Pamukkale Resort 8th Wonder of the World!!!!

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    PamukkalePamukkalePamukkale is located in the Inner Aegean region

    at a distance of 20 km from the town of Denizli in Turkey.

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    Pamukkale (Hierapolis) translates to Cotton Castle.

    The great attraction is the white immensity of the cliff with

    sculptured basins full of water and congealed waterfalls; they

    seem done of snow, cloud, cotton.

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    On approaching Pamukkale,the first thing you will see isa rock platform over 100 m

    in height rising upfrom the plain.

    The slopes of this hill, whichlook from a distance

    like a great white speck, are

    covered withlarge numbers of pools

    and terraces.

    As you come nearer,you will begin to see

    this natural phenomenon,which resembles a frozen

    waterfall,in greater detail.

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    The scientific explanation is the hot thermal

    places that lie under the mount provoke

    the calcium carbonate spill, that makes

    the forms as solid as Travertino marble.

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    The temperature of the water forming the travertines,

    which issues from the hot springs on the hills above,

    falls to around 33C lower down.

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    Although the water flowing from the hot springs on the

    southern slopes of alda rapidly loses heat during its flow

    through the open channels, it is still hot enough to make it

    possible for one to bathe (throughout six months of the year)

    in the open-air swimming pools and on the terraces.

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    On emerging to the surface, the solution of calcium-carbonate in the spring water decomposes into

    carbon dioxide, calcium carbonate and water.

    The carbon dioxide is released into the air while the

    calcium carbonate separates off from the waterto form a grayish-white limestone sediment.

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    The beds of the water-courses are filled up with these

    limestone deposits and the water, confronted with these

    obstacles, splits up into several branches.

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    The water flows over the slopes into pools, the small basins

    surrounding them and finally into the fields below.

    It is in this way that these terraces over 100 m in height

    composed of layers of the accumulated limestone sediment

    have been gradually formed in the course of the ages.

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    As the limestone sediment reaches a certain level the water

    accumulates in pools and, as these pools fill up,

    overflows into smaller pools in the vicinity and from these

    flows into the small hollows and depressions around them.

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    The limestone layers in the pools rise up in steps,

    one above the other, and the continual flow of water

    keeps this process in operation.

    The stalactites form one of the most important

    features in the landscape.

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    With the formation of the layers and the emergence of steps

    and terraces one above the other, the water leaves

    the limestone deposit behind it and drips down

    in the form of stalactites, as in the Damlata caverns.

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    The calcium oxide in the water adds to the thickness ofthe white layers and widens the terraces,

    producing pools in fantastic shapes reminiscent of

    oyster shells or flower petals, while the small amount of

    sulphur and iron oxide produces stripes of yellow,

    red and green over the white of the limestone.

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    As much the cascades of calcium carbonate

    as the water change color in accordance

    with changes of the solar light that

    illuminates them, and the effect is surprising.

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    At times white, others blue,

    or green or other colors.

    The spectacle is flaring.

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    The continuous dynamics of the erosion and

    the transformation of the natural landscape

    result in an unusual environment.

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    PAMUKKALE is one of the most

    unique phenomena in nature.

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    We can call PAMUKKALE the 8th Wonder

    of the world.