Ziwa Van : Tofauti kati ya masahihisho

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[[Picha:Van1_20_modified.jpg|right|thumb|250x250px| Ziwa Van ]]
[[Picha:Ziwa Van.png|350px|thumb|Ramani ya Ziwa Van]]
[[Picha:Van1 20.jpg|right|thumb|250x250px| Ziwa Van pamoja na kanisa kwenye kisiwa cha Akdamar]]
'''Ziwa Van''' ( Turkish , Armenian ) ni [[Ziwa la chumvi|ziwa kubwa la chumvi]] na [[ziwa]] kubwa zaidi nchini [[Uturuki]], mashariki mwa nchi.
'''Ziwa Van''' ( Turkish , Armenian ) ni [[Ziwa la chumvi|ziwa kubwa la chumvi]] na [[ziwa]] kubwa zaidi nchini [[Uturuki]], mashariki mwa nchi.


==Jiografia==
Ziwa Van iko katika nyanda za juu kwenye kimo cha mita 1,640. Inapokea maji yake kutoka milima jirani lakini hakuna njia ya maji kutoka; mto uliotoka zamani ulifungwa na miamba ya volkeno miaka milioni iliyopita.
Ziwa Van iko katika nyanda za juu kwenye kimo cha mita 1,640. Inapokea maji yake kutoka milima jirani lakini hakuna njia ya maji kutoka; mto uliotoka zamani ulifungwa na miamba ya volkeno miaka milioni iliyopita.


Umbali kati ya miji Tatvan upande wa magharibi na [[Van]] upande wa mashariki ni kilomita 93, umbali mkubwa wa magharibi hadi mwisho wa hori upande wa mashariki ni km 127. Umbali mkubwa kutoka kaskazini hadi kusini ni km 52.
Maji yake ni ya chumvichumvi, hasa [[Ziwa la Magadi|magadi]].

Umbali kati ya miji Tatvan upande wa magharibi na Van upande wa mashariki ni kilomita 93, umbali mkubwa wa magharibi hadi mwisho wa hori upande wa mashariki ni km 127. Umbali mkubwa kutoka kaskazini hadi kusini ni km 52.


Kina kikubwa ni mita 451.
Kina kikubwa ni mita 451.
Mstari 12: Mstari 12:
Kuna feri ya reli inayozunguka baina ya Tatvan na Van. Treni za kimataifa baina ya Uturuki na Iran zinavuka hapa.
Kuna feri ya reli inayozunguka baina ya Tatvan na Van. Treni za kimataifa baina ya Uturuki na Iran zinavuka hapa.


Chumvi na ekolojia
== Chumvi na ekolojia ==
Maji yake ni ya chumvichumvi, takriban nusunusu [[magadi]] na [[NaCl]]. Maji huwa kwa wastani na [[thamani pH]] ya 9.8. <ref>Andreas Reimer, Günter Landmann & Stephan Kempe, Lake Van, Eastern Anatolia, hydrochemistry and history. Aquatic Geochemistry 15: 195-222, 2009</ref>


Kiwango cha magadi kwenye ziwa kinabadilika kufuatana na majira na pia ni tofauti kufuatana nakina cha maji. Maji yenye chumvi nyingi ni nzito zaidi hivyo maji ya usoni haina magadi mengi sawa na maji ya chini. Pia sehemu karibu na ufuko ambako mito inaingia huwa na maji matamu zaidi kuliko eneo la katikati.
Kiwango cha magadi kwenye ziwa kinabadilika kufuatana na majira na pia ni tofauti kufuatana nakina cha maji. Maji yenye chumvi nyingi ni nzito zaidi hivyo maji ya usoni haina magadi mengi sawa na maji ya chini. Pia sehemu karibu na ufuko ambako mito inaingia huwa na maji matamu zaidi kuliko eneo la katikati.


Kuna spishi moja ya samaki pekee inayopatikana katika ziwa; wakati wa kuzaa wanarudi kwenye midomo ya mito ambako kiasi cha maji matamu ni juu zaidi, baadaye wanaweza kurudi katika sehemu ambako kiwango cha magadi ni juu kiasi.
Kuna spishi moja ya samaki pekee (alburnus tarichi) inayopatikana katika ziwa; wakati wa kuzaa wanarudi kwenye midomo ya mito ambako kiasi cha maji matamu ni juu zaidi, baadaye wanaweza kurudi katika sehemu ambako kiwango cha magadi ni juu kiasi.


Kuna aina nyingi za planktoni.
i. Van iko kwenye urefu wa {{Convert|1640|m|ft|abbr=on}} na rangi ya jua kali, haiganda kwa sababu ya chumvi nyingi isipokuwa mara kwa mara sehemu ya kaskazini ya kaskazini. <ref> The New Encyclopædia Britannica, [http://www.britannica.com/EBchecked/topic/622548/Lake-Van Lake Van]</ref> Kisiwa cha Akdamar kiko katika ziwa hili.


== Historia ==
==Historia na utamaduni==
Katika [[milenia ya kwanza KK]] Ziwa Van ilikuw sehemu ya [[milki ya Urartu]].
Ziwa hilo lilikuwa kitovu cha milki ya Urartu kutoka karibu 1000 KK, na mji mkuu wa Urartu, Tushpa, ulikuwa kwenye mwambao wa Ziwa Van (kwenye tovuti ya jumba la enzi kuu la Van, magharibi mwa Van mji ). <ref>''The Concise Encyclopædia of Archaeology'' – Page 488 by Leonard Cottrell – 1960</ref>

Tangu karne ya 3 KK Ziwa Van ilikuwa katikati ya maeneo yaliyokaliwa na [[Waarmenia]]. Ushuhuda wake hadi leo ni [[monasteri]] ya Kiarmenia kwenye kisiwa cha [[Akdamar]]. Tangu [[maangamizi ya Waarmenia]] taifa hili halipo tena hapa lakini watalii wengi Waarmenia wanatembelea Akdamar.

Siki hizi kuna [[Wakurdi]] wengi katika mazingira ya ziwa.


Baadaye ardhi iliyozunguka ziwa ilitawaliwa na Waarmenia. <ref>''The Penguin Atlas of Diasporas'' – Page 77
by Jean-Pierre Rageau, Gérard Chaliand</ref> Pamoja na Ziwa Sevan kule [[Armenia]] ya leo na [[Ziwa Urmia]] katika [[Uajemi|Irani]] ya leo, <ref>''The Armenians'' – Page 12 by A. E. (Anne Elizabeth) Redgate</ref> <ref>''The Ancient Kingdom of Urartu'' – Page 1 by David Frankel</ref> Van alikuwa mmoja wa maziwa makuu matatu ya Ufalme wa Armenia, unaojulikana kama ''bahari ya [[Armenia]]'' . <ref>''Turkey'' – Page 28 by Pat Yale</ref> <ref>''Traditio'' – Page 7 by Institute of Research and Study in Medieval Canon Law</ref> <ref>''The Encyclopedia Americana'' – Page 330 by Grolier Incorporated</ref>


== Marejeo ==
== Marejeo ==
{{Reflist}}
{{Reflist}}

==Tovuti za Nje==
{{commons category|Lake Van}}
{{refbegin|33em}}
* {{Citation |url=http://www.hurriyetdailynews.com/ancient-castle-studied-in-lake-van-122422 |title=Ancient castle studied in Lake Van |website=Hürriyet Daily News |language=en |access-date=27 February 2018 |ref={{harvid|Ancient castle studied...|2017}} }}
* {{Citation |author=APA |url=http://yenisafak.com.tr/English/?t=27.07.2007&i=58392 |title=Turkey, Iran agree on joint railway |date=27 July 2007 |journal=Yeni Şafak |authorlink=Azerbaijan Press Agency }}
* {{Citation |last=Coskun |first=M. |last2=Musaoğlu |first2=N. |contribution-url=http://www.isprs.org/istanbul2004/comm7/papers/52.pdf |title=Proceedings of the 20th Congress of the International Society for Photogrammetry and Remote Sensing |year=2004 |contribution=Investigation of Rainfall-Runoff Modelling of the Van Lake Catchment by Using Remote Sensing and GIS Integration}}
* {{Citation |title=The Concise Encyclopædia of Archaeology |first=Leonard |last=Cottrell |date=1960 }}
* {{Citation |title=Nitrogenous waste excretion and accumulation of urea and ammonia in ''Chalcalburnus tarichi'' (Cyprinidae), endemic to the extremely alkaline Lake Van (Eastern Turkey) |url=http://www.springerlink.com/content/p4050j7u81790t3k/ |journal=Fish Physiology and Biochemistry |date=February 1992 |volume=9 |issue=5–6 |pages=377–386 |first1=Eva |last1=Danulat |first2=Stephan |last2=Kempe |doi=10.1007/BF02274218 |pmid=24213814 }}
* {{Citation |last=Degens |first=E.T.| last2=Wong |first2=H.K.| last3=Kempe |first3=S.| last4=Kurtman |first4=F.| title=A geological study of Lake Van, eastern Turkey |url=http://www.springerlink.com/content/x5285613642v3665/| journal=International Journal of Earth Sciences| publisher=Springer|date=June 1984| volume=73| issue=2| pages=701–734| doi=10.1007/BF01824978}}
* {{Citation |last1=Ebeling |first1=Erich |last2=Meissner |first2=Bruno |title=Reallexikon der Assyriologie und vorderasiatischen Archäologie |date=1997 |publisher=de Gruyter |location=Berlin |isbn=978-3110148091 |page=2 |url=https://books.google.com/books?id=O1yFrzi-MgYC |lang=de |trans-title=Lexicon of Assyriology and Near Eastern Archeology }}
* {{Citation |first=Sarah |last=Gibbens |url=https://news.nationalgeographic.com/2017/11/underwater-fortress-urartu-lake-van-turkey-archaeology-video-spd/ |title=Ancient Ruins Discovered Under Lake in Turkey |date=15 November 2017 |access-date=27 February 2018 |publisher=National Geographic }}
* {{Citation |last=Hewsen |first=Robert H. |author-link=Robert Hewsen |contribution=The Geography of Armenia |pages=1–17 |editor-last=Hovannisian |editor-first=Richard G. |editor-link=Richard G. Hovannisian |title=The Armenian People From Ancient to Modern Times |volume=Volume I – The Dynastic Periods: From Antiquity to the Fourteenth Century |date=September 1997 |publisher=St. Martin's Press |location=New York |isbn=978-0-312-10169-5 |ref={{Harvid|Hewsen|1997}} |url-access=registration |url=https://archive.org/details/armenianpeoplefr00rich_0 }}
* {{Citation |last1=Kempe |first1=S. |last2=Degens |first2=E.T. |date=1978 |chapter=Lake Van varve record: the past 10,420 years |title=Geology of Lake Van |publisher=MTA Press |editor-last1=Degens |editor-first1=E.T. |editor-last2=Kurtman |editor-first2=F. |place=Ankara |pages=56–63}}
* {{Citation |last=Kempe |first=S. |last2=Kazmierczak |first2=J. |last3=Landmann |first3=G. |last4=Konuk |first4=T. |last5= Reimer |first5=A. |last6=Lipp |first6=A. |title=Largest known microbialites discovered in Lake Van, Turkey |url=http://www.nature.com/nature/journal/v349/n6310/abs/349605a0.html |journal=Nature |date=14 February 1991 |volume=349 |pages=605–608 |doi=10.1038/349605a0 |issue=6310 }}
* {{Citation |encyclopedia=The New Encyclopædia Britannica |url=https://www.britannica.com/place/Lake-Van |title=Lake Van |date=1998 |ref={{Harvid|"Lake Van"|1998}} }}
* {{Citation |first=Günter |last=Landmann |first2=Andreas |last2=Reimera |first3=Gerry |last3=Lemcke |first4=Stephan |last4=Kempe |title=Dating Late Glacial abrupt climate changes in the 14,570 yr long continuous varve record of Lake Van, Turkey |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |publisher=[[Elsevier|Elsevier Science B.V.]] |date=June 1996 |volume=122 |issue=1–4 |pages=107–118 |doi=10.1016/0031-0182(95)00101-8}}
* {{Citation |first=Muhammed |last=Mina |url=http://www.hurriyet.com.tr/turkiyenin-en-buyuk-feribotu-van-golunde-deneme-seferine-cikti-40029217 |title=Türkiye'nin en büyük feribotu Van Gölü'nde deneme seferine çıktı |publisher=[[Hürriyet]] |date=19 December 2015 |accessdate=4 June 2016 |lang=tr |trans-title=Turkey's Largest Ferry Begins Trial Voyage on Lake Van }}
* {{Citation |url=http://www.losangeleschronicle.com/articles/viewArticle.asp?articleID=26515 |title=On the Roads of Anatolia&nbsp;— Van |first=Yüksel |last=Oktay |publisher=Los Angeles Chronicle |date=8 May 2007 |url-status=dead |archiveurl=https://web.archive.org/web/20070928150051/http://www.losangeleschronicle.com/articles/viewArticle.asp?articleID=26515 |archivedate=28 September 2007 }}
* {{Citation |title=A Treatise on the Geology of Armenia |url=https://books.google.com/books?id=veAQAAAAIAAJ&pg=PA102-IA2 |first=Felix |last=Oswald |date=1906}}
* {{Citation |last=Sarı |first=Mustafa |title=Inci Kefalı Summary |url=http://www.incikefali.net/ozet-en.htm |date=2006 |archive-url=https://web.archive.org/web/20080111200308/http://www.incikefali.net/ozet-en.htm |archive-date=11 January 2008 |publisher=Doğa Gözcüleri Derneği }}
* {{Citation |last=Sarı |first=Mustafa |title=Threatened fishes of the world: Chalcalburnus tarichi (Pallas 1811) (Cyprinidae) living in the highly alkaline Lake Van, Turkey |journal=Environmental Biology of Fishes |volume=81 |issue=1 |pages=21–23 |publisher=Springer Netherlands |year=2008 |doi=10.1007/s10641-006-9154-9 }}
* {{Citation |title=The structural elements and tectonics of the Lake Van basin (Eastern Anatolia) from multi-channel seismic reflection profiles |journal=[[Journal of African Earth Sciences]] |first1=Mustafa |last1=Toker |first2=Ali Mehmet Celal |last2=Sengör |first3=Filiz |last3=Demirel Schluter |first4=Emin |last4=Demirbağ |first5=Deniz |last5=Çukur |first6=Caner |last6=İmren |first7=Frank |last7=Niessen |doi=10.1016/j.jafrearsci.2017.01.002 |volume=129 |date=May 2017 |pages=165–178 |url=https://www.researchgate.net/publication/312222090 |ref={{Harvid|Toker|Sengör|Filiz|Demirbağ|2017}} }}
* {{Citation |last=Tomonaga |first=Yama |last2=Brennwald |first2=Matthias S. |last3=Kipfer |first3=Rolf |title=Spatial distribution and flux of terrigenic He dissolved in the sediment pore water of Lake Van (Turkey) |journal=Geochimica et Cosmochimica Acta |volume=75 |issue=10 |pages=2848–2864 |year=2011 |doi=10.1016/j.gca.2011.02.038 }}
* {{Citation |url=http://whc.unesco.org/en/tentativelists/1401/ |title=Tentative World Heritage Sites |author=[[UNESCO]] |ref={{harvid|UNESCO|n.d.}} }}
* {{Citation |title=Turkey's Lake Van Provides Precise Insights Into Eurasia's Climate History |url=https://www.sciencedaily.com/releases/2007/03/070314110552.htm |date=15 March 2007 |publisher=[[Science Daily]] |ref={{harvid|University of Bonn|2007}} |author=University of Bonn }}
* {{Citation |last=Warren |first=J.K. |title=Evaporites: Sediments, Resources and Hydrocarbons |publisher=Springer |date=2006 |isbn=978-3-540-26011-0 }}
* {{Citation| last=Wong| first=H.K. |last2=Degens| first2=E.T. |contribution=The bathymetry of Lake Van, eastern Turkey |title=Geology of Lake Van |pages=6–10 |publisher=General Directorate of Mineral Research and Exploration |place=Ankara |year=1978| issue=169}}

[[Jamii:Jiografia ya Uturuki]]
[[Jamii:Jiografia ya Uturuki]]
[[Jamii:Maziwa ya Asia]]
[[Jamii:Maziwa ya Asia]]

Pitio la 21:05, 14 Oktoba 2019

Ramani ya Ziwa Van
Ziwa Van pamoja na kanisa kwenye kisiwa cha Akdamar

Ziwa Van ( Turkish , Armenian ) ni ziwa kubwa la chumvi na ziwa kubwa zaidi nchini Uturuki, mashariki mwa nchi.

Jiografia

Ziwa Van iko katika nyanda za juu kwenye kimo cha mita 1,640. Inapokea maji yake kutoka milima jirani lakini hakuna njia ya maji kutoka; mto uliotoka zamani ulifungwa na miamba ya volkeno miaka milioni iliyopita.

Umbali kati ya miji Tatvan upande wa magharibi na Van upande wa mashariki ni kilomita 93, umbali mkubwa wa magharibi hadi mwisho wa hori upande wa mashariki ni km 127. Umbali mkubwa kutoka kaskazini hadi kusini ni km 52.

Kina kikubwa ni mita 451.

Kuna feri ya reli inayozunguka baina ya Tatvan na Van. Treni za kimataifa baina ya Uturuki na Iran zinavuka hapa.

Chumvi na ekolojia

Maji yake ni ya chumvichumvi, takriban nusunusu magadi na NaCl. Maji huwa kwa wastani na thamani pH ya 9.8. [1]

Kiwango cha magadi kwenye ziwa kinabadilika kufuatana na majira na pia ni tofauti kufuatana nakina cha maji. Maji yenye chumvi nyingi ni nzito zaidi hivyo maji ya usoni haina magadi mengi sawa na maji ya chini. Pia sehemu karibu na ufuko ambako mito inaingia huwa na maji matamu zaidi kuliko eneo la katikati.

Kuna spishi moja ya samaki pekee (alburnus tarichi) inayopatikana katika ziwa; wakati wa kuzaa wanarudi kwenye midomo ya mito ambako kiasi cha maji matamu ni juu zaidi, baadaye wanaweza kurudi katika sehemu ambako kiwango cha magadi ni juu kiasi.

Kuna aina nyingi za planktoni.

Historia na utamaduni

Katika milenia ya kwanza KK Ziwa Van ilikuw sehemu ya milki ya Urartu.

Tangu karne ya 3 KK Ziwa Van ilikuwa katikati ya maeneo yaliyokaliwa na Waarmenia. Ushuhuda wake hadi leo ni monasteri ya Kiarmenia kwenye kisiwa cha Akdamar. Tangu maangamizi ya Waarmenia taifa hili halipo tena hapa lakini watalii wengi Waarmenia wanatembelea Akdamar.

Siki hizi kuna Wakurdi wengi katika mazingira ya ziwa.


Marejeo

  1. Andreas Reimer, Günter Landmann & Stephan Kempe, Lake Van, Eastern Anatolia, hydrochemistry and history. Aquatic Geochemistry 15: 195-222, 2009

Tovuti za Nje

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