For thousands of years an underground spring
located deep
in the earth has been pouring out streams
of hot mineral-saturated
water. The water has shaped the
area by depositing limestone.
The Pamukkale Springs form part of a network
extending
on the north-west as far as the city of
Alasehir (the ancient
Philadelphia) 70km. away, and on the west
to the
Meander valley and the Aegean Sea beyond.
Pamukkale, in Turkey is famous for its
limestone terraces,
waterfalls and thermal springs.
These natural springs form
open air pools in the stepped limestone
deposits. The warm
mineral-rich water has been acknowledged
as having
therapeutic powers for centuries.
The waters coontain calcium magnesium sulphate
and
bicarbonate with carbon dioxide is solution.
The mineral
content of the water is 2430 mg/litre,
with a pH of 6
(more-or-less neutral) and a radiation
count of
1537 picokuri/litre. The springs
flow at a rate
of 400 liters per second.
The waters are used both for drinking and
bathing. They
are recommended for the treatment of rheumatic,
dermatological
and gynaecological diseases, mental and
physical exhaustion,
minor digestive problems and nutrition
disorders.
The name Pamukkale means "cotton castle".
Local legend
has it that in ancient times giants were
known to dry cotton
crops along the terraces.
When the water emerges from the springs
the pressure drops
causing the CO2 in the
water to vapourises and the calcium
carbonate (limestone) to be precipitated
out, to form the "travertine"
formations that now constitute the distinctive
features of the site.
The formations have been described as
"frozen waterfalls".
The terraced layers cover an area of about
3000m by 300m at a
height of about 100 m above the surrounding
plain.
The Pamukkale springs have been affected
from time to time by
the strong earthquakes characteristic
of the region. Some springs
have even dried up altogether, the water
sometimes re-emerging
from a completely new spring nearby.
The stepped pools at Pamukkale, fed by
natural thermal springs.