Travertine rock formations from calcium deposits

RMID:PK88EN

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Contributor:

Moment Photography / Alamy Stock Photo

Image ID:

PK88EN

File size:

17.3 MB (930.5 KB Compressed download)

Releases:

Model - no | Property - noDo I need a release?

Dimensions:

3008 x 2008 px | 25.5 x 17 cm | 10 x 6.7 inches | 300dpi

Date taken:

14 May 2005

Location:

Pamukkale

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RMC8DPCY–Mammoth Hot Springs is a series of hot springs on a hill of travertine in Yellowstone National Park in Wyoming. The travertine was created over thousands of years of calcium carbonate deposits coming from the hot springs travel through a fault line in limestone. The many colors of visible on the terraces are a result of algae growth in the warm pools which are roughly 170 degrees fahrenheit.

RMAPBT0J–Close up of travertine mineral deposits from hot springs at Puente del Inca, Mendoza Province, Argentina

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RFMYMDMA–View from the top of the travertine terraces with their thermal pools at the hot springs, Pumakkale, Anatolia, Turkey a UNESCO World Heritage Site

RMC8B8B2–Mammoth Hot Springs is a series of hot springs on a hill of travertine in Yellowstone National Park in Wyoming. The travertine was created over thousands of years of calcium carbonate deposits coming from the hot springs travel through a fault line in limestone. The many colors of visible on the terraces are a result of algae growth in the warm pools which are roughly 170 degrees fahrenheit.

RMAPBT8H–Close up of travertine mineral deposits from hot springs at Puente del Inca, Mendoza Province, Argentina

RMEEMMWT–View from travertine terraces of Pamukkale at sunset. Pamukkale, Denizli Province, Turkey.

RF2BD50MJ–Top view of travertine terrace formations at Pamukkale, Turkey. Spring water is light blue. Travertine - a sedimentary rock deposited by water from t

RMCMPJWB–Mammoth Hot Springs is a series of hot springs on a hill of travertine in Yellowstone National Park in Wyoming. The travertine was created over thousands of years of calcium carbonate deposits coming from the hot springs travel through a fault line in limestone. The many colors of visible on the terraces are a result of algae growth in the warm pools which are roughly 170 degrees fahrenheit.

RMAPBWDH–Detail of travertine mineral deposits from nearby hot springs at Puente del Inca, Mendoza Province, Argentina

Travertine rock formations from calcium deposits

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