Here is a list of travel locations that look so unreal, you’ll wish you had a teleportation machine equipped with cannabis and shrooms.

Crystal Cave – Skaftafell, Iceland

surreal-travel-spot-crystal-cave-icelandCreated by the awesome forces of the Vatnajvkull ice cap in the south of the volcanic island, the deep blue cave was formed by the glacier meeting the coastline.

The centuries old ice that has come from the slopes of 6,921 feet tall Vrffajvkull, Iceland’s tallest active volcano, has compressed all air out of the ice adding to the texture and color of the cave.


Mt. Roraima, Venezuela

surreal-travel-spot-mt-roraima-venezuelaThe mountains of this range, including Roraima, are considered to be some of the oldest geological formations known, some dating back to two-billion years ago. Its near daily rains have also created a unique ecosystem which includes several endemic species, including a unique carnivorous pitcher plant, and some of the highest waterfalls in the world.


Salar de Uyuni, Bolivia

surreal-travel-spot-salar-de-uyuniSalar de Uyuni is the world’s largest salt flat. The area, some 11,985 feet above sea level, is always a tourist playground, with salt hotels and hot springs serving as major attractions.


Zhangye, China

surreal-travel-spot-zhangye-chinaEarly landscape formation joined together all the rock layers of colors imaginable in one place, specifically in the area known as Zhangye Danxia, thus achieving what is perhaps the greatest gathering of different pigments in natural stone in the world.


The Stone Forest – Yunnan, China

surreal-travel-spot-stone-forest-yunnan-chinaThe Stone Forest is a notable set of limestone formations located in Yunnan Province, China. The tall rocks seem to emanate from the ground in the manner of stalagmites, with many looking like petrified trees thereby creating the illusion of a forest made of stone. 


Lake Retba – Senegal

surreal-travel-spot-lake-retba-senegalThe bizarre pink color of Lake Retba is caused by Dunaliella salina, a type of halophile green micro-algae, that is found in the water.  The high salt content of the lake means that not only is there a booming salt collecting industry on its banks, but like the Dead Sea, you are able to float in it.


Grand Prismatic Spring – Yellowstone National Park, Wyoming

surreal-travel-spot-grand-prismatic-spring-yosemiteGrand Prismatic Spring has the distinction of being the park’s largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m) deep. A hot spring is an area where heated water can easily rise through cracks and fractures in the earth’s surface.

The breathtaking colors are attributed to the various species of thermophilic bacteria living in the spring. The blue water in the center is very hot, but it may support chemotrophic life – a chemotroph is an organism that uses chemicals for a source of energy. As you move farther from the heat source of the spring, life begins to flourish. The cyanobacteria – aquatic photosynthesizing bacteria – that live at the edges of Grand Prismatic Spring cover the color spectrum including yellow, green, orange, red, and brown.


Door to Hell – Derweze, Turkmenistan

surreal-travel-spot-Derweze-TurkmenistanThe Door to Hell is a natural gas field in Derweze (also spelled Darvaza, meaning “gate”), Ahal Province, Turkmenistan. The Door to Hell is noted for its natural gas firing which has been burning continuously since 1971, fed by the rich natural gas deposits in the area. The pungent smell of burning sulfur pervades the area for some distance.


The Richat Structure – Mauritania

surreal-travel-spot-richat-structure-MauritaniaRichat Structure is not the site of an ancient meteor crater, as many people originally postulated. These concentric circles are actually alternating layers of sedimentary, metamorphic, and igneous rocks that were pushed upward in a symmetrical anticline, geologic dome, from below due to a small incursion of magma. The structure is a deeply eroded. The sedimentary rock exposed in this dome range in age from Late Proterozoic (2.5 billion years) within the center of the dome to Ordovician (480 million years) sandstone around its edges.