Highway 9
Highway 9
Between Mildmay and Walkerton, Ontario
randy SUTHERLAND : GUELPH ontario CANADA
Looking off Dundas Peak into the valley I think of how this rock I'm standing on was the bottom of a tropical sea, south of the equator, filling with coral 450 million years ago. You can see fossils of sea life and then wonder at how the matter which existed on the earth 6 or so billion years ago had evolved into this. Sometimes it's amazing how long the earth was so similar, sometimes amazing how quickly some things evolve and change. If we want to be sure that in 450 million years from now that we'll be more than bone fossils in rock we'll have to smarten up and not kill ourselves.
Dundas, Ontario
"Numerous areas in Nova Scotia are underlain by Carboniferous strata. These strata are the province's source of coal, oil shale, salt, limestone, dolomite, celestite, barite, gypsum and anhydrite.
The Windsor Group consists of marine sediments. These include sandstone, shale, conglomerate, limestone, dolomite, gypsum, anhydrite and salt. Above the basal limestone, most of the limestones are very fossiliferous. It is within the Windsor Group that the majority of industrial minerals are mined. Total thickness of the Windsor Group varies from 1,000 feet to 10,000 feet."
- Geology Minerals and Mining in Nova Scotia
August 2006, near Walton, Nova Scotia
A 45 turbine wind farm just north of Shelburne on the Dundalk Plateau is a wonderful site to see - but some people are still blowing against the wind.
near Shelburne, Ontario
On our way out to catch the impressive view of the Hamilton/Dundas valley from Dundas Peak we stopped to watch the flow over Tew's Falls - over 400 meters down - almost as tall as Niagara. But without the crowds and casinos. It's perfect hiking weather now - not too hot and no bugs.
Tew's Falls, Dundas, Ontario
The Mad River is peaceful right now - the slow flow in the mill pond above Glen Huron reflects the turning of the season. Nice hike along the escarpment where the Ganaraska Trail meets up with the Bruce Trail.
Mad River, Glen Huron, Ontario
Rocks and pristine white sand line the shore at St Catherine's Beach. Seals sun on the rocks.
August 2006, Nova Scotia
The Grand River still flows through a preglacial spillway over limestone formed 400 million years ago from coral reefs when this area was just below the equator in the southern hemisphere. Now when the river flow is low you can see how the bed has been smoothed by years of water passing over.
Elora Gorge
These layers of sedimentary rock used to be horizontal but have been twisted into many interesting angles. Very interesting geology in Nova Scotia.
Rainy Cove, Nova Scotia