Grand Canyon at twilight.

© RicardMN Photography

© RicardMN Photography

Grand Canyon at twilight.

Grand Canyon is a steep-sided canyon carved by the Colorado River in the United States in the state of Arizona.
The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile (6,000 feet / 1,800 metres) Nearly two billion years of the Earth’s geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.

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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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Ramesses II In Battle

© RicardMN Photography

© RicardMN Photography

Wall Painting of Temple of Beit El-Wali, which Ramses II constructed in Nubia during a period of the New Kingdom (1550 B.C. to 1069 B.C.) when the ancient Egyptians controlled the area. This Plaster Cast is in the British Museum, London, United Kingdom.
The Beit el-Wali temple is located in the area south of Egypt known to the Egyptians as Wawat, and to us as ancient ‘Nubia’. It supposed to remind the local people of the power of the Egyptian pharaoh, and to promote the worship of Egyptian gods.
There is a courtyard, decorated with scenes showing the pharaoh Ramesses II in battle against the enemies of Egypt. The southern wall of the courtyard has reliefs showing a battle between the Egyptians and their enemies to the south, the Nubians.
The plaster cast of the wall reliefs from the Beit el-Wali temple is on display in the ‘Egypt and Africa’ room (Room 65) of the British Museum in London.

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Golden Gate Bridge Looking South

© RicardMN Photography

© RicardMN Photography

The Golden Gate Bridge is a suspension bridge spanning the Golden Gate strait, the mile-wide, three-mile-long channel between San Francisco Bay and the Pacific Ocean. The structure links the U.S. city of San Francisco, on the northern tip of the San Francisco Peninsula, to Marin County, bridging both U.S. Route 101 and California State Route 1 across the strait. The bridge is one of the most internationally recognized symbols of San Francisco, California, and the United States. It has been declared one of the Wonders of the Modern World by the American Society of Civil Engineers.

The Frommers travel guide considers the Golden Gate Bridge “possibly the most beautiful, certainly the most photographed, bridge in the world”. It opened in 1937 and was, until 1964, the longest suspension bridge main span in the world, at 4,200 feet (1,300 m).

Before the bridge was built, the only practical short route between San Francisco and what is now Marin County was by boat across a section of San Francisco Bay. Ferry service began as early as 1820, with regularly scheduled service beginning in the 1840s for purposes of transporting water to San Francisco.

The weight of the roadway is hung from two cables that pass through the two main towers and are fixed in concrete at each end. Each cable is made of 27,572 strands of wire. There are 80,000 miles (130,000 km) of wire in the main cables. The bridge has approximately 1,200,000 total rivets.

As a prominent American landmark, the Golden Gate Bridge has been used in numerous media which includes books, films and video games.

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Canadian Rockies

© RicardMN Photography

B&W photographs of Canadian Rockies by RicardMN Photography. (See in 480p)
Music: Dream On – Aerosmith
The Canadian Rockies comprise the Canadian segment of the North American Rocky Mountains range. They are the eastern part of the Canadian Cordillera, extending from the Interior Plains of Alberta to the Rocky Mountain Trench of British Columbia. The southern end borders Idaho and Montana of the USA. The northern end is at the Liard River in northern British Columbia.

The Canadian Rockies have numerous high peaks and ranges, such as Mount Robson (3,954 m (12,972 ft)) and Mount Columbia (3,747 m (12,293 ft)). The Canadian Rockies are composed of shale and limestone. Much of the range is protected by parks and a World Heritage Site.

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