Tafkin Taka

Tafkin Taka
General information
Height above mean sea level (en)	650 m
Labarin ƙasa
Tsarin Daidaiton Labarin Kasa	37°26′N 22°22′E
Kasa	Greek
Territory	Tripoli Municipality (en)
Ƙasantuwa a yanayin ƙasa	Peloponnese (en)

Ruwa, ambaliyar ruwa a kusa, ponors, tsohon Lake Taka na wucin gadi

Tafkin Taka (Girkanci) tafki ne na wucin gadi wanda ke kudu da babban kwandon da ake kira "Tripoli-Plateau" a Girka . A cikin hunturu, kudancin ɓangaren kwandon sau da yawa yana ambaliya, kuma tafkin yana samuwa daga ruwan sama mai yawa saboda rashin isasshen ruwa. A wetland Biotope da sauri ci gaba, da kuma nau'ikan dabbobin da ke son ruwa sun bayyana. A lokacin zafi da bushewa, tafkin ya bushe. A tsawon lokaci, karstification yana haifar da ponors da yawa, inda ruwa ke barin kwandon ta hanyar ruwa na ƙasa.

Ɗaya daga cikin 7 ponors da ke zubar da Tafkin Taka

Babbar ponor (Κατα Diostaθρα katavothra) na tsohuwar Tafkin Taka

Hoton tarihi na mafi girman katavothra na tsohuwar Tafkin Taka

Tafkin Taka

Yanayin ƙasa

Tafkin Taka yana zaune a tsawo na mita 650 a gabashin Tegea kuma ca. Km 10 kudu da Tripoli, babban birnin Arcadia.  Tafkin yana tattara ruwan sama, wanda ya fito ne daga duwatsu da ke kewaye da kwandon, wanda ake kira "Tripoli-Plateau" (tsawon kusan kilomita 30 da faɗin tsakanin kilomita 12.5 da 25).   A lokacin zafi da bushewa, tafkin na wucin gadi yawanci ya bushe gaba ɗaya (ya bar wasu ruwan ban ruwa a cikin tafkin da aka yi).

Ƙasar Tripoli Basin a hankali ta zama mai tsarawa (musamman bayan 1945) kuma mafi yawansu sun zama gonar gona. An gina babban tafkin a kusa da shekara ta 2000 tare da goyon bayan asusun EU, don riƙe ruwa don ban ruwa a lokacin fari.

elimin dutse na kasa

Duwatsu sun kewaye kwandon. Rashin ba shi da wani gagarumin lalacewa. Yankin yana narkewa ta hanyar hanyoyin ruwa. Irin waɗannan "kayan da aka rufe" da kuma faruwarsu a kan Peloponnese da kuma Arcadia wani abu ne mai ban mamaki. A kusan dukkanin yankin Peloponnese, tectonics mai tsanani ya rushe dutse- da irin wannan tsarin carbonate na Arcadia a tsawon lokaci. Ruwa yana gudana ta hanyar fashewar da aka haifar da tectonically kuma yana narkar da dutse (karstifikation) kuma ta haka ne ya fadada fashewar a tsawon lokaci. A kasan gangaren, inda ruwan tafkin yake cikin hulɗa kai tsaye tare da dutsen carbonate waɗannan raguwa sannu a hankali suna girma don zama ponors (Katvothres, Girkanci), wanda ke zubar da ruwa. Ponors bakwai na girma daban-daban (babban ponor ya zana bango mai zurfi ta hanyar ca. 25 m), don zubar da tafkin. Ko da lokacin da ba a rufe waɗannan katavothres ba, magudanar ruwa tana da jinkiri. Wannan shine dalilin da ya sa aikin gona ba zai iya farawa a lokacin da ya dace ba. A cikin hunturu mai ruwan sama, kamar yadda 2003, samun ruwa yana ambaliya ƙasa a kusa da madatsar ruwan, saboda wannan shine mafi ƙasƙanci na Tripoli-Plateau .

Muhalli da yanayi

Lokacin da ambaliyar ruwa a waje da tafkin da aka yi amfani da shi ta faru, ruwan sama yana taimakawa ci gaba da sauri na yanayin ruwa. Fauna sun hada da tsuntsayen teku da kingfishers. Binciken bincike a tafkin ya sami alamun tsohon birnin Manthirea, wanda ya samo asali ne daga tsohon sunan yankin "Manthuriko Plain". An kare wurin da ya fi girma a matsayin wurin zama na Natura 2000.

Tushen

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• Mariolakos, Ilias. Yanayin Geomythological da Ayyukan Geotechnical da Hydraulic na Prehistoric a Arkadia, Taron Kasa da Kasa na 12 na Geological Society of Greece, Jagoran Tafiye-tafiye, Patras Mayu 2010 a Girkanci

Haɗin waje

• Mariolakos, Yanayin Geomythological a Arcadia a cikin Girkanci
• Φιλότης, βιότοπος Φιλότηος, βιιότο Consoine a cikin Girkanci