江都区 topographic map

苏州的地貌特征以平缓平原为主，全市的地势低平，太湖水网平原可分为河网冲积—堆积高亢平原、低洼湖荡平原、平坦水网化平原、滨湖圩田平原。全市自西向东缓慢倾斜，平原的海拔高度3—4米，阳澄湖和吴江一带仅2米左右。低山丘陵零星散布，一般高100—300米，分布在西部山区和太湖诸岛，其中以穹窿山最高（341米），此外比较著名的还有洞庭山缥缈峰（336米）、洞庭山莫里峰（293米）、南阳山（338米）、七子山（294米）、天平山（201米）、灵岩山（182米）、虞山（261米）、潭山（252米）、渔洋山（170米）等。主要山体沿太湖呈东北—西南走向，构成七子山—东洞庭山，穹隆山—渔洋山—长沙岛—西洞庭山，邓尉山—潭山—漫山岛，…

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境内地势平坦，海拔2.5-5.2米，属亚热带季风气候。年平均气温15℃，日照2250小时，无霜期230天左右。海门区年平均降水量1040.4毫米，年平均蒸发量1282.0毫米。

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徐州地处黄淮平原中部，属北方与南方的过渡地带，四周环山，平原、丘陵相间，属江苏省内平均海拔较高的市。徐州有大洞山、泉山、皇姑山、拉犁山、云龙山、小泰山、卧牛山等山峰，其中主城区有72座山头。位于贾汪区北部的大洞山为全市海拔最高点。

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南京市地貌特征属宁镇扬丘陵地区。其中，低山丘陵面积为4255.07平方千米、江河面积752.06平方千米、圩洲面积1589.88平方千米。从地形组成来看，低山占土地总面积的3.5%，丘陵占4.3%，岗地占53%，平原、洼地及河流湖泊占土地总面积的39.2%。长江从西南方向流入南京，在此折向东进入镇江。秦淮河、滁河分别从南北岸汇入长江:35-45。

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