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398 E 5th Avenue
Unity Unity S0K 4L0

$399,000
Residential beds: 4 baths: 2.0 1,884 sq. ft. built: 1953

Main Photo: 398 E 5th Avenue in Unity: Residential for sale : MLS®# SK016783
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Status:
Active
Prop. Type:
Residential
MLS® Num:
SK016783
Bedrooms:
4
Bathrooms:
2
Year Built:
1953
Eccentric and modern throughout, this incredible 1884 sq. ft. slab on grade bungalow is a breath of fresh air to view! The amount of natural lighting doesn't prevent the bold paint shades from making their statement while still feeling airy inside. Excellent design choices throughout make this space feel very cohesive and intentional with nods to the mid-century bones it was originally crafted in. From the natural wood accents, to the brick feature walls, all the way to the lighting in the laundry room and pantry. An excellent smash of old made new. The oversized corner lot has a striking appearance and offers loads of yard space, plus a double car garage with rubber cement drive and walkways. The sheltered patio space is private and cozy. The south wing of the home offers you 3 bedrooms and 4-piece main bathroom with ample hall closet storage to keep you organized. The primary bedroom is located on the north side of the home off the family room, which features its own 4-piece bathroom and walk-in closet. This space is plenty large enough for a king size bed plus furniture. But the heart of the home is right in the center and features an open concept layout with quartz countertops, custom hardware on the cabinetry, artistic lighting and upgraded appliances throughout. A truly unique and stand out property!
Listing Area:
Unity
Property Type:
Residential
Property Sub Type:
Detached
Building Type:
House
Home Style:
Bungalow
Year built:
1953 (Age: 73)
Total Floor Area:
1,884 sq. ft.
Bedrooms:
4
Number of bathrooms:
2.0
Kitchens:
1
Taxes:
$2,074 / 2025
Frontage:
75'2"
Ownership Title:
Freehold
Heating:
Forced Air, Natural Gas
Furnace:
Furnace Owned
Water Heater:
Included
Water Heater Type:
Gas
Water Softener:
Not Included
Construction:
Wood Frame
Basement:
Slab, Not applicable
Basement Walls:
Other
Roof:
Metal
Exterior Finish:
Metal, Siding
Air Conditioner (Central), Gas Bbq Hookup
Fenced, Garden Area, Lawn Back, Lawn Front, Patio, Trees/Shrubs
Heated Garage: Yes
Floor
Type
Size
Other
Main
Living Room
14'6" × 13'1"
Vinyl tile
Main
Dining Room
13'6" × 7'8"
Vinyl tile
Main
Kitchen
13'6" × 11'
Vinyl tile
Main
Laundry
7'1" × 4'11"
Vinyl tile
Main
Storage
7'6" × 6'2"
Vinyl tile
Main
Foyer
11'4" × 4'10"
Vinyl tile
Main
Recreation Room
19' × 14'
Vinyl tile
Main
Primary Bedroom
13'11" × 12'11"
Vinyl tile
Main
Other
5'6" × 5'1"
Vinyl tile
Main
Bedroom
12'4" × 9'4"
Vinyl tile
Main
Bedroom
12'8" × 9'4"
Vinyl tile
Main
Bedroom
12'11" × 11'5"
Vinyl tile
Floor
Ensuite
Pieces
Other
Main
Yes
4
5'11" x 7'11" Vinyl tile
Main
No
4
5'6" x 7'4" Vinyl tile
Occupancy:
Owner
Equipment Included:
Fridge, Stove, Washer, Dryer, Dishwasher Built In, Garage Door Opnr/Control(S), Microwave Hood Fan, Reverse Osmosis System, Window Treatment
Lot Size:
10,528 sq. ft.
Lot Shape:
Corner, Rectangular
Garage:
2 Car Detached, Parking Spaces
Garage Door WiFi:
No
Parking Places:
4.0
Parking Surface:
Double Drive, Rubber Pavement
Date Listed:
Days on Mkt:
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Listed by Oak & Stone Real Estate Unity
Data was last updated February 6, 2026 at 11:35 AM (UTC)
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Luseland Saskatchewan Information

Luseland is a small town in Rural Municipality of Progress No.351, in the west-central region of Saskatchewan. The town’s population as of the 2006 Canadian Census was 571, down 5% from the 2001 Census.[5] It is known as the hometown of the Canadian business magnate Jim Pattison. The Métis people led explorer John Palliser into this district in 1858, and it was he who saw most of the country as barren and unsuitable for agriculture. [5] Botanist John Macoun, traversing the same country in 1881 after the buffalo had been nearly wiped out, saw the country as an agricultural Eden. [6] A quarter of a century later, the first settlers arrived in the Luseland district, drawn by accounts of the rich pastures of prairie wool along the Grass Lake valley. It is for this reason that Luseland became one of the most productive wheat-growing areas in the west, boasting as many as six grain elevators. George Hoddinott and the Abbs Bros. were the first settlers, applying for a homestead, called Abbnott, in April 1906. Luseland, derived from the Luse Land and Development Company, was officially declared a village on Dec 10, 1910.[6] Established by Mr. J.F. Luse in 1904, with headquarters in St. Paul, Minnesota, its goal was to establish a German Lutheran colony for families that had initially settled in the mid-western states of Nebraska, Indiana, Wisconsin, Illinois, and Minnesota, after they had been forced to leave their Russian colonies along the Volga River. In September, 1907, Sam Luse, son of the Company president wrote the Hon. Frank Oliver, Minister of the Interior, indicating that the Co. had made a deal to purchase Canadian Northern Railway lands, provided they could secure the remaining homesteads in Townships 35 and 36, Range 24-26. The district was already located within the large German Catholic block settlement of St. Joseph’s Colony, established in 1905.[7] In November 1907, the Commission of public lands advised that though German Lutherans would make desirable settlers it was contrary to regulations to reserve homestead lands in the manner suggested. In January 1908, the Canadian representative of the Luse Co. wrote Mr. Oliver that they had closed a deal for 100,000 acres (400 km2) from the railway company along with a deal with the Evangelical German Lutheran Church for settlement. Mr. Oliver replied that they were unable to grant this request. Meanwhile, British-Canadian settlers had begun to take up homesteads in 1907, and large numbers, particularly from Ontario, began to arrive in 1908, lured by stories of the rich dark soils along the Grass Lake valley. By 1909, the Luse Land Company had arranged for several special train loads of settlers to travel to the closest station in Scott, then overland by horse and carts with their livestock and belongings to the new land. Many of these immigrants were Russian Volga Germans who had been lured from their initial settlements in the mid-western states by Canadian government propaganda and the promise of a German Lutheran colony but instead found themselves within the large St. Joseph’s Catholic colony, living side by side with British-Canadian settlers. More German settlers arrived during the next two decades, most of them coming directly from the Russian Volga colonies as conditions deteriorated there. Other ethnic and religious groups also arrived (Swiss, Polish, Hungarian, Irish and Scottish), but the genetic melting pot ( and telephone book ) today, survivors of the Dirty Thirties, consists of roughly equal parts Anglo and Teutonic, adapted to climatic change, and rapidly adapting new agricultural practices. Initially the German Catholics established country parishes throughout St. Joseph’s Colony, but over time, with improvements in roads and transportation these country churches were abandoned, along with homesteads, and have become shrines like the beautiful Holy Rosary Church at Reward, and St. Anthony stone church at Grosswerder. The first German Lutheran Church was erected in the town in 1914 and the first Methodist/Presbyterian ( United ) Church was erected in 1913. Because religion was such an essential part of pioneering life, and because of the diverse cultural mosaic, the small town of Luseland once boasted six churches.[8] Luseland, elevation 701 m ( 2300 ft), is situated directly beneath the apex of Palliser’s Triangle, on the southern fringe of the aspen parklands, between the arms of two ancient glacial valleys that originate in the Neutral Hills ( glacial moraines), just across the Alberta border to the west. Hearts Hill, the most prominent feature in the Luseland district, is the most eastern outlier of the moraine fields, separating the Buffalo Coulee system that drains into the South Saskatchewan River valley, from the Grass Lake system that drains eastward into Tramping Lake. Finer glacial sediments along these valleys gave rise to the rich black chernozemic soils that supported the Fescue grasslands, or prairie wool as it was called by early settlers, and, consequently, to the “buffalo highways” that led toward the Neutral Hills and the sand lands around Sounding Lake. These glacial channels were very important for the earliest aboriginal peoples and it is no accident that a major archaeological site is located just across the border in Bodo, Alberta,[9] and that many ancient artifacts and tent rings can be found around Hearts Hill and Cactus Lake. As war escalated in the 19th century between the westward expanding Cree, middlemen with the Hudson’s Bay Company, and the equine-proficient Blackfeet, the hilly moraine country became neutral territory where neither tribe ventured, and the last of the bison herds took refuge.[10] These herds, following their ancient pathways along the Fescue-flanked valleys and long alkali marshes, were eventually pursued by the Métis “hivernants” who based their winter operations out of Round Plain, south of present-day Saskatoon.[11] Situated as it is, directly beneath the apex of Palliser’s Triangle, the region was once dominated by short-grass ( Spear Grass and Blue Grama) on lighter soils and Fescue grass on the heavier clay soils along glacial river valleys ( Grass Lake and Buffalo Coulee) that drained southeast from the moraine fields ( Neutral Hills). Luseland is situated on the southern slope of a low ridge that separates the two main glacial channels, and looks out over the flat basin containing Shallow Lake, a large alkali pan, surrounded by the sandier soils of the R.M. of Progress Community Pasture, that contain the most extensive area of native short-grass prairie in the area. The last of the bison were killed off in the region by 1883, and, along with the elimination of prairie fires that regularly swept through the region, the vegetation began to change. When the first settlers arrived in 1905, the area was “bald” prairie littered with bison bones. Willows immediately began springing up around the numerous potholes, and aspens followed, such that the Luseland now marks the southern fringe of the Aspen Parkland Belt.[12] Because of their underlying richness and organic content of 7 – 8 percent, the Fescue grasslands ( or prairie wool as it was called ) were quickly broken, leaving only small fragments today. Prior to settlement, the ecosystem was shaped by periods of drought, frequent fires and intense but sporadic grazing by large herds of bison which tended to follow the richer Fescue pastures along the valleys, and find water and mineral salts in the long marshes in the valley bottoms. Antelope were the only other abundant grazer. The Buffalo Wolf was the top predator, and its dens were often located in the sandier soils and steep coulees associated with Wolf or Silver Willow ( known as mahihkanahtik or Wolf Shrub in the Cree language). Coyotes were abundant and formed part of the scavenger guild. The small Swift Fox found shelter and avoided the larger predators by living in burrows. In the 2021 Census of Population conducted by Statistics Canada, Luseland had a population of 559 living in 274 of its 311 total private dwellings, a change of -10.3% from its 2016 population of 623. With a land area of 1.59 km2 (0.61 sq mi), it had a population density of 351.6/km2 (910.6/sq mi) in 2021.[13] Luseland has many amenities. These include a swimming pool, skating rink, library, large historical museum, two parks, and a movie theatre. Luseland School is a Kindergarten to Grade 12 school with an enrollment of approximately 190 students.[18] A full range of courses are available, as well as many extra-curricular programs. Prairie Park is located in the middle of town, occupying the site which was once the schoolyard of Luseland’s first brick schoolhouse. It now is a natural prairie environment, with the natural grasses, flowers and terrain found in the area before it was settled. Source: https://en.wikipedia.org/wiki/Luseland

Luseland Saskatchewan Homes MLS®

Welcome to our Luseland Saskatchewan Homes MLS® Search page, where you can explore a diverse selection of Homes MLS® listings.

www.FarmForSale.ca is produced by Steve LeBlanc, an experienced Farm and Commercial Realtor®, The search pre-set includes Homes listings within a 50 km radius of Luseland Saskatchewan, each listing provides detailed insights into the Luseland Saskatchewan area.

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 Luseland Saskatchewan area real estate market, community highlights, and essential amenities, helping you understand each property’s unique characteristics.

Steve LeBlanc’s years of experience in Farm and Commercial real estate ensure you receive knowledgeable and personalized assistance throughout your buying or selling journey.

Welcome to www.FarmForSale.ca

Steve LeBlanc

Farm | Ranch | Land | Commercial
Alberta & Saskatchewan

Licensed Realtor® | Associate
Marcel LeBlanc Real Estate Inc.

Contact
Phone: 403-391-6447
Email: steve@leblancrealty.ca
Website: www.FarmForSale.ca

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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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