The Best Attractions In Saint-Louis-de-Kent

Quebec City, Quebec, Canada, North America

Quebec, also Québec, City of Québec, Quebec City, or Québec City, is the capital of the Canadian province of Quebec. In 2011 the city had a population of 516,622, and the metropolitan area had a population of 765,706, making it the second most populous city in Quebec after Montreal, which is about 233 km (145 mi) to the southwest. The narrowing of the Saint Lawrence River proximate to the city's promontory, Cap-Diamant (Cape Diamond), and Lévis, on the opposite bank, provided the name given to the city, Kébec, an Algonquin word meaning where the river narrows. Founded in 1608 by Samuel de Champlain, Quebec City is one of the oldest cities in North America. The ramparts surrounding Old Quebec (Vieux-Québec) are the only fortified city walls remaining in the Americas north of Mexico, and were declared a World Heritage Site by UNESCO in 1985 as the 'Historic District of Old Québec'. According to the federal and provincial governments, Québec is the city's official name in both French and English, although Quebec City (or its French equivalent, Ville de Québec) is commonly used, particularly to distinguish the city from the province. The city's famous landmarks include the Château Frontenac, a hotel which dominates the skyline, and La Citadelle, an intact fortress that forms the centre-piece of the ramparts surrounding the old city. The National Assembly of Quebec (provincial legislature), the Musée national des beaux-arts du Québec (National Museum of Fine Arts of Quebec), and the Musée de la civilisation (Museum of Civilization) are found within or near Vieux-Québec. Quebec City is known for its Winter Carnival, its summer music festival and for its Saint-Jean-Baptiste Day celebrations. Tourist attractions located near Quebec City include Montmorency Falls, the Basilica of Sainte-Anne-de-Beaupré, the Mont-Sainte-Anne ski resort, and the Ice Hotel. Jardin zoologique du Québec, reopened in 2002 after two years of restorations but closed in 2006 after a political decision. It featured 750 specimens of 300 different species of animals. The zoo specialized in winged fauna and garden themes, but also presented several species of mammals. While it emphasized the indigenous fauna of Quebec, one of its principal attractions was the Indo-Australian greenhouse, featuring fauna and flora from these areas. Parc Aquarium du Québec, reopened in 2002 on a site overlooking the Saint Lawrence River, presents more than 10,000 specimens of mammals, reptiles, fish and other aquatic fauna of North America and the Arctic. Polar bears and various species of seals of the Arctic sector and the Large Ocean, a large basin offering visitors a view from underneath, form part of the principal attractions. There are a number of historic sites, art galleries and museums in Quebec City, such as Citadelle of Quebec, Musée national des beaux-arts du Québec, Ursulines of Quebec, and Musée de la civilisation. Throughout its over 400 years of existence, Quebec City has served as a capital. From 1608 to 1627 and 1632 to 1763, it was capital of French Canada and all of New France; from 1763 to 1791, it was the capital of the Province of Quebec; from 1791 to 1841, it was the capital of Lower Canada; from 1852 to 1856 and from 1859 to 1866, it was capital of the Province of Canada; and since 1867, it has been capital of the Province of Quebec. The administrative region in which Quebec City is situated is officially referred to as Capitale-Nationale, and the term national capital is used to refer to Quebec City itself at provincial level. Quebec City is located in the Saint Lawrence River valley, on the north bank of the Saint Lawrence River near its meeting with the St. Charles River. The region is low-lying and flat. The river valley has rich, arable soil, which makes this region the most fertile in the province. The Laurentian Mountains lie to the north of the city. Upper Town lies on the top of Cap-Diamant (Cape Diamond) promontory. A high stone wall surrounds this portion of the city. The Plains of Abraham are located near the edge of the promontory. Lower Town is located at shore level, below Cap-Diamant. Much of the city's most notable architecture is located east of the fortification walls in Vieux-Québec (Old Quebec) and Place Royale. This area has a distinct European feel with its stone buildings and winding streets lined with shops and restaurants. Porte St-Louis and Porte St-Jean are the main gates through the walls from the modern section of downtown; the Kent Gate was a gift to the province from Queen Victoria and the foundation stone was laid by the Queen's daughter, Princess Louise, Marchioness of Lorne, on 11 June 1879. West of the walls are the Parliament Hill district and the Plains of Abraham.

#ExploreNB - Pabineau Falls Bathurst

Pabineau Falls in Bathurst New Brunswick. These are worth the visit especially when it's the Salmon run up the river.
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What to do in New-Brunswick?
Quoi faire au Nouveau-Brunswick?
#ExploreNB

Pabineau Falls is a settlement in New Brunswick. It is the administrative office of the Pabineau Mi'kmaq First Nation band government. The Pow Wow is held at the Flying Eagle Memorial Pow-wow Grounds the first weekend of July (Saturday and Sunday). It is located on the Nepisiguit River, upriver from Bathurst.

Autumn Day by Kevin MacLeod is licensed under a Creative Commons Attribution licence (
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Equipment and software used.
Drone: yuneec Q5004k
software : windows live movie maker and Wondershare ( Filmora )

Seafood Boil Bag

Uncle John's Cafe in LA gives you a giant bag full of seafood.

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Urlaub USA: Road Trips Maryland, DC

Urlaub an der Chesapeake Bay: Insider-Tipps fuer einen unvergesslichen Road Trip im US-Bundesstaat Maryland.

Shaw's Garden St Louis MO

Paseo al jardin botanico en St Louis, oct 2008

Drapeaux régionaux du Canada 2017: provinces et territorires

Drapeaux des provinces et territoires du Canada avec des informations générales.

Web: mapasybanderas.com

Walking in San Luis Obispo

Walking along and someone turns down the wrong way on a one way street.

Constant sorrow in New-Brunswick.

On TCH in St-Leonard, NB

What the Niagara River looks like 2 days before an Ice Bridge forms

Here is a how the Niagara River looked, as seen on Jan.9, 2015, prior to the formation of the Ice Bridge. Last night, ice shelves began forming along the Canadian and US banks. The Niagara River is now pushing ice flow through the center.
(Note: The Ice Bridge DID form, just two days later, on Jan.11, 2015 - see video:
The 9 min. time-lapse video seen here, actually took place over an almost two-hour period.
Along the riverbanks there is a reverse-current which flows upriver, now carrying ice upstream. This is a slower current of continuing, drawn-out eddies, and the ice it's carrying is pushed back towards the shore by the faster, center flowing current.
This slower ice is eventually pressed against the shore, and then upon itself, where it compounds and layers into a solid non-moving mass - this is how those ice shelves slowly develop.
Overtime (in this case, the growth occurred quite quickly: since just yesterday) the shelves begin to extend further out into the river, narrowing the center passage.
In a continuous process, large slices of a shelf will peel away into the center flow, be spun around, get broken up, and then get re-attached to the shelf somewhere farther downstream. Eventually the river center becomes so constricted by the two ice shelves growing from each bank, that much of the new ice, which relentlessly keeps flowing from upstream, is then forced to go underneath the ice shelves.
This process causes the ice shelves to solidify even more and thicken from the bottom. Eventually, large slices of thickened ice will break off the leading edge of the shelves, get pushed and spun into the shrinking center flow, get wedged in with other chunks of ice between the two-non-moving shelves, and slow down the surface river flow to a point when it completely jams up.
This is when the actual Ice Bridge forms, when the center band stops moving due to the surface blockage, thereby making a solid connection of non-moving ice, from bank-to-bank.
Further ice solidification occurs when the river - still flowing and still carrying new ice - begins to be pulled entirely underneath the jammed ice cap. This adds still more thickness to the ice cap from underneath, thereby pushing the ice higher.
This process creates a solid Ice Bridge, which can stretch for two miles along the Niagara River, as happened last year in the brutally-cold month of Jan.2014 - see videos:

and

(Another two-mile-long Niagara River Ice Bridge also formed in the brutally-cold months of Jan. and Feb. 2015, see:

and