for organizing the vast tracts of land and making them accessible to buyers.
- Transportation Routes: The map highlights major transportation routes, including railways and roads, which were crucial for accessing the land and facilitating movement of goods and people.
- Topographical Features: Natural features such as rivers, lakes, and terrain types are marked on the map, providing prospective buyers with important information about the land’s characteristics and suitability for farming or other uses.
Significance - Settlement and Development: The sale of CPR lands was instrumental in populating and developing Central Alberta. It attracted settlers from various parts of Canada and abroad, contributing to the growth of agricultural communities.
- Economic Impact: The proceeds from land sales helped finance the construction and expansion of the CPR, which in turn boosted economic activities by connecting remote areas to markets and resources.
- Historical Record: Maps like these serve as valuable historical records, offering insights into land use, settlement patterns, and the economic strategies of the early 20th century. They are crucial for understanding the transformation of Western Canada from a frontier region to a developed agricultural and economic hub.
Conclusion
The “CP Rail Lands for Sale 1910 Central Alberta” map is a testament to the strategic role of the Canadian Pacific Railway in shaping the settlement and development of Western Canada. By selling land to settlers, the CPR not only financed its operations but also facilitated the growth of thriving communities in Central Alberta. This historical map provides a glimpse into the land distribution practices and the early development of the region, highlighting the interconnectedness of transportation, land use, and economic growth.
Additional Resources
For further reading and exploration of historical maps and the role of the Canadian Pacific Railway in Canadian history, you can refer to: - Historical Atlas of Canada
1967 Detailed Soil map for Saskatchewan
Saskatchewan Detailed Soil Map from 1967: A Historical Perspective
The Saskatchewan Detailed Soil Map from 1967, created by R. C. McKinnon, L. J. Schappert, and R. R. D. Cumming, is an invaluable resource for understanding the diverse soil types and their distribution across the province. This map, available through the Canadian Soil Information Service (CanSIS) and Agriculture and Agri-Food Canada (AAFC), offers detailed insights into the soil landscapes of Saskatchewan.
Key Features of the Map
Soil Classification:
The map categorizes soils into various types, each represented by distinct colors and patterns. These classifications include Brunisolic, Chernozemic, Gleysolic, Luvisolic, Organic, and Solonetzic soils.
Orthic Gray: These soils are predominantly found in the northern forested regions, indicated in blue on the map.
Black and Dark Brown: Fertile soils in agricultural areas are shown in darker shades, crucial for crop production.
Soil Texture and Composition:
Information on soil texture, such as loam, sandy loam, and clay loam, is detailed on the map. This is vital for understanding soil fertility, water retention, and suitability for different crops.
Rough Broken Land: Identified in specific regions, these areas have significant elevation changes and are less suitable for agriculture.
Saline and Solonetzic Soils:
The map marks areas with saline and Solonetzic soils, which pose challenges for agriculture due to high salt content and poor soil structure. These regions require careful management and are highlighted to aid in agricultural planning.
Importance of the Map
Agricultural Planning:
Farmers and agronomists can utilize this map to identify suitable areas for various crops based on soil type and texture, optimizing crop selection, irrigation, and soil conservation practices.
Environmental Conservation:
The map assists in identifying areas that need protection and sustainable management practices to prevent soil degradation and erosion, contributing to environmental conservation efforts.
Historical Reference:
The 1967 soil map provides a historical reference point for soil studies, allowing comparisons with modern data to assess changes in soil health and land use over time.
Conclusion
The 1967 detailed soil map of Saskatchewan remains a crucial tool for anyone involved in agriculture, land management, and environmental conservation. By providing detailed information on soil types, textures, and topographical features, it aids in making informed decisions for sustainable land use and agricultural productivity.
Sources
Saskatchewan Soil Information System
Farm address count per postal code Alberta, Saskatchewan, Manitoba
Farm Count per Postal Code:
Alberta, Saskatchewan, Manitoba
The map illustrates farm density across Alberta, Saskatchewan, and Manitoba, measured by the number of farms per postal code. This representation helps identify areas with high agricultural activity and regions with fewer farms, highlighting the distribution of farming operations in these provinces. Canada Post is the data source for this map.
Key Features of the Map
Farm Density Representation:
- Color Gradient: The map uses a color gradient to show farm density. Darker colors indicate higher farm densities, while lighter colors show lower densities.
- Farm Count Range: The farm counts range from 1 to over 600 farms per postal code, with the highest densities in dark red.
Geographical Distribution:
- High-Density Areas: Regions with darker colors, indicating higher farm densities, are primarily found in the southern and central parts of Alberta, Saskatchewan, and southern Manitoba.
Low-Density Areas: Northern regions and areas with fewer postal codes show lighter colors, indicating fewer farms.
Data Sources:
- Canada Post: Provides the postal code data, ensuring accurate representation of farm distribution.
- Agricultural Statistics: Supplementary data from agricultural agencies and Statistics Canada help validate the farm counts.
Applications of the Farm Density Map
Agricultural Planning:
- Resource Allocation: The map helps allocate agricultural resources such as seeds, fertilizers, and machinery. Areas with higher farm densities may need more resources and support services.
- Infrastructure Development: Identifying high-density farming areas can guide agricultural infrastructure development like roads, storage facilities, and irrigation systems.
Market Analysis:
- Supply Chain Optimization: Businesses can use the map to optimize supply chains by identifying regions with high agricultural output, ensuring efficient distribution of goods and services.
- Investment Decisions: Investors can use farm density data to identify promising regions for agricultural investments, supporting new ventures and expansions.
Policy Making:
- Support Programs: Policymakers can design targeted support programs for farmers based on density, focusing on areas with high farming activity to enhance productivity and sustainability.
- Rural Development: The map can inform rural development strategies, ensuring balanced growth and addressing the needs of farming communities.
Conclusion
The farm count per postal code map for Alberta, Saskatchewan, and Manitoba is essential for farmers, agronomists, businesses, and policymakers. By providing a clear picture of farm density, it supports informed decision-making in agricultural planning, market analysis, and policy development.
Sources - Canada Post
- Statistics Canada
- Government of Saskatchewan Agriculture
For more detailed information and access to the complete data, you can visit the Canada Post and Statistics Canada websites.