, ▁me and ering ▁stream , ▁with ▁a ▁minimal ▁descent , ▁it ▁has ▁long ▁been ▁not orious ▁for ▁flo oding . ▁The ▁prede cess or ▁of ▁the ▁K ash io ▁River ▁was ▁the ▁shall ow ▁ Ō f una ▁Est u ary ▁( 大 <0xE8> <0x88> <0xB9> 入 江 ), ▁which ▁existed ▁from ▁the ▁end ▁of ▁the ▁last ▁ice ▁age ▁to ▁about ▁ 3 0 0 ▁BC . ▁Sub sequently , ▁earth qu akes ▁caused ▁cr ust al ▁u pl ift , ▁which ▁cut ▁off ▁the ▁est u ary ▁from ▁the ▁bay , ▁making ▁it ▁into ▁a ▁flo od plain ▁with ▁the ▁K ash io ▁River ▁at ▁its ▁center . ▁As ▁the ▁river ▁often ▁flo oded , ▁it ▁formed ▁a ▁lake ▁that ▁left ▁behind ▁a ▁sw amp ▁as ▁it ▁dra ined . ▁The ▁early ▁lake ▁formed ▁in ▁the ▁flo od plain ▁of ▁the ▁K ash io ▁River ▁is ▁probably ▁the ▁lake ▁mentioned ▁in ▁the ▁En osh ima ▁Eng i , ▁a ▁history ▁of ▁the ▁area . ▁ ▁References ▁ ▁External ▁links ▁ ▁( mouth ) ▁ ▁Category : R ivers ▁of ▁Kan ag awa ▁Pref ect ure ▁Category : R ivers ▁of ▁Japan <0x0A> </s> ▁E o oph y la ▁p isc ator um ▁is ▁a ▁moth ▁in ▁the ▁family ▁Cr amb idae . ▁It ▁was ▁described ▁by ▁David ▁John ▁Lawrence ▁Ag ass iz ▁in ▁ 2 0 1 2 . ▁It ▁is ▁found ▁in ▁Ken ya . ▁ ▁The ▁wings pan ▁is ▁ 1 8 – 2 2   mm . ▁The