磨山,坐落于武汉市武昌东湖之滨。它东、北、西三面环水,形如半岛伸入于东湖之中。它近正东西走向,长仅千米有余,海拔百米左右,但它耸立于万顷碧波之上,仍显得巍峨挺拔。山下,湖光潋滟;山上,草木葱葱;湖光山色,相映生辉,是闻名遐迩的风景胜地。磨山,还是大地沧桑巨变的见证。沿新建的环山公路盘旋而上,到处都可看到地壳运动,海陆变迁的形迹。浅海中形成的岩石磨山的岩石层层相叠,有典型层理构造。岩层明显地分为上下两部分,分别形成于两个不同的地质时代。下部是志留系的页岩和砂岩。页岩浅黄或浅黄绿色,泥质,结构致密而硬度很小,极易破碎成碎片,散落于岩 Moshan, located in Wuchang, Wuhan City, East Lake. It is east, north, west water on three sides, shaped like a peninsula into the East Lake. It is nearly east-west direction, more than kilometers long, about 100 meters above sea level, but it stands on the vast expanse of blue waves, still appears towering tall and straight. Yamashita, lagoon 滟 滟; mountains, plants and lush; lakes and mountains, matched Shenghui, is the world famous scenic spots. Moshan, or witness the vicissitudes of the earth. Along the newly built ring road around the mountain, everywhere you can see the crustal movement, the traces of land and sea changes. Rock formations in the shallow sea are overlain by layers of rock with typical bedding structures. Rock formation is clearly divided into two parts, respectively, formed in two different geological times. The lower part is the Silurian shale and sandstone. Shale light yellow or light yellow-green, muddy, dense structure and hardness is very small, easily broken into pieces, scattered in the rock