About this waterfall.

About Rosamond Rapids

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This site used to be called 'Arklan Rapids' in earlier versions of this web site. The Arklan Rapids are actually found further downstream, and may be visible from Anthony Cumo Park. Rosamond Rapids is a long, gently sloped rock rapids on the Mississippi River in the east end of Carleton Place.

This is not much of a waterfall, and you shouldn't go out of your way to see it. But the rapids, while very low, are attractive. From the one lane bridge that carries Gillies St, you can see the rapids upstream and downstream. The edge of the river is lined with low sedimentary rock outcrops on the downstream side.

There are several old stone mills in the vicinity, including one on the left side of the river, right beside the rapids. Other historic buildings are to be found in the town, and it is worth a quick tour to see the industrial heritage.

Previously, you could walk downstream from the bridge on the right side of the river. In the late 2010s, this trail was blocked when development of this property began; the site will house condos that overlook the river.

As this site is undergoing development and construction, the parking situation may be in flux. The directions on this site lead to a small gravel area just west of the bridge.

Some Key Facts
Region Eastern
County Lanark
Near Carleton Place
Watercourse Mississippi River
Watershed / % Lakes 3 / 21%
Ownership Roadside only
Landscape Urban
Size Very Small
Type Rock Rapids
Modification Bridge, old mill
Access Easy
Top / Bottom Easy to view / Easy to view
Trail conditions Paved
Hiking Time 2 min
Coordinates 45.1435,-76.1428
Parking
45.1435,-76.1428
Site ID WOO.LAN.011
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Finding Rosamond Rapids

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Visiting Rosamond Rapids


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Waterfalls of Ontario Project

This project has been online since 1999, in print since 2003, and on social since 2011. (See archives: 2003, 2012, 2018). It was the first to inventory and map Ontario's waterfalls for recreational purposes. With your continued help, it grows. Learn more...
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This page last updated on April 20, 2024. Earlier versions can be examined on Archive.org, dating back to 2003.