Moraine Lake, Banff National Park, Alberta, Canada

Moraine Lake is a glacially-fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta,Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of .5 square kilometres (0.19 sq mi).

The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinct shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.

The area around the lake has several walking/hiking trails which are, from time to time, restricted. This is the one most commonly taken by tourists. The Rockpile Trail along the actual moraine is approximately 300 metres long, with an elevation change of 24 metres (79 ft). The view of the lake from the top of the rockpile is one of the most photographed locations in all of Canada.^[1] That view of the mountains behind the lake in Valley of the Ten Peaks is known as the Twenty Dollar View, as Moraine Lake was featured on the reverse side of the 1969 and 1979 issues of theCanadian twenty dollar bill.

 

Along the same trailhead, the Consolation Lakes trail starts, which is approximately 3 kilometres (1.9 mi) long, with an elevation change of 90 metres (300 ft). Upon reaching Consolation Lakes hikers may continue along to the upper lake, which is not visible from the end of the lower lake. There is, however, no clearly marked trail, and can often be a scramble over large rocky areas.

Near the canoe docks of Moraine Lake Lodge there is another trailhead. This trailhead is the start of two trails, one of which branches out into four different trails - so there are in total, five trails starting at that trailhead (Moraine Lake Lakeshore Trail, Eiffel Lake, Wenkchemna Pass, Larch Valley, and Sentinel Pass). The Lake Louise & Yoho Map provides information on these trails.

 

Mountaineering routes

The Neil Colgan Hut can be reached in 8 to 12 hours climbing the Perren Route from Moraine Lake.

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The Bay of Fundy, Canada

The Bay of Fundy (French: Baie de Fundy) is a bay on the Atlantic coast of North America, on the northeast end of the Gulf of Maine between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the U.S. state ofMaine. Some sources believe the name "Fundy" is a corruption of the French word "Fendu", meaning "split", while others believe it comes from the Portuguese funda, meaning "deep". The bay was also named Baie Française (French Bay) by explorer/cartographer Samuel de Champlain during a 1604 expedition led by Pierre Dugua, Sieur de Monts which resulted in a failed settlement attempt on St. Croix Island.

The Bay of Fundy is known for having the highest tidal range in the world. Rivaled by Ungava Bay in northern Quebec, King Sound in Western Australia, Gulf of Khambhat in India, and the Severn Estuary in the UK, it has one of the highest vertical tidal ranges in the world. The Guinness Book of World Records (1975) declared that Burntcoat Head, Nova Scotia has the highest tides in the world:

“The Natural World, Greatest Tides: The greatest tides in the world occur in the Bay of Fundy.... Burntcoat Head in the Minas Basin, Nova Scotia, has the greatest mean spring range with 14.5 metres (47.5 feet) and an extreme range of 16.3 metres (53.5 feet).”

Portions of the Bay of Fundy, Shepody Bay and Minas Basin, form one of six Canadian sites in the Western Hemisphere Shorebird Reserve Network, and is classified as aHemispheric site. It is administered by the provinces of New Brunswick and Nova Scotia, and the Canadian Wildlife Service, and is managed in conjunction with Ducks UnlimitedCanada and the Nature Conservancy of Canada.

In July 2009, the Bay of Fundy was named as a finalist for the New 7 Wonders of Nature contest that ended in November 2011. It was not chosen as a wonder.

The Bay of Fundy lies in a rift valley called the Fundy Basin; as the rift began to separate from mainland North America, volcanic activity occurred, forming volcanoes and flood basalts. These flood basalts poured out over the landscape, covering much of southern Nova Scotia. Sections of the flood basalts have been eroded away, but still form a basaltic mountain range known as North Mountain. As a result, much of the basin floor is made of tholeiitic basalts giving its brown colour. The rift valley eventually failed (see aulacogen) as theMid-Atlantic Ridge continued to separate North America, Europe, and Africa.

The upper part of the bay splits into Chignecto Bay in the northeast and the Minas Basin in the east. Chignecto Bay is further subdivided into Cumberland Basin and Shepody Bay and the extreme eastern portion of Minas Basin is called Cobequid Bay. Some of these upper reaches exhibit exposed red bay muds, for which the Bay of Fundy is noted (for their appearance and biological productivity).

Cape Chignecto defines Chignecto Bay whereas Cape Split defines the Minas Channel, leading to the Minas Basin. The Minas Channel connects the Minas Basin with the main body of the bay. The channel is 5.6 kilometers across and approximately 106.7 meters deep. The tides that flow through the channel are very powerful. They are as powerful as 8000 train engines or 25 million horses.  Facing Cape Split at the entrance to the Minas Channel are the basalt cliffs ofCape d'Or.

The lower part of the bay is also home to four important sub-basins: Passamaquoddy Bayand Back Bay on the New Brunswick shore, Cobscook Bay on the Maine shore, and theAnnapolis Basin on the Nova Scotia shore.

The bay is home to several islands, the largest of which is Grand Manan Island at the boundary with the Gulf of Maine. Other important islands on the north side of the bay includeCampobello Island, Moose Island, and Deer Island in the Passamaquoddy Bay area. Brier Island and Long Island can be found on the south side of the bay while Isle Haute is in the upper bay off Cape Chignecto. Smaller islands and islets also exist in Passamaquoddy Bay, Back Bay, and Annapolis Basin. The Five Islands, in the Minas Basin, are particularly scenic.

The Bay of Fundy is also home to another interesting geologic feature, the Hopewell Rocks formation. This formation is where the “famous flower-pot rocks” are located on a short, one kilometer long portion of Shepody Bay. These rocks are shaped by the tides, the strength of the rocks, and the presence of the joints in the rocks. The rock in the cliffs the stacks are being cut from are arkosic sandstone and coarse poorly sorted conglomerates. The tides that are eroding away the cliffs are between 10.7 meters and 14.7 meters high on average.

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Top 10 Swimming Pool on the Top

1- Marina Bay Sand Building, Singapore

2- ARTS Hotel, Spain

3- UNIQUE Hotel, Brazil

4- Fasano Hotel, Brazil

5- Intercontinental Hotel, Hong Kong

6- Soho House, New York, United States

7- Thompson Hotel, Canada

8- Grand Hotel, Spain

9- Molino Stucky Hilton Hotel, Italy

10- Athen Ledra Marriott Hotel, Greece

Enjoy !!!

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CN Tower, Canada

The CN Tower is the World's Tallest Building and Free-Standing Structure and has the world's highest public observatory, although it is not considered to be a traditional building. At a height of 553.33m, it is an important telecommunications hub. It is almost twice as tall as the Eiffel Tower and more than three times the height of the Washington Monument.
Located in Toronto, Ontario, Canada at the southern end of town to the north shore of Lake Ontario, the CN Tower is easily accessible from many major streets and highways. It was erected as a communications and tourist tower.

The CN Tower consists of a main hexagonal hollow pillar of concrete containing the elevators, stairwells and power and plumbing connections. To the main pillar are attached the broadcast antenna and the two main visitors area. The main pillar has three supporting legs giving it the appearance of a camera tripod.

Some floors of the Main Level are open to the public. At 342 m is the Glass Floor and Outdoor Observation Deck. The Glass Floor consists of thermal glass units that are 64mm thick. The floor has an area of 24sq metre and can withstand a pressure of 600psi. At 346m is the Horizons Cafe and Look Out level.

There is a rotating restaurant at 351m called the 360 Restaurant. It revolves completely in 360 degrees every 72 minutes. The rotation is slow enough that you can enjoy the fantastic views of Toronto without realizing your view is changing every moment. Below the Main Level is the tower's microwave receiver shaped like a big white donut.

The Sky Pod is presently the highest observation deck in the world. From here, you can see 100-120 km away, to the city of Rochester across Lake Ontario in the US, and see the mist rising from Niagara Falls.

The CN Tower has the tallest metal staircase in the world. At the 1776th step, the staircase reaches the Main Level. The staircase is intended only for emergency use, and is not open to the public outside three times a year during the charity stair-climbing events.

At the base of the Toronto CN tower is an attraction called the Tour of the Universe. For the price of entry you can walk through a simulated space port, see a laser show and experience what it’s like to fly through space. Tour of the Universe is open daily from 10am until 10pm. The CN Tower is open 364 days a year (closed on Christmas Day). Hours of Operation are daily from 9am-10pm January-April; 8am-11pm May-December. Cost is $16 for adults.

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