Alberta travel, Top 35 Places to Visit In Alberta, Canada
Alberta is a western territory of Canada. With an expected populace of 4,067,175 starting at 2016 registration, it is Canada's fourth-most crowded territory and the most crowded of Canada's three prairie areas. Its region is around 660,000 square kilometers (250,000 sq mi). Alberta and its neighbor Saskatchewan were regions of the Northwest Territories until the point that they were set up as areas on September 1, 1905. The head has been Rachel Notley since May 2015.
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Alberta most beautifule places we're visiting lists bellow:
Banff National Park,
Lake Louise,
Bow river. Banff,
Calgary,
Jasper National Park,
Canmore,
Edmonton,
Maligne Lake,
Drumheller,
Waterton Park,
Lake Minnewanka,
Kananaskis ,
Dinosaur Provincial Park,
Elk Island National Park,
Crowsnest Pass,
Downtown Calgary,
Peter Lougheed Provincial Park,
Medicine Hat ,
Grande Prairie ,
Saskatchewan River Crossing,
Fort McMurray,
Spray Lakes Reservoir,
Cypress Hills Interprovincial Park,
Rocky Mountain House,
Cochrane ,
Bragg Creek,
Wood Buffalo National Park,
Sylvan Lake,
St. Albert,
Upper Kananaskis Lake,
Spray Valley Provincial Park,
Bow Valley Provincial Park,
Inglewood ,
Leduc,
Airdrie ,
Abraham Lake,
Pincher Creek,
Grande Cache
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Crowsnest Pass - Driving from Alberta to Sparwood, British Columbia (BC) - Highway Drive Tour
There's a bit of life around the Crowsnest Pass in Alberta, Canada.
We officially go over the border of Alberta and BC at 14:15 (see the sign to the right). By 20:27 we are about to enter Sparwood.
6:38 has probably the biggest roadkill I've seen in my life. Let's slow down for the animals...
Music by Mark Quigley (Korg Volca Keys)
Niagara Falls Travel Guide for first timers - Travel Episode 12
So you’re heading to Niagara Falls and your trying to decided what to do and which side of the falls works best for you. In this travel guide I’m going to break down both the American and Canadian side to help you make the best travel plans for you.
And now it’s time for 1 of 3 Tones Travel Tips!
Don’t forget your passport it’s the only thing that was needed as an American citizen to go across and come back. However when crossing the bridge you might want to avoid peak travel times especially on weekends and holidays as I was told the lines can be as long as 2 hours. We crossed over at 10pm and then again at 5:30 am and only waited a few minutes
Probably the most popular thing to do is the boat tour along the falls. On the Ny side it’s called the Maid of the Mist and on the Canadian side it’s called the Hornblower.
We rode the Maid of the Myst
While it looked to me that both are very similar on water the Ny side seemed to have one advantage that when you get off you can get up close and personal with the falls by walking up a pathway called the crows nest.
On the Canadian side there are casinos off in the distant. But the part We visited was called Clifton hill. And oh my they have a little something for everyone. A giant Ferris wheel, miniature golf, haunted houses, a Ripley's believe it or not, where by far they have some very strange exhibits
And oh yea A very fun go-kart track.
And now it’s time for another Tones Travel Tip!
Book all your major activities in advance as they do sell out. We tried to book the zip line on the Canadian side on a Sunday at 10:30 am and they were already booked for the day. Also pack your patience as Niagara Falls is a very popular tourist destination so there will be some long lines.
The Views
From the American side you can get some really nice views from several different vantage points. However the Canadian side you really get the full and amazing views of the falls. Plus at night with the lights is definitely a sight to see.
By far our favorite part of our Niagara Falls trip was taking the cave of the winds tour which is located on the American side. They give you a poncho and sandals to wear and it’s a good thing because you’re certainly going to need it.
There’s something so amazing standing right next to the falls. The sounds of the water falling. The smell of the water in the air. It truly is an experience worth doing.
And here’s where those ponchos and sandals came in extremely handy.
Here’s a my final Tones Travel Tip.
Even if you’ve bought a ticket in advance like we did, you still have to go over to the cave of the winds tour to book a time for that day. No reservations are taken in advance. You will also want to go early. We got to the booth around 3pm and the earliest reservation they could give that day was 7pm. This worked fine for us as it gave us time then to enjoy the park and ride the maid of the myst.
So if you’re going to Niagara Falls definitely try to get in one full day on each side. While there’s more activities to do on the Canadian side, the Cave of The Winds tour and the ability to go up the crows nest after the maid of the myst makes it a must do on the American side.
Make sure you Like and subscribe if you enjoyed this video. What are you planning to do when traveling to Niagara Falls and was there an attraction in Niagara Falls that we might have missed while we were there.
#NiagaraFalls #TravelGuide #TonedInEnt
The Frank Slide, Alberta
The Frank Slide, Alberta
A small town shown at the base of a mountain. The mountain's face stands barren following a large rockslide and a light cloud of dust is visible in the air.
The town of Frank and Turtle Mountain on April 30, 1903, one day after the slide
Date April 29, 1903
Time 4:10 AM MST
Location Frank, District of Alberta, Northwest Territories(note)
Coordinates 49°35′28″N 114°23′43″WCoordinates: 49°35′28″N 114°23′43″W
Deaths 70–90+
Website Frank Slide Interpretive Centre
The Frank Slide was a rockslide that buried part of the mining town of Frank, Northwest Territories,[nb 1] Canada at 4:10 am on April 29, 1903. Over 82 million tonnes (90 million tons) of limestone rock slid down Turtle Mountain within 100 seconds, obliterating the eastern edge of Frank, the Canadian Pacific Railway line and the coal mine. It was one of the largest landslides in Canadian history and remains the deadliest, as between 70 and 90 of the town's residents were killed, most of whom remain buried in the rubble. Multiple factors led to the slide: Turtle Mountain's formation left it in a constant state of instability. Coal mining operations may have weakened the mountain's internal structure, as did a wet winter and cold snap on the night of the disaster.
The railway was repaired within three weeks and the mine was quickly reopened. The section of town closest to the mountain was relocated in 1911 amid fears that another slide was possible. The town's population nearly doubled its pre-slide population by 1906, but dwindled after the mine closed permanently in 1917. The community is now part of the Municipality of Crowsnest Pass in the Province of Alberta and has a population around 200. The site of the disaster, which remains nearly unchanged since the slide, is now a popular tourist destination. It has been designated a Provincial Historic Site of Alberta and is home to an interpretive centre that receives over 100,000 visitors annually.
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Please watch: Motorcycle Madness 2019
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BC Hwy 3: Cranbrook - Fernie BC (Time Lapse)
Highway 3 follows the southern-most pass through the Canadian Rockies (Crowsnest Pass). In this video, we travel the 96 km between Cranbrook and Fernie, British Columbia. The last 1/3 of the video is the most impressive as we have to make our way through a narrow pass just before Fernie. I recorded the Crowsnest Pass in a separate video, so look for that at a later date!
Best places to visit
Best places to visit - Lethbridge (Canada) Best places to visit - Slideshows from all over the world - City trips, nature pictures, etc.
Hope Slide Jan 9,1965 || Aerial views || Beautiful British Columbia
The landslide was caused by the presence of pre-existing tectonic structures (faults and shear zones) within the southwestern slope of Johnson Ridge.[17] The lower parts of the slide scar are underlain by felsite sheets (which may have failed first) while the upper parts of the slide scar are underlain by highly jointed Paleozoic greenstone beds.[18] Ongoing weathering and tectonic activity weakened the slide mass to the point where it had reached limiting equilibrium. Johnson Peak was the site of a previous smaller prehistoric rock-slide.[19]
Just what triggered the 1965 landslide remains unclear; the two so-called earthquakes were likely too small to trigger the slide[20] and thus the seismic events were more likely caused by the impact of the landslide masses on the opposite valley wall. Changes in groundwater condition, often a trigger for landslides, is not thought to have played a role in the Hope Slide as the slide occurred during a protracted period of sub-zero temperatures in the winter, though some have suggested that freezing of seepage exit points may have caused an increase in water pressure at the toe of the slide.[21]
The highway has since been rerouted around and over the base of the slide's debris field 55 metres above the original ground level on the other side of valley. Most of the massive scar on the mountain face remains bare rock, without significant growth of trees or other large vegetation. It is quite easily visible from aircraft passing overhead.
A view point on Highway 3 allows tourists to view the scar.
A four kilometre stretch of the prior routing lays disused to the north of the new highway alignment.
Prior avalanche[edit]
Prior to the landslide, a small avalanche had forced five people to stop a few miles southeast of the town of Hope, British Columbia—150 kilometres (93 mi) east of Vancouver—on a stretch of the Hope-Princeton Highway below Johnson Peak.[5]
Landslide[edit]
Two earthquakes were said to have been recorded in the general area of the slide.[6] One quake occurred at 3:56 am and the second at 6:58 am. The slide that obliterated the mountain's southwestern slope was discovered when members of the RCMP detachment at Hope BC were dispatched to what were first reported as a couple of small rock slides. The first news reports of the slide were from CHWK Radio in Chilliwack where morning news reporter Gerry Pash and later news director Edgar Wilson filed voice reports with Broadcast News and Canadian Press.
The slide completely displaced the water and mud in Outram Lake[7] below with incredible force, throwing it against the opposite side of the valley, wiping all vegetation and trees down to the bare rock, then splashed back up the original, now bare, slope before settling. Recent research[8] shows that these impacts against the opposite valley sides produced the seismic signatures interpreted as earthquakes.
The slide buried a 1957 yellow Chevy convertible[9] that had become stuck in the first slide, an Arrow Transfer oil tanker truck, and a loaded hay truck that had stopped behind the tanker[10] under a torrent of 47 million cubic metres of pulverized rock, mud, and debris 152.4 metres (500 ft) deep and 2 kilometres (1.2 mi) wide, which came down the 1,220-metre (4,000 ft) mountainside.[11]
Norman Stephanishin, the Arrow truck driver, had stopped behind the stuck convertible. Stephanishin, unable to turn his rig around on the narrow and icy road, tried to talk the four others into walking the five kilometres back to Sumallo Lodge. Unable to convince them, Stephanishin walked east to Sumallo Lodge to phone the Highways Dept.[12] In a short distance, Stephanishin flagged down a Greyhound Lines bus traveling to Vancouver[13] and persuaded the driver, David Hughes, to return with him to Sumallo Lodge. Hughes turned back and is credited with saving his passengers from a tragedy.[14]
Rescue workers from Hope and Princeton found the body of Thomas Starchuck, 39, of Aldergrove BC, driver of the hay truck. The body of Bernie Lloyd Beck, 27, of Penticton BC, driver of the convertible was also retrieved. Beck's passengers, Dennis George Arlitt, 23, of Penticton BC, and Mary Kalmakoff, 21, of Shoreacres BC, were never recovered. Their bodies remain entombed under the rock.[15]
British Columbia Highways Minister Phil Gaglardi attended the scene and directed the construction of a temporary tote road over the southern portion of the slide. In twenty-one days a bumpy route had been established over the slide.[16]
Copied over from Wikipedia
Time Lapse: 4,500km From Toronto to Vancouver in 30 minutes
This motion timelapse (or hyperlapse) is shot with two GoPro cameras while driving 7 days through Canada from Toronto to Vancouver. Every 10 seconds we did 1 shot and once every 2 seconds while passing Banff and Yoho National Parks.
50,000 still images (100GB) were then joined in half an hour video.
Key moments and processing described here
Photos and stories from the trip can be found here:
Music: Hans Zimmer
Alberta's Kananaskis Country: Highway 40 Drivelapse Dashcam
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This drive takes you in and out of Kananaskis Country, on the Kananaskis Trail, Highway 40, east of Banff, Alberta. It begins and ends at Trans Canada 1, and the u-turn happens somewhere near Mt. Kidd.
Music used with written permission:
Artist: Lee Fraged
Tracks may include:
Skunk Ghost (tup007)
Bless The Sinners (original fix) (tup007)
Bring Your Own Booze (Art035)
Helix (TDN009)
You can find information on my rights to use this music here:
Lethbridge Alberta to Coaldale Town. Driving Tour of Highway in Canada. Countryside.
We are driving from southern Alberta's largest city Lethbridge to Coaldale, a town that seems to have everything (according to its website).
Music by Free Jazz Vancouver (Mark Quigley & Michael Quigley).