Everything about Lake Van totally explained
Lake Van (, ("Lake of Van")) is the largest
lake in
Turkey, located in the far east of the country. It is a
saline and soda lake, receiving water from numerous small streams that descend from the surrounding mountains. Lake Van is one of the world's largest
endorheic lakes (having no outlet). The original outlet from the basin was blocked by an ancient volcanic eruption.
Hydrology and chemistry
Lake Van is 119 km across at its widest point, averaging a depth of with a maximum recorded depth of . The lake surface lies above sea level and the shore length is . Lake Van has an area of [[1E9 m²|]] and a volume of .
The lake water is strongly
alkaline (
pH 9.7–9.8) and rich in
sodium carbonate and other
salts, which are extracted by evaporation and used as
detergents.
Geology
The lake's outlet was blocked at some time during the
Pleistocene, when
lava flows from
Nemrut volcano blocked westward outflow towards the
Muş Plain. Now dormant,
Nemrut Dağı is close to the western shore of the lake, and another dormant
stratovolcano,
Süphan Dağı dominates the northern side of the lake.
The water level of the lake has often altered dramatically: near Tatvan, Oswald (see Geology of Armenia, 1901) noted a raised beach high above the present level of the lake as well as recently drowned trees. Investigation by Degens and others in the early 1980s determined that the highest lake levels (72m above the current height) had been during the last ice age, about 18,000 years ago. About 9,500 years ago there was a dramatic drop to more than 300m below the present level. This was followed by an equally dramatic rise around 6,500 years ago.
As a deep lake with no outlet, Lake Van has accumulated great amounts of sediment washed in from surrounding plains and valleys, and occasionally deposited as ash from eruptions of nearby volcanoes.
This layer of sediment is estimated to be up to 400m thick in places, and has attracted climatologists and vulcanologists interested in drilling cores to examine the layered sediments.
In 1989 and 1990, an international team of geologists led by Dr. Stephan Kempe from the University of Hamburg (now Professor at the Technische Universität Darmstadt) retrieved ten sediment cores from depths up to . Although these cores only penetrated the first few meters of sediment, they provided sufficient
varves to give climate data for up to 14,570 years
BP.
A team of scientists headed by palaeontologist Professor Thomas Litt at the
University of Bonn has applied for funding from the
International Continental Scientific Drilling Program (ICDP) for a new, deeper drilling project to examine the lake's sediments. Litt expects to find that "Lake Van stores the climate history of the last 800,000 years—an incomparable treasure house of data which we want to tap for at least the last 500,000 years." A test drilling in 2004 detected evidence of 15 volcanic eruptions in the past 20,000 years.
Ecology
The only
fish known to live in the
brackish water of Lake Van is
Chalcalburnus tarichi the Pearl Mullet or
inci kefalı, a
Cyprinid fish related to
chub and
dace, which is caught during the spring floods. In May and June, these fish migrate from the lake to less alkaline water, spawning either near the mouths of the rivers feeding the lake or in the rivers themselves. After spawning season it returns to the lake.
103 species of
phytoplankton have been recorded in the lake including
Diatome,
Bacteriophyta,
Cyanophyta,
Chlorophyta,
Flagellata and
Phaeophyta. 36 species of
zooplankton have also been recorded including
Rotatoria,
Cladocera and
Copepoda in the lake.
In 1991, researchers reported the discovery of tall
microbialites in Lake Van. These are solid towers on the lake bed created by mats of coccoid
cyanobacteria (
Pleurocapsa group) that create
aragonite in combination with
calcite precipitating out of the lake water.
The Lake Van region is the home of the rare
Van Kedisi breed of
cat, noted for among other things its unusual fascination with water.
Since about 1995 there have been reported sightings of a
'Lake Van monster' about in length named
Van Canavarı ("Monster of Van").
The lake is surrounded by
fruit and
grain-growing
agricultural areas.
History
Tushpa, the capital of
Urartu, was located near the shores of Lake Van, on the site of what became medieval Van's castle, west of present-day
Van city. The ruins of the medieval city of Van are still visible below the southern slopes of the rock on which
Van Castle is located.
Armenian kingdoms
The lake was the centre of the
Armenian kingdom of Ararat from about
1000 BC, afterwards of the Satrapy of Armina,
Kingdom of Greater Armenia, and the Armenian Kingdom of
Vaspurakan.
Along with
Lake Sevan in today's
Armenia and
Lake Urmia in today's
Iran, Van was one of the three great lakes of the Armenian Kingdom, referred to as
the seas of Armenia (in ancient Assyrian sources: "tâmtu ša mât Nairi" (Upper Sea of Nairi), the Lower Sea being
Lake Urmia). Over time, the lake was known by various Armenian names, including .
Byzantine empire
By the
11th century the region around Lake Van was on the border between the
Byzantine empire, with its capital at
Constantinople, and the
Seljuk Turkish empire, with its capital at
Isfahan. In the uneasy peace between the two empires, local Armenian-Byzantine landowners employed
Turcoman gazis and Byzantine
akritoi for protection. However, these mercenaries often turned to looting for their own benefit.
In the second half of the 11th century the situation on the southeast border of the Byzantine empire had reached such a point that Emperor
Romanus IV Diogenes launched a campaign to re-conquer Armenia and head off growing Seljuk control. Diogenes and his large army crossed the
Euphrates and confronted a much smaller Seljuk force led by
Alp Arslan at the
Battle of Manzikert, north of Lake Van on
26 August 1071. Despite their greater numbers, the cumbersome Byzantine force was defeated by the more mobile Turkish horsemen and Diogenes was captured.
Seljuk empire
Alp Arslan divided the conquered eastern portions of the Byzantine empire among his Turcoman generals, with each ruled as a hereditary
beylik, under overall sovereignty of the
Great Seljuq Empire. Alp Arslan gave the region around Lake Van to his commander Sökmen el Kutbî (literally
Sökmen the Slave), who set up his capital at Ahlat on the western side of the lake. The dynasty of
Ahlatshahs (also known as
Sökmenler) ruled this area from 1085 to 1192.
The Ahlatshahs were succeeded by the
Ayyubid dynasty.
Architecture
Near the
Van Castle and the southern shore, on
Akdamar Island lies the
Church of the Holy Cross (Armenian: Սուրբ Խաչ, Surb Khach), which served as a royal church to the Armenian
Vaspurakan kingdom.
The Ahlatshahs left a large number of historic
tombstones in and around the town of
Ahlat. Local administrators are currently trying to have the tombstones included in
UNESCO's
World Heritage List, where they're currently listed tentatively.
Transportation
The railway connecting Turkey and
Iran built in the
1970s uses a
train ferry across Lake Van between the cities
Tatvan and
Van, rather than building railway tracks around the rugged shore line. Transfer from train to ship and back again limits the total carrying capacity.
Islands
Further Information
Get more info on 'Lake Van'.
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