Banff National Park

© RicardMN Photography

© RicardMN Photography

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© RicardMN Photography

© RicardMN Photography

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Banff National Park is Canada’s oldest national park, established in 1885 in the Rocky Mountains.

The park, located 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast.

Over the past few million years, glaciers have at times covered most of the park, but today are found only on the mountain slopes though they include the Columbia Icefield, the largest uninterrupted glacial mass in the Rockies. Erosion from water and ice have carved the mountains into their current shapes.

Johnston Creek is a tributary of the Bow River in Canada’s Rocky Mountains. The creek is located in Banff National Park.

Johnston Creek originates north of Castle Mountain in a glacial valley southwest of Badger Pass and south of Pulsatilla Pass, at an elevation of 2,500 meters (8,200 ft). The creek flows southeast between Helena Ridge and the Sawback Range, and then south through a gorge known as Johnston Canyon. The stream empties into the Bow River, south of Castle Mountain, between Banff and Lake Louise, at an elevation of 1,440 meters (4,720 ft).

As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.

A popular hiking trail follows the canyon and leads to a meadow within the Johnston Valley above the canyon. The first part of the trail consists of a constructed walkway with safety rails and bridges, while the last part of the trail is natural and more rugged. Within the meadow are the Ink Pots, which are six blue-green spring-fed pools.

Ice climbing is a popular activity on the frozen waterfalls in winter. (Description from Wikipedia).

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Bridalveil Fall in Yosemite Valley

© RicardMN Photography

© RicardMN Photography

Bridalveil Fall is one of the most prominent waterfalls in the Yosemite Valley in California, seen yearly by millions of visitors to Yosemite National Park. The waterfall is 188 metres (617 ft) in height and flows year round.

The Ahwahneechee tribe believed that Bridalveil Fall was home to a vengeful spirit named Pohono which guarded the entrance to the valley, and that those leaving the valley must not look directly into the waterfall lest they be cursed. They also believed that inhaling the mist of Bridalveil Fall would improve one’s chances of marriage.

Yosemite National Park is a United States National Park spanning eastern portions of Tuolumne, Mariposa and Madera counties in the central eastern portion of the U.S. state of California. Yosemite is one of the largest and least fragmented habitat blocks in the Sierra Nevada, and the park supports a diversity of plants and animals. The park has an elevation range from 2,127 to 13,114 feet (648 to 3,997 m) and contains five major vegetation zones: chaparral/oak woodland, lower montane forest, upper montane forest, subalpine zone, and alpine.

The geology of the Yosemite area is characterized by granitic rocks and remnants of older rock. About 10 million years ago, the Sierra Nevada was uplifted and then tilted to form its relatively gentle western slopes and the more dramatic eastern slopes. The uplift increased the steepness of stream and river beds, resulting in formation of deep, narrow canyons. About 1 million years ago, snow and ice accumulated, forming glaciers at the higher alpine meadows that moved down the river valleys. Ice thickness in Yosemite Valley may have reached 4,000 feet (1,200 m) during the early glacial episode. The downslope movement of the ice masses cut and sculpted the U-shaped valley. (Description from Wikipedia)

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Trinity Waterfall In Monasterio De Piedra Park

© RicardMN Photography

© RicardMN Photography

Monasterio de Piedra (Piedra Monastery) is a monastery, hotel and park complex in the Iberian System mountain ranges, near Nuévalos, province of Zaragoza, Aragon, Spain.

The monastery is located near the Piedra River Canyon, home to many species of birds, damselflies, trout, and endangered fish like the South-west European nase and an endangered species of barbel. The canyon itself includes a network of mossy, garden-like caves (natural and man-made), waterfalls and lagoons that contrast with the otherwise dry hills of southern Aragon.

The dissolution and precipitation of local limestone has created numerous rivulets, springs, and Karst topography. The Piedra River meanders around a mountain known as “El Espolón” (The Ram). In 1959, a dam was constructed across the river which created the 1300 acre La Tranquera Reservoir, flooding part of the canyon, some of the best local farmland, and several villages. The roofs of some drowned houses can still be seen when the water levels are down. The reservoir provides a domestic water supply, irrigation and electrical energy. (Description from Wikipedia)

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Uelhs Deth Joeu Falls

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© RicardMN Photography

Uels Deth Joeu Falls, Vall d’Aran, Lleida, Spain. 2012.

A thesis about the origin of the Garonne holds that the river rises on the slopes of Pic Aneto, at 2,300 m a.s.l. and flows by way of a sink hole known as the Forau de Aigualluts (42º40′00″N 0º40′01″E) through the limestone of the Tuca Blanca de Pomero and a resurgence in the Val dera Artiga above the Aran Valley in the Spanish Pyrenees. This underground route was suggested by the geologist Ramond de Carbonnieres in 1787, but there was no confirmation until 1931, when caver Norbert Casteret poured fluorescein dye into the flow and noted its emergence a few hours later 4 kilometres (2.5 mi) away at Uelhs deth Joeu (“Jove’s eyes” 42º40′51″N 0º42′28″E) in the Artiga de Lin on the other side of the mountain. From Aigualluts to the confluence with the main river at the bed of the upper Garonne valley (800 m a.s.l.), the Joeu has run for 12.4 km (16 more to get to the French border), carrying 2.16 m3/s. of water, while the main river is carrying 17.7 m3/s.

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Bridalveil Fall in Yosemite Valley

© RicardMN Photography

© RicardMN Photography

Bridalveil Fall is one of the most prominent waterfalls in the Yosemite Valley in California, seen yearly by millions of visitors to Yosemite National Park. The waterfall is 188 metres (617 ft) in height and flows year round.
The Ahwahneechee tribe believed that Bridalveil Fall was home to a vengeful spirit named Pohono which guarded the entrance to the valley, and that those leaving the valley must not look directly into the waterfall lest they be cursed. They also believed that inhaling the mist of Bridalveil Fall would improve one’s chances of marriage.

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