Düden Waterfalls
Encyclopedia
Düden Waterfalls are a group of waterfalls in the province of Antalya
, Turkey
. The waterfall, formed by the Düden River (one of the major rivers in southern Anatolia), is located 12 km north-east of Antalya; which ends, where the limpid waters of the Lower Düden Falls drop off a rocky cliff directly into the Mediterranean Sea
in a dazzling show.
(which goes through Dösemealti town) there appear two big Karstic sources. These sources, Kirkgözler and Pinarbasi which are very rich waterwise, coincide after a very short flow and they disappear finally in Biyikli Sinkhole
. Some of the sinkholes are so big that they can swallow a huge river or a big lake. In this region there are the Sugla (Konya) big sinkhole the Biyikli sinkhole with its output of 30 m³/s. This quantity is the output of Kirkgöz and Pinarbasi springs at inundation.
The water which disappears at Biyikli Sinkhole goes 14 km underground and comes out again at Varsak pit; after a very short fall it disappears again from the other end. To understand the mechanism correctly you must follow the map and schema. The water which disappears at Varsak goes underground for 2 km and comes out again at Düdenbasi by pressure made by a syphon. The water which falls from Düdenbasi is the water coming from Kepez Hydroelectrical Complex. By all these actions (water coming in and out) Kepez Hydroelectrical Complex has been built.
By means of regulator built in front of the Biyikli Sinkhole, the waters of Kirkgözler and Pinarbasi are directed into a canal and then by a long canal to the Kepez Hydroelectric Plant to the collector from where by a pressure pipe it is carried to the balancing funnel and then dropped over the plant's turbines.
The water from the plant's discharge unit is brought to Düdenbasi again by a long canal where it forms artificial cascades. From there the amount of water is that of a large river and this water by means of seven irrigation trenches is used to irrigate the land north-east of the city of Antalya.
After Düdenbasi the waters of Düdençay separate into a number of streams and finally east of Antalya at a height of 40 m plunge from a platform into the Mediterranean in the form of cascades.
At the spot where the cascades fall into the Mediterranean is an attractive park. In spring when water is plentiful this is a sight not to be missed. They can be seen from the sea by talking a boat trip from Antalya yacht harbour, which is a very pleasant trip.
Antalya Province
Antalya Province is located on the Mediterranean coast of south-west Turkey, between the Taurus Mountains and the Mediterranean sea.Antalya Province is the centre of Turkey's tourism industry, attracting 30% of foreign tourists visiting Turkey. The province of Antalya corresponds to the lands of...
, Turkey
Turkey
Turkey , known officially as the Republic of Turkey , is a Eurasian country located in Western Asia and in East Thrace in Southeastern Europe...
. The waterfall, formed by the Düden River (one of the major rivers in southern Anatolia), is located 12 km north-east of Antalya; which ends, where the limpid waters of the Lower Düden Falls drop off a rocky cliff directly into the Mediterranean Sea
Mediterranean Sea
The Mediterranean Sea is a sea connected to the Atlantic Ocean surrounded by the Mediterranean region and almost completely enclosed by land: on the north by Anatolia and Europe, on the south by North Africa, and on the east by the Levant...
in a dazzling show.
Düdenbasi Waterfall Karstic System
At the 28th and 30th km of the old route from Antalya-BurdurBurdur
Burdur , is a city southwestern Turkey and the seat of the Burdur Province of Turkey. It is located at , on the shore of Lake Burdur...
(which goes through Dösemealti town) there appear two big Karstic sources. These sources, Kirkgözler and Pinarbasi which are very rich waterwise, coincide after a very short flow and they disappear finally in Biyikli Sinkhole
Sinkhole
A sinkhole, also known as a sink, shake hole, swallow hole, swallet, doline or cenote, is a natural depression or hole in the Earth's surface caused by karst processes — the chemical dissolution of carbonate rocks or suffosion processes for example in sandstone...
. Some of the sinkholes are so big that they can swallow a huge river or a big lake. In this region there are the Sugla (Konya) big sinkhole the Biyikli sinkhole with its output of 30 m³/s. This quantity is the output of Kirkgöz and Pinarbasi springs at inundation.
The water which disappears at Biyikli Sinkhole goes 14 km underground and comes out again at Varsak pit; after a very short fall it disappears again from the other end. To understand the mechanism correctly you must follow the map and schema. The water which disappears at Varsak goes underground for 2 km and comes out again at Düdenbasi by pressure made by a syphon. The water which falls from Düdenbasi is the water coming from Kepez Hydroelectrical Complex. By all these actions (water coming in and out) Kepez Hydroelectrical Complex has been built.
By means of regulator built in front of the Biyikli Sinkhole, the waters of Kirkgözler and Pinarbasi are directed into a canal and then by a long canal to the Kepez Hydroelectric Plant to the collector from where by a pressure pipe it is carried to the balancing funnel and then dropped over the plant's turbines.
The water from the plant's discharge unit is brought to Düdenbasi again by a long canal where it forms artificial cascades. From there the amount of water is that of a large river and this water by means of seven irrigation trenches is used to irrigate the land north-east of the city of Antalya.
After Düdenbasi the waters of Düdençay separate into a number of streams and finally east of Antalya at a height of 40 m plunge from a platform into the Mediterranean in the form of cascades.
At the spot where the cascades fall into the Mediterranean is an attractive park. In spring when water is plentiful this is a sight not to be missed. They can be seen from the sea by talking a boat trip from Antalya yacht harbour, which is a very pleasant trip.