.  Scattered around the globe are more than 100 small regions of isolated volcanic activity known to geologists as hot spots. Unlike most of the world's volcanoes, they are not always found at the boundaries of the great drifting plates that make up the earth's surface; on the contrary, many of them lie deep in the interior of a plate. Most of the hot spots move only slowly, and in some cases the movement of the plates past them has left trails of dead volcanoes. The hot spots and their volcanic trails are milestones that mark the passage of the plates.
    That the plates are moving is not beyond dispute. Africa and South America, for example, are moving away from each other as new material is injected into the sea floor between them. The complementary coastlines and certain geological features that seem to span the ocean are reminders of where the two continents were once joined. The relative motion of the plates carrying these continents has been constructed in detail, but the motion of one plate with respect to another cannot readily be translated into motion with respect to the earth's interior. It is not possible to determine whether both continents are moving in opposite directions or whether one continent is stationary and the other is drifting away from it. Hot spots, anchored in the deeper layers of the earth, provide the measuring instruments needed to resolve the question. From an analysis of the hot spot population it appears that the African plate is stationary and that it has not moved during the past 30 million years.
    The significance of hot spots is not confined to their role as a frame of reference. It now appears that they also have an important influence on the geophysical processes that propel the plates across the globe. When a continental plate comes to rest over a hot spot, the material rising from deeper layer creates a broad dome. As the dome grows, it develops seed fissures (cracks); in at least a few cases the continent may break entirely along some of these fissures, so that the hot spot initiates the formation of a new ocean. Thus just as earlier theories have explained the mobility of the continents, so hot spots may explain their mutability (inconstancy).25.  The author believes that ______.
【正确答案】 B
【答案解析】 从文章第1段的内容可知,地球上散布着一百多个热点;大多数的热点独自缓慢运动,某些情况下,经过这些热点的板块运动留下死火山的痕迹;热点及其火山痕迹是标志板块迁移的符号。从文章第2段的内容可知,如今,有关板块在运动的理论已经无可争辩;然后举例进一步说明。从文章最后一段内容可知,热点的重要性并不仅限于作为参照体系这一作用上;现在看来,它们对推动板块在地球上移动的地球物理过程也产生了重大影响;因此,正如早期的理论解释了大陆的移动那样,热点或许可以解释大陆的不稳定性。据此可知,作者认为有关大陆移动的理论是正确的。B项与文中的意思相符,因此B项为正确答案。
[参考译文] 地球上散布着一百多个相互独立并且面积不大的火山活动区,地质学家称之为“热点”。和世界上的大多数火山不同,它们不都位于形成地球表面的巨大漂移板块的连接点,反而有很多藏于板块的深处。大部分热点区移动极其缓慢,有时候,板块滑过这些热点区,便留下死火山的痕迹。热点区加上其火山痕迹是板块移动的象征。
   板块漂移学说如今已无可争辩。例如非洲和南美洲,因为有新物质注入它们之间的洋底,这两个大陆距离愈来愈远。即使远隔大洋,可相互吻合的海岸线和似乎跨越海洋的地质特征,均会让人想到这两个大陆曾是相连的。带着两个大陆漂移的板块做相对运动,这已得到具体解释,但不能把一个板块相对于另一板块的运动简单地解释为板块与地球内部之间的运动。由于人们还没法肯定两个大陆是在朝相反的方向运动,还是一个大陆原地不动,而另一个大陆正在远它而去,因而位于地壳深处的热点区提供了解决这一问题的测量仪。热点密度的分析显示,非洲板块静止不动了3000万年。
   热点区的重要意义并不仅仅在于它们所起到的参照物的作用。如今它们还对推动板块在地球表面漂移这一地球物理进程有重要作用。当大陆板块漂移到热点区上方时,由地壳深处涌出的物质便会使板块凸起,形成巨大圆丘。随着圆丘不断增长,板块出现深深的裂痕。在某些情况下,大陆至少可能会沿着这样一些裂缝完全分裂。因而,热点区便形成了一个新海洋。正如早些时候的一些理论已经解释了大陆的移动一样,热点理论或许能对大陆板块的不稳定性加以说明。