| Thirty Mile Creek Falls | TorontoHiking Ontario Waterfalls |
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Thirty Mile Creek Falls (Rating=B) is a ribbon cascade falls that runs 15 m down a 25 m slope into the deep gorge below and is about 2.5 m wide at the crest.
THIRTY MILE CREEK FALLS AREA WALKING TRAILS:Bruce Trail. For a map of area trails, click on the Trail Map icon above. From the roadside parking area on Ridge Road E, continue to the road intersection ahead and turn right walking downhill on Thirty Road. On your left part way down you will see a Bruce Trail sign and a log across the start of the trail. Past this log, head down into a wet marshy area and follow the path to a bridge across Thirty Mile Creek. The cascading waterfall is at your feet. From this vantage point it seems to be one small falls. Look behind you and up the hill to see a second waterfall. By crossing the bridge and walking along the gorge on the other side you can see that it is a series of cascading waterfalls all the way to the bottom of a very deep gorge. Both sides of the gorge provide good views. In dry periods you will see only a gully of rocks devoid of water. Spring is the best time to view all of these waterfalls. Across the gorge you will see several caves lining the gorge wall that may have been used for shelter by early explorers to the area. Some of these caprock overhangs extend 3 to 4 m out from the wall. Several trees exhibit octopus like roots that wrap around rocks gripping as if out of fear of falling into the gorge. Continue along the gorge edge until you come to a small wooden bridge over a creek. There is not much point in going further so return back to the road and your parking spot. FOR THE ADVENTUROUS ONLY:The gorge walls are very steep on both sides. Standing on top of the path over the creek, the path to the right side soon ends and the vegetation growth becomes quite thick. On the other side, the Bruce Trail continues along the gorge edge and gradually descends. The trail then turns sharply left and heads uphill. At this point the slope to the right has become quite gradual and descent is possible here into the gorge where you would have to make your way back upstream over a rocky bed. HIKES VISITING THIS FALLS:L49F Mountainview CA to Beamer's Falls Waterfall Comments
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Thirty Mile Creek Falls


11,000 years ago, this spot was the shoreline of glacial Lake Iroquois, which created the shore bluff in the escarpment caprock just to the south. The step effect in the waterfall is cause by alternating layers of hard and soft rock that make up the Niagara Escarpment. The uppermost layer is hard dolostone. Below this are the alternating softer layers of shale and sandstone. The sandstone is more resistant to erosion than the shale, leading to the appearance that the creek flows over a series of steps.
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