海蚀的

The sea cave in Scotland is especially interesting to note; known as Fingal's Cave.

苏格兰的海蚀洞穴——芬格洞穴特别有趣。

The hummocky cross bedding of the storm event deposits and the seismic micro-fractures and micro-corrugated laminations of the earthquake event deposits on the marine cliff add more beautiful matural patterns to it.

海蚀崖上的风蚨事件沉积的丘状交错层理及地震事件沉积的地震微断裂，微褶皱纹理等更给海蚀崖增添了自然优美的图案。

Marine cliff is a natural geologic section and abrasion platform can reflect the lithic structure and tectonin character of a certain rock formation.

海蚀崖 是一个天然的地质剖面，海蚀平台可以反映某一层岩性的结构，构造特征。

It is thought that the channel bay line evolution processes can be divided into four stages. The first stage is soon of the sea level stable when the bayhead mountines are eroded and developed abrasion geomorphy and the productive materials were transport into the bay deposition by the tidal current and wave current and were reworked into gravel dams. The second stage is characterized by the fluvial output sediments and eroded sediments mixed deposition in channel bay and developed marine accumulation plain and sand riges in the plain under the wave reworked. The third stage developed clay silt marine accumulation plain under the action of the channel current and the wave action is very limited. The fourth stage is marked by human being reclaim which result in the channel bay filled and evoluted into a strait arce coast.

文章认为，峡道海湾的充填经历了四个阶段，第一阶段以峡道海湾湾顶山体在波浪作用下产生的侵蚀物质充填为主，发育了海蚀崖、海蚀洞、海蚀穴等侵蚀地形和湾顶砂砾石堤等堆积地形交替的峡道湾顶地貌，第二阶段以河流输出物质和峡道湾岛屿、礁石侵蚀物质在潮流作用下向峡道湾输运，由潮流和波流共同沉积为特征，发育海积平原，部分粗颗粒泥沙在波浪的改造峡，发育平原沙堤，第三阶段以河流输出物质为主，在涨落潮流搬运下进入峡道和峡道湾沉积，在峡道湾中发育以淤泥质粉砂为主要物质的海积平原，第四阶段以人类围涂造田为标志，加速峡道湾的充填过程，使峡道海湾最终趋于夷平，形成顺直均衡的弧形海岸。

The southern part of Jin Island was being eroded by waves which led the head land was separared from the main rock to form sea stack called "Tiu Chung Rock". As the erosion proceeds, there is a 30m high long sea arch developed called "Tiu Chung Arch".

吊钟洲南面长期受著海浪拍打侵蚀，使岬角与岩体分离形成海蚀柱名为「吊钟岩」，因海浪持续的侵蚀，岩中续渐形成一个高30米的长形海蚀拱「吊钟洞」。

The rocks from Sharp Island are of volcanic origin. One of the examples is the rhyolite formed by viscous lava spewed from the volcano vents can be found near the caldera edge. The southern part of Jin Island was being eroded by waves which led the head land was separared from the main rock to form sea stack called "Tiu Chung Rock". As the erosion proceeds, there is a 30m high long sea arch developed called "Tiu Chung Arch".

桥咀洲的岩石大多源於火山，其中包括流纹岩，由附近火山喷道喷出的稠熔岩形成，属破火山口边的产物；吊钟洲南面长期受著海浪拍打侵蚀，使岬角与岩体分离形成海蚀柱名为「吊钟岩」，因海浪持续的侵蚀，岩中续渐形成一个高30米的长形海蚀拱「吊钟洞」。

The sight of "Banyang Stone Sail" is reputed as the most famous wonder in the world. Among other wonderful sights of sea modellings are Immortal's Well, Immortal Peak, Immortal Terrace, Immortal Cave and the mysterious Golden Guanyin.

景点&半洋石帆&被认为是世界上最著名的奇观，在其他的诸多精彩海蚀造型景点有仙人井，仙人峰，仙人台，仙人洞以及神秘莫测的金观音。

The movements of crustal movement to make the land sink, submerged in water, the formation of the continental shelf; sea hit the coast, resulting in wave-cut platforms, submerged underwater, but also the formation of the continental shelf.

地壳的升降运动使陆地下沉，淹没在水下，形成大陆架；海水冲击海岸，产生海蚀平台，淹没在水下，也能形成大陆架。

Dongtou country is one of fourteen island country in china, the marine-abrasion topography of the island coast is developed fully, especially the south coast and northeast coast form typical topography of wave-cut bridge and beach, majestic with the features of " wonderful island, clear water, beautiful reef, fine beach, fresh fish, excellent zoology".

洞头县是全国第十四个海岛县之一，岛岸海蚀地貌发育充分，尤其是各岛的南岸、东北岸形成的海蚀桥和沙滩等典型的海岸地貌，雄伟壮观，具有&岛奇、水清、礁美、滩佳、鱼鲜、生态优&的特点。

Along the southeastern coast of Jiangkou Office for the alluvial plain or marine plain and sea and the landscape Harbor Island and the distribution.

东南部沿海沿出江口处为冲积平原或海积平原和海蚀地貌以及港湾和岛屿的分布。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。