My Photos / Photography

IN MY HIGHT SCHOOL "Lycée paul éluard"

My crazy friends :) 

One Of the World's Largest Mirror

It's also called "Salar de Uyuni" (salar  in Spanish is salt flat ) is currently the world’s largest salt flat at 10,582 square kilometers (4,086 sq mi). 

No, This is not  a Photoshop trick..!!

 The Salar was formed as a result of transformations between several prehistoric lakes. It is covered by a few meters of salt crust, which has an extraordinary flatness with the average altitude variations within one meter over the entire area of the Salar.

 Salar de Uyuni is also a climatological transitional zone since the towering tropical cumulus congestus and cumulus incus clouds that form in the eastern part of the salt flat during the summer cannot permeate beyond its drier western edges, near the Chilean border and the Atacama Desert.

 Salar de Uyuni is part of the Altiplano of Bolivia in South America. The Altiplano is a high plateau, which was formed during uplift of the Andes mountains. The plateau includes fresh and saltwater lakes as well as salt flats and is surrounded by mountains with no drainage outlets

 Isn't it beautiful? or Just look like a painting 

Don't you belive me? Have a look :)

Yellowstone National Park USA

YELLOWSTONE. DON’T JUST SEE IT, EXPERIENCE IT!

The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: theColorado Plateaus, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section .

Have you ever seen  arc on earth ? 

No , I'm not kidding and I'm not mad ......

Yes, There is an arc on earth and it's in the Yellowstone National Park USA

Yellowstone is at the northeastern end of the Snake River Plain, a great U-shaped arc through the mountains that extends from Boise, Idaho some 400 miles (640 km) to the west. This feature traces the route of the North American Plate over the last 17 million years as it was transported by plate tectonics across a stationary mantle hotspot. The landscape of present-day Yellowstone National Park is the most recent manifestation of this hotspot below the crust of the Earth.

 

Winter scene in Yellowstone

VENICE-ITALY

Oh Venice, where do I start? I  personally loved every single Photo and videos of Venice That I watched On the internet and on YouTube . What a beautiful, magical place. . One day I hope I'll go there I haven't word to  describe the Beauty of Venice.

Venice, Italy, From Above

Venice  is a city in northeastern Italy sited on a group of 118 small islands separated by canals and linked by bridges. It is located in the marshy Venetian Lagoon which stretches along the shoreline, between the mouths of the Po and the Piave Rivers. Venice is renowned for the beauty of its setting, its architecture, and its artworks. The city in its entirety is listed as a World Heritage Site, along with its lagoon.

 Here we have Francesco Guardi, The Grand Canal,  isn't it realy beautiful ?

Here is some pictures in night 

The buildings of Venice are constructed on closely spaced wooden piles. Most of these piles are still intact after centuries of submersion. The foundations rest on the piles, and buildings of brick or stone sit above these footings. The piles penetrate a softer layer of sand and mud until they reach a much harder layer of compressed clay.

Giant’s Causeway, Ireland

The Giant's Causeway (known as Clochán an Aifir or Clochán na bhFomhórach in Irish and tha Giant's Causey inUlster-Scots) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption.

It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills.

Around 50 to 60 million years ago, during the Paleogene Period, Antrim was subject to intense volcanic activity, when highly fluid molten basalt intruded throughchalk beds to form an extensive lava plateau. As the lava cooled, contraction occurred. Horizontal contraction fractured in a similar way to drying mud, with the cracks propagating down as the mass cooled, leaving pillarlike structures, which are also fractured horizontally into "biscuits". In many cases the horizontal fracture has resulted in a bottom face that is convex while the upper face of the lower segment is concave, producing what are called "ball and socket" joints. The size of the columns is primarily determined by the speed at which lava from a volcanic eruption cools. The extensive fracture network produced the distinctive columns seen today. The basalts were originally part of a great volcanic plateau called the Thulean Plateau which formed during the Paleogene.

Some of the structures in the area, having been subject to several million years of weathering, resemble objects, such as the Organ and Giant's Boot structures. Other features include many reddish, weathered low columns known as Giants Eyes, created by the displacement of basalt boulders; the Shepherd's Steps; theHoneycomb; the Giant's Harp; the Chimney Stacks; the Giant's Gate and the Camel's Hump.

Santorini, Greece

Santorini is the most popular island in Greece. It may be the most popular island in the world. There are few travel destinations that combine beautiful beaches, spectacular scenery, ancient cities, amazing restaurants, some of the world's best wine, and an active volcano. But Santorini has all this and more .....

 Santorini is a mix of towering cliffs, inky waters and whitewashed villages. Perfect for a post-summer break.