The Niagara Escarpment is a notable feature of the Ontario landscape.
I have long had an interest in The Physiography of Southern Ontario, Third Edition (1984), and have recently bought my own copy, given that the copies of the book at the Toronto Public Library have missing pages and/or maps.
It’s a well written, authoritative book. This classic text reminds me that good writing begins with, and is driven by, a good understanding of the material that a person seeks to write about.
Having recently been reading about the Humber River, I was interested to read what L.J. Chapman and D.F. Putnam, authors of The Physiography of Southern Ontario (1984), have written about the Niagara Escarpment and the Humber River.
I learned (p. 167) that the Humber River actually starts at the Niagara Escarpment. I found that of much interest – to realize that a close connection exists between the escarpment and the river.
The link at the previous paragraph describes the geology of the escarpment:
- The 725 kilometre long Niagara Escarpment began to take shape over 450 million years ago as the bed of a tropical sea. During the millions of years that followed, the sediments were compressed into rock, mainly magnesium-rich limestone (dolostone) and shale. The progressive action of glaciers, water flows and the elements caused the more resilient dolostone to weather at different rates than the shale, resulting in the very dramatic land forms that we see today: sea stacks, karst formation caves, deep valleys, scenic waterfalls, rugged hills, and perhaps most remarkable, the spectacular cliffs along the Niagara Escarpment itself.
[End of excerpt]
Toronto During the French Regime, 1615-1793
Recently, I’ve also learned that Étienne Brûlé arrived at the mouth of the Humber River in 1615. This detail of history has prompted me to learn more about the river.
The King’s Mill (1793) and The Old Mill (various versions, built later)
A topic that has intrigued me is the relationship between Old Mill Toronto and the first mill that was built in York in 1793.
I was pleased to learn that a framed text at Old Mill Toronto answers the question.
The text is laid out in capital letters, an arrangement that detracts from readability. In lowercase format, however, it’s easy enough to follow:
The Old Mill
“The ruins standing here today are all that remain of a [seven-storey] flour mill built in 1848 to replace an earlier mill, both built by William Tyrell of Weston for William Gamble, Etobicoke’s first reeve. This mill suffered the fate of earlier mills and was destroyed by fire. The ruins were designated under the Ontario Heritage Act in 1983.
“The King’s Mill, Toronto’s first industrial building, was built on 1793 near this site, on order of Lieutenant Governor John Graves Simcoe, to mill lumber for the proposed Town of York. German-speaking Nicholas Miller was the millwright, assisted by Queen’s Rangers.
“The Old Mill Tea Garden Restaurant was opened in 1914 by Robert Home Smith, the developer of the Kingsway area.
“Erected by the Etobicoke Historical Board and the Etobicoke Historical Society with the assistance of the Ontario Heritage Foundation.”
[End of text]
Hurricane Hazel brought devastation to Toronto exactly 60 years ago today, on Oct. 15, 1954. The green areas on the Hertz Toronto Car Rentals map on the left – you can click on the image to enlarge the map; click again to enlarge it further – speak to the legacy of the hurricane.
Regarding the events of 60 years ago, Chapman and Putnam (1984) remark:
“The Humber was in the main path of Hurricane Hazel on October 14-15, 1954, when up to 8 inches of rain fell, most of it within 16 hours. The resulting flood caused extensive property damage and great loss of life. At Weston a row of houses built on a low terrace near the river was swept downstream, carrying some of their occupants to their deaths, an awful price to pay for having built upon land belonging to the river.”
[End of excerpt]
Toronto During the French Regime, 1615-1793 (1933)
Toronto During the French Regime, 1615-1793 (1933) was originally published in 1933. A second edition was published in 1965. The photos and maps are of interest. Click on the images below to enlarge them.