Bat iyeltak tir mal Wikimedia Commons ise gan yonar abdumimaks rotir zo faver.
Pimtara moe inafu iyeltakbu valeveon zo nedir.
Pimtara
PimtaraChato Volcano & Cerro Chato Lake (Arenal Volcano National Park, Costa Rica, Central America) (39885276554).jpg
(photo provided by Anna Yoder)
(summer 2014)
Chato Volcano is an inactive stratovolcano in the Central American Volcanic Arc. This Tertiary- and Quaternary-aged chain of volcanoes extends from Guatemala to Panama. It formed next to a subduction zone where the ~northeast-moving Cocos Plate is diving below the North American Plate and the Caribbean Plate along the Middle-America Trench. About 50 major volcanic centers are present. Chato was active from the Late Pleistocene to the late Holocene (38 ka to 3.8 ka).
Shown above is Cerro Chato Lake that fills Chato Volcano's summit crater.
Locality: Chato Volcano, northwestern Tilarán Range, Arenal Volcano National Park, western Alajuela Province, northern Costa Rica, Central American Volcanic Arc (10° 26' 33" North latitude, 84° 41' 17.15" West longitude)
Ta walzilira – ta ksudara va kobara azu walzilira azu deara
Ta warzafa ponara – Ta zalera va grabom
Nope valevef kredeem :
gaara – Va folack govanzilil ise va gluyaxa godaful ise gobazel kase betara al zo skud. Laninde gonaskil voxe mekane gometiavel da gelfasik va rin ik rinafa favera vanovar.
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Bat iyeltak va loplekufa giva ruldar. Bata giva male reduso ok tuotukaso wanuyasiko iku ksudasiko lanon zo loplekuyur. Ede iyeltak malion di zo betayar, konaka pinta va betayana ewava rotir me co tcazecked.