一、滁河的历史概况滁河是长江下游的一条支流,源起古庐州旧梁县蜃母池(即今安徽省肥东县梁园),东南入全椒界,又入含山,再经和州(即和县)复入全椒,东北流入滁州境与江浦以河为界,又北入江浦界至六合出瓜埠口入于江。滁河古称涂水,至唐代改涂为滁。民间名称亦多, 有古河或全河、后河或前河之称。《方舆记要·江南大川篇》称瓦梁河。滁河干线河谷宽阔,纵坡平缓,两侧阶地约束。下游土质沙,且受江潮影响,河床多湾。瓜埠口外大江古称黄天荡。自明天启年间(公元1621～1627年)泥沙淤积成长洲,因长期排水等影响,瓜埠以下入江已成四口。而今长洲分为玉带和龙袍二圩,原瓜埠 First, the Chuhe historical overview Chuhe is a tributary of the lower reaches of the Yangtze River, originating from the ancient Lu Mirage Lao Mirage pool (now Feiyang County, Anhui Province Liang Garden), southeast into the whole industry, into the mountains, and then by And state (ie County) into Quanjiao, northeast flows into Chuzhou territory and Jiangpu to the river as the boundary, and north into the Jiang Pu boundary to the Luhe out of the melon port into the river. Chuhe ancient name Tu water, to the Tang Dynasty Tu Chu Chu. Folk name is also more, there are ancient river or river, after the river or former river. “Party press to Jiangnan Okawa articles” said Waring River. Chuhe River valley broad, gentle slope, both sides of the terrace constraints. Downstream soil quality sand, and by the impact of the river tide, more than a bay bed. Guabu mouth outside the river known as the Huang Dang swing. Since the beginning of the Ming dynasty (AD 1621 ~ 1627) sedimentation siltation Changzhou, due to the impact of long-term drainage, the following Kuabu into the river has become four. Now Cheung Chau is divided into two jade belt and robes, the original Kuabu