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Pamukkale, meaning "cotton castle" in
Turkish, is a
natural site in
Denizli Province
in south-western
Turkey. The city
contains hot springs and
travertines,
terraces of carbonate minerals left by the flowing water. It is located
in Turkey's Inner
Aegean region, in
the
River Menderes
valley, which has a temperate climate for most of the year.
The ancient city of
Hierapolis was
built on top of the white "castle" which is in total about 2,700 metres
(8,860 ft) long, 600 m (1,970 ft) wide and 160 m (525 ft) high. It can
be seen from the hills on the opposite side of the valley in the town of
Denizli, 20 km
away.
Tourism is and has been a major industry.
People have bathed in its pools for thousands of years. As recently as
the mid 20th century, hotels were built over the ruins of Heropolis,
causing considerable damage. An approach road was built from the valley
over the terraces, and motor bikes were allowed to go up and down the
slopes. When the area was declared a world heritage site, the hotels
were demolished and the road removed and replaced with artificial pools.
Wearing shoes in the water is prohibited to protect the deposits.
Pamukkale's terraces are made of
travertine, a
sedimentary rock deposited by water from the hot springs.
In this area, there are 17 hot water springs in
which the temperature ranges from 35 °C (95 °F) to 100 °C (212 °F).[citation
needed]
The water that emerges from the spring is transported 320 metres (1,050
ft)[citation
needed]
to the head of the travertine terraces and deposits calcium carbonate on
a section 60 to 70 metres (200 to 230 ft) long covering an expanse of
240 metres (790 ft) to 300 metres (980 ft). When the water,
supersaturated with
calcium carbonate,
reaches the surface,
carbon dioxide
degases from it, and calcium carbonate is deposited. The depositing
continues until the carbon dioxide in the water balances the carbon
dioxide in the air.[citation
needed]
Calcium carbonate is deposited by the water as a soft jelly,[citation
needed]
but this eventually hardens into travertine.
This reaction is affected by the weather
conditions, ambient temperature, and the flow duration. Precipitation
continues until the carbon dioxide in the thermal water reaches
equilibrium with the carbon dioxide in the atmosphere. Measurements made
at the source of the springs find atmospheric levels of 725 mg/l carbon
dioxide, by the time this water flows across the travertines, this
figure falls to 145 mg/l. Likewise calcium carbonate falls from
1200 mg/l to 400 mg/l and calcium 576.8 mg/l to 376.6 mg/l. From these
results it is calculated that 499.9 mg of CaCO3 is deposited on the
travertine for every liter of water. This means that for a flow rate of
1 ı/s of water 43191 grams are deposited daily. The average density of a
travertine is 1.48 g/cm3 implying a deposit of 29.2 dm3. Given that the
average flow of the water is 465.2 l/s this implies that it can whiten
13,584 square metres (146,220 sq ft) a day, but in practice this area
coverage is difficult to attain. These theoretical calculations indicate
that up to 4.9 square kilometres (1.9 sq mi) it can be covered with a
white deposit of 1 millimetre (0.039 in) thickness.
The former Roman Bath of the ancient city of
Hierapolis has been used as the site of the Hierapolis Archaeology
Museum since 1984.
In this museum, alongside historical artifacts
from Hierapolis, there are also artifacts from Laodiceia, Colossae,
Tripolis, Attuda and other towns of the Lycos (Çürüksu) valley. In
addition to these, the museum has a large section devoted to artifacts
found at Beycesultan Hüyük that includes some of the most beautiful
examples of Bronze Age craft.
Artifacts from the Caria, Pisidia and Lydia
regions are also on display in this museum. The museum’s exhibition
space consists of three closed areas of the Hierapolis Bath and the open
areas in the eastern side which are known to have been used as the
library and gymnasium. The artifacts in open exhibition space are mostly
marble and stone.
Pamukkale is a
tourist
attraction. It is recognized as a
World Heritage Sites
together with
Hierapolis.
Hierapolis-Pamukkale was made a
World Heritage Site
in 1988.[1]
The underground volcanic activity which causes
the hot springs also forced
carbon dioxide
into a cave, which was called the
Plutonium meaning
place of the god,
Pluto. This cave
was used for religious purposes by priests of
Cybele, who found
ways to appear immune to the suffocating gas.
Tadpoles can be
found in the pools. |