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How did the Niagara Whirlpool form?
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questions).
The Niagara Whirlpool
formed nearly 4,200 years ago when the erosion and
recession of Niagara
Falls, which up to this point was a sluggish process, reached
a soft spot in the landscape. Saint David's Buried Gorge was an
ancient, pre-glacial river valley filled in with soft glacial silt and
stone. When Niagara Falls eroded its way into this hidden gorge, it
rapidly began washing away the gorge's soft filling. It is speculated
that when the Falls hit the buried gorge, it was just a matter of weeks,
perhaps even days of violent erosion while it carved out the Whirlpool
basin. It was a swift and powerful geological event considering the
Falls had taken nearly 8000 years to get to this point.
Saint David's Buried Gorge ran
perpendicular to the current path of the Fall's erosion, and
resulted in a 90 degree turn in the river. Just upstream the
narrow Niagara Gorge at the
Whirlpool rapids sends water jetting
into the Whirlpool basin. It hits the solid rock basin across
the Whirlpool at Niagara Glen. Thousand of years of these forces
has resulted in a dimpling of the basin; giving it an oval shape
that juts past the turn in the river.
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In what direction does the Niagara
Whirlpool flow?
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questions).
When the Niagara River is
at full flow the Whirlpool will flow in a counterclockwise direction.
When the river flow drops, usually when more flow is diverted to the
power plants, the flow of the whirlpool reverses (clockwise). This
usually happens during the tourist off-season (November 1 through April
1).
Just upstream from the Whirlpool is the
narrowest section of the Niagara: the Eddy Basin. This pinch in
the gorge is not sufficient for the normal flow of the river to
pass through, so some of the water is pushed backward. The water
at the shore actually flows backward at this location.
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How deep is the water at the Niagara Whirlpool?
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questions).
The Niagara River reaches
depths of 125 ft (38 m) as it passes through the Niagara Whirlpool.
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What class of rapids is the Niagara River?
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questions).
Different sections of the Niagara River
are classified differently. First let's review what the classes stand
for. Whitewater rapids are graded on the International Scale of
River Difficulty, which has 6 "Classes."
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Class I: Easy.
Waves small; passages clear; no serious obstacles.
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Class II: Medium.
Rapids of moderate difficulty with passages clear.
Requires experience plus suitable outfit and boat.
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Class III:
Difficult.
Waves numerous, high, irregular; rocks; eddies; rapids
with narrow passages , requiring expertise in
maneuvering; scouting usually needed. Requires good
operator and boat.
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Class IV: Very
difficult. Long rapids; waves high, irregular;
dangerous rocks; boiling eddies; best passages difficult
to scout; scouting mandatory first time; powerful and
precise maneuvering required. Demands expert boatman and
excellent boat and good quality equipment.
-
Class V:
Extremely Difficult. Exceedingly difficult,
long and violent rapids, following each other almost
without interruption; riverbed extremely obstructed; big
drops; violent current; very steep gradient; close study
essential but often difficult. Requires best person,
boat, and outfit suited to the situation. All possible
precautions must be taken.
-
Class VI:
Unrunnable. Chances are: you're going to die on
this.
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Most of the Niagara River's waters are
graded as Class I. This includes the run
from Lake Erie up to the Cascade Rapids just above the falls. Here the
water's classification is up for debate. Although the whitewater is runnable (probably a
Class IV), that would mean ending up over the falls at the end. The Falls themselves
and the immediate area below are certainly a Class VI: unrunnable.
he navigable portions of the Upper Great Gorge
(below the Falls, where the Maid of the Mist boats run) are
roughly a Class IV. Although the water here
lacks free-standing waves and obvious obstacles, the whirlpool
currents can trap small craft and push them towards the rocky
cliff or into the downpour of the falls. In addition, high
quantities of bubbles rising from below can cause buoyancy
problems for personal craft.
Heading downriver from the basin of the Falls,
the gorge remains wide and the water calms, eventually
decreasing to a Class I. At the Whirlpool Rapids Bridge
the gorge suddenly narrows by more than half and water speeds up
to approximately 22 mph (35 kmph) forming the world famous
Whirlpool Rapids. Here the large volume of the Niagara is forced
through a basin unable to fully support its bulk, forming
violent currents and standing waves reaching 15 ft high. The
rapids shoot out of the narrow gorge and into the swirling
Niagara Whirlpool. Here craft would need to fight the powerful
current to navigate the 90 degree bend in the river, in order to
escape the rapids. The Whirlpool Rapids run is easily a
Class V and at times of higher flow, unrunnable.
Just past the Whirlpool, the gorge widens and the river slows for a short bit, until it reaches Devil's
Hole at the Lower Great Gorge. Again, a constriction of the
gorge basin speeds up and agitates the Niagara; forming the
Lower Whirlpool Rapids. Not nearly as violent as upriver, the water here
reaches a Class III.
After Devils Hole, the river calms and it is
smooth sailing all the way north to Lake Ontario.
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What is Devil's Hole?
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questions).
The Devil's Hole is the name given to a small ravine cut into the
American side of the Niagara Gorge by an ancient post-glacial tributary,
Bloody Run. The tributary is now virtually developed away, but 12,000 or so years ago is was a much larger torrent into
the Niagara Glen. During the events outlined below it was a seasonal
creek.
The Hole and stream got their modern names from the
Devil's Hole Massacre that occurred her on September 14
1763, during the French and Indian War. A force of 300 to 500 Seneca
warriors ambushed a British supply (led by Porter Master John Stedman)
convoy and drove them, their wagon, supplies and horses off the cliff
here. 102 members of the convoy died, including several civilians. Only
a few people escaped, including one drummer boy and John Stedman. When
reinforcements arrived they found only 80 bodies in the ravine, and the
creek was flowing red with blood.
There is a limestone cave at Devil's Hole, which is commonly thought to
be the "Devil's Hole" itself. It's not. Devil's Hole is the ravine, the
State Park is the 42 acres surrounding it, and the cave is often
referred to as the Cave of Evil Spirits.
See our page on Devil's
Hole State Park for more information.
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Where are the Niagara River Gorge
walls the tallest?
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questions).
The Niagara River Gorge's massive cliffs
reach maximum height at the
escarpment itself near Queenston, ON. Here
the Gorge walls are nearly 322 ft (98 m) high. The height of cliffs
decline as you move further south, eventually reaching their lowest
height at Niagara Falls.
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