
There are signs that a huge part of East Africa is starting to break away from the African continent.
有迹象表明,东非的一大片地区正开始从非洲大陆分离出去。
Geologists (people who study the Earth and its land and rocks) studied a deep crack that runs along a large part of Zambia.
地质学家(研究地球、陆地和岩石的人)研究了一条贯穿赞比亚大部分地区的深裂缝。
The crack is called a rift.
这条裂缝被称为“裂谷”。
It is a major fault in the rock that covers Earth's surface.
它是覆盖地球表面的岩层中的一条主要断层。
Geologist Mike Daly of the University of Oxford is studying Zambia's Kafue Rift.
来自University of Oxford的地质学家Mike Daly正在研究赞比亚的卡富埃裂谷。
He believes there is activity in the rift that suggests a giant piece of land is breaking away.
他认为,裂谷中的活动表明一大片陆地正在分离。
He wrote: "There is evidence that the fault boundary of the Kafue Rift is active and therefore the Southwest African Rift Zone is too."
他写道:“有证据表明,卡富埃裂谷的断层边界是活跃的,因此西南非裂谷带也是活跃的。”
He warned that this "may be an early indication of the break-up of sub-Saharan Africa".
他警告说,这“可能是撒哈拉以南非洲分裂的早期迹象”。
The land on Earth is constantly moving.
地球上的陆地一直在不断移动。
Three hundred million years ago, there was just one huge supercontinent.
三亿年前,地球上只有一个巨大的超级大陆。
It was called Pangea.
它被称为“盘古大陆”。
Over millions of years, Pangea broke up.
经过数百万年,盘古大陆逐渐分裂。
Giant areas of land slowly moved across the oceans to form the continents we know today.
巨大的陆地区域缓慢穿越海洋,形成了我们今天所知道的各大洲。
This movement is called continental drift.
这种运动被称为“大陆漂移”。
Rifts are one reason why land masses split apart.
裂谷是大陆板块分裂的原因之一。
The Kafue Rift in Zambia is part of a 2,500-kilometre-long rift zone stretching from Tanzania to Namibia.
赞比亚的卡富埃裂谷是一个长达2500公里裂谷带的一部分,该裂谷带从坦桑尼亚延伸至纳米比亚。
The rift is moving at a rate of about 4.7 mm per year.
该裂谷正以每年约4.7毫米的速度移动。
At this rate, it will take millions of years for Africa to split in two.
按照这个速度,非洲大陆需要数百万年才会分裂成两部分。
Scientists believe that in 200 million years from now, there could be just one supercontinent again.
科学家认为,在两亿年之后,地球可能又会重新形成一个超级大陆。
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