The Jiaozhou bay is a tidal inlet of bedrock bay type, the typical flood and ebb tidal deltas are developed inside and outside the bay mouth, and the geomorphologic system in the bay is complete.
胶州湾属基岩海湾型潮汐通道，湾口内、外发育较为典型的涨、落潮流三角洲，地貌体系较为完整。
The obliquely inflowing current forms an asymmetric geomorphologic system in the tidal inlet, the tidal deltas are more developed on the east side of inner bay and on the northeast side of outer bay.
由于 水流的非正向入射，潮汐通道地貌 体系不对称，潮流三角洲在湾内东侧发育、在湾外东北侧发育。
It is also not suitable for the deposits formed in sedimentary environments such as firths, tidal zones and fluvial deltas.
在河口湾、潮间带和河流三角洲前缘环境中形成的沉积体也不适合进行构型单元分析。
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