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Name : Dragon ’s Eye

fix : Uttakleiv Beach , Lofoten Islands , Norway

The Dragon Eye at dusk with the surrounding bay in the background. The eye is lit for the photograph.

Norway’s Dragon Eye likely formed under the ice around 20,000 years ago and emerged 4,000 years later with deglaciation.

Coordinates:68.20987277137073 , 13.499777198454572

Why it ’s incredible : White sand , algae and a big bowlder give this born landform its distinctive eyelike appearance .

" Dragon ’s Eye " is a natural hollow in the rock’n’roll along Norway ’s northwestern coastline that looks just like a reptilian eye . A boulder that sits at the bottom of the hole support out against a seam of ashen Amandine Aurore Lucie Dupin and algae , form the eye ’s school-age child .

Long exposure photograph of the dragon eye shaped rock at Uttakleiv Beach, Lofoten, the Norwegian Arctic.

Geological features like Norway’s Dragon’s Eye are called potholes. Dragon’s Eye measures roughly 5 feet (1.5 meters) across.

" The Dragon Eye is a rude feature that very belike formed beneath the large Fennoscandian Ice Sheet , possibly duringthe last frosting age,“Francis Chantel Nixon , an associate prof of forcible geography and quaternary geology at the Norwegian University of Science and Technology , told Live Science in an email . " This specific character of polar landform is call a pothole . "

Related : Why does Norway have so many fiord ?

The Fennoscandian Ice Sheet was an enormous glacier that blanket Scandinavia , as well as parts of Northern Europe and northwesterly Russia , during the last glacial maximum , around 20,000 age ago . Glaciation can go to all kinds of geological organization , including features call plastic forms , or phosphorus - physique , which result from erosion of the bedrock beneath the trash sail , Nixon say .

Aerial view of the water-filled Savonoski Crater surrounded by green vegetation.

" P - word form are make by meltwater full of scratchy sediments , " Nixon enunciate . These sediment include rocks of all shapes and sizes , ranging from fine backbone to giant boulders . High - pressing meltwater currents moving beneath the sparkler may " sculpt the basics into smooth - walled depression , which can be straight , curving or circular , and on the order of centimeters to several meters in width and deepness , " Nixon say .

pothole like Dragon ’s Eye are a eccentric of atomic number 15 - shape thought to be shaped by particularly churning meltwater flow that reduce abrasion and erosion in round patterns . " When the meltwater eventually slow up down or disappears , the rough-cut sediments will take root out of suspension and become trammel inside the chuckhole , " Nixon say , adding that this might be how a boulder come to sit down at the bottom of Dragon ’s Eye .

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Dragon ’s Eye probably emerged from beneath the water ice around 16,000 years ago , when deglaciation occurred in the surrounding part , Nixon said . The retreat of the Fennoscandian Ice Sheet endanger the fundamental principle and its pothole , which are made of gneiss , a case of metamorphic rock with colorfulmineral bandsthat add to the fantastical visual aspect of the centre .

An aerial photo of a roughly triangular island in the sea, which looks almost completely black

The eye , which measure roughly 5 feet ( 1.5 meters ) across , look different depending on the fourth dimension of solar day and the tides . At gamey lunar time period , waves wash over the rock and roll , episodically stick and removing sand from the empty , so that the boulder sometimes pose on mere fundamentals . The algae inside the eye also face different depending on the metre of year and the light source .

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