Kirkness House: Two Edmonton Pioneers

Thank you to Melanie Moore (Board Member of the Highlands Historical Society in Edmonton) for sharing this important piece of history. 

There is an old house in the Virginia Park neighbourhood of Edmonton, on 73rd Street and Ada Boulevard. Now empty, it has seen better years. The shingles are coming off, the paint old and faded, the yard overgrown. When asked about the house, neighbours knew little of its story.

Kirkness House, Edmonton, 2018 (photograph by Melanie Moore).

Having recently explored the history of my own 100 year old home in Edmonton, I decided to find out more. James Kirkness, and his wife Sarah Steinhauer, built the house in 1909. Prior to that, he and Sarah lived in an adjacent log cabin where they raised their children. The City of Edmonton Archives has a painted-over photograph of James in front of the 1870s log cabin with the new 1909 house behind. Likely James had the painting commissioned, put it in an ornate frame, and hung it proudly in his new home. Read more

Plough your Furrows Deep: The Foundations of Agriculture in Alberta

Farming in Alberta has been shaped by a deep and layered history of geological, biological, and human forces. This article takes us back to the beginning.

Farming is based on a sliver of soil that caps kilometers of sediment and bedrock. To understand how our fields first formed, we need to read an ancient geological story of how Alberta has been raised and tilted then scoured and capped over time. Alberta has sat inside a continental plate (or ‘craton’) for over 300 million years. Around 180 million years ago, the western edge of this plate began crunching to form the up-and-down terrain of the Coast Mountains of British Columbia (B.C.) and the Rocky Mountains between B.C. and Alberta (Figure 1). Mountain building finished about 50 million years ago.

Bedrock geology draft 4
Figure 1. This is a bedrock map of Alberta and B.C. “Bedrock” refers to the stony basement below our modern soil and loose sediment (gravel, sand, and silt). B.C. is striped with colour because its bedrock is made of diverse chunks of land called terranes that got repeatedly mashed against a moving continental plate that Alberta lay within. One product of this mash-up (‘accretion’) was mountain building (‘orogeny’). Creation of the western mountains forever shaped the development of soils and agriculture in the Prairie Provinces (map by Todd Kristensen with bedrock data from the USGS 2015).

For almost 200 million years, Alberta has been tilted: our bedrock is formed largely of shales and sandstones that built up when sediment either poured off the mountains and solidified into rock or settled down in ancient waters that once filled a basin over Alberta. From about 50 to 5 million years ago, huge sheets of gravel and sand continued to shed off the Rockies (carried by rivers and streams) before settling into our basement. Read more

Building skills: Using seeds and shells to learn about Alberta’s ancient environments

How do we know about past environments?

Historic and precontact archaeological and palaeoenvironmental sites from across Alberta tell us much about people and past environments. But how can we learn the details about that environment? This blog post will tell you how we use environmental indicators, especially macrofossils, to reconstruct what conditions were like at sites in the past.

It may seem reasonable to assume that the environment when an archaeological site was inhabited by people was generally the same as it is now, and this is sometimes the case. However, the archaeological record in Alberta goes back at least 13,000 years , to the end of the last major glaciation and its transition to our present epoch (the Holocene). Given this long and varied history, it’s obvious some considerable changes have occurred. Read more

Alberta’s Wooden Country Grain Elevators – Update

This post was originally published on RETROactive on March 6th, 2012 and again on August 26, 2015. Interest in grain elevators remains strong, so a revisit seems in order. Some additional data has been added, an updated list of communities with elevators can be accessed below, as well as a variety of resources and documents relating to Alberta’s Grain elevators.

The twentieth century saw the rise and fall—literally—of the wooden country grain elevator in Alberta. As rail lines spread across the province in the early 1900s, grain elevators sprouted like mushrooms after a spring rain. The height of wooden country grain elevators was reached in 1934. New ones continued to be added until the 1990s, but with increasing numbers being demolished, these icons of the prairie became scarcer. Today, the remaining wooden country grain elevators number only about six percent of the maximum reached in the 1930s. Check out the following “index” of Alberta’s wooden country grain elevators, called “elevators” for short in this article.

Number of elevators in Alberta: Read more