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单词 Plate boundaries
释义

Plate boundaries

原声例句
当月 CNN 10 学生英语 2021年3月合集

The majority of all earthquakes and volcanoes happen along plate boundaries.

大多数地震和火山都发生在板块边界。

全球玩乐指南

It's a massive tectonic plate boundary and it splits Iceland literally in half.

这是一个巨大的构造板块边界,它将冰岛一分为二。

TED-Ed(视频版)

Iceland and Japan are near active volcanoes and tectonic plate boundaries, where magma rises up through the crust.

冰岛和日本靠近活火山和构造板块边界,岩浆从地壳上升起。

当月 CNN 10 学生英语

Now, Iceland sits on a tectonic plate boundary between the North Atlantic and Arctic Oceans, and that plate continually splits farther apart, pushing North America and Europe farther apart.

现在,冰岛位于北大西洋和北冰洋之间的构造板块边界上,该板块不断分裂,将北美和欧洲推得越来越远。

新东方优美短文背诵

The site of this destruction is another kind of plate boundary: a subduction zone. There one plate dives under the edge of another and is reincorporated into the mantle.

一块潜没的区域。在这里,一块板块潜没到另一板块的边缘之下并结合入地幔之中。

202329

Undersea Mountains: The Mid--Ocean Ridges Mid--ocean ridges, the longest mountain chains on Earth, are formed at divergent plate boundaries where two oceanic plates move apart.

海底山脉:大洋中脊 大洋中脊是地球上最长的山脉,形成于两个大洋板块分开的不同板块边界处。

202329

This heat drives the convection currents in the mantle, causing tectonic plates to move and interact, leading to the formation of volcanoes at certain plate boundaries.

这种热量驱动地幔中的对流,导致构造板块移动和相互作用,导致某些板块边界形成火山。

202329

Deep Ocean Trenches: The Subduction Zones In contrast to mid--ocean ridges, deep ocean trenches form at convergent plate boundaries, where one plate descends, or 'subducts, ' beneath another.

深海海沟:俯冲带 与洋中脊相反,深海海沟形成于会聚板块边界处,其中一个板块下降或“俯冲”到另一个板块下方。

中文百科

板块构造论 Plate tectonics

(重定向自Plate boundaries)
地球板块结构
现存于地表的板块
三种不同的板块边界
世界各板块边界详略图



                     张裂型板块边界
                     聚合型板块边界


                     错动型板块边界
 隐没带


30→ 相对于非洲板块的移动速度(mm/Y)
 Alps  造山带

板块构造论(又称板块构造假说板块构造学说板块构造学,总称「板块飘移」)是为了解释大陆漂移现象而发展出的一种地质学理论。该理论认为,地球的岩石圈是由板块拼合而成;全球分为六大板块(1968年法国勒皮雄划分),海洋和陆地的位置是不断变化的。根据这种理论,地球内部构造的最外层分为两部分:外层的岩石圈和内层的软流圈。这种理论基于两种独立的地质观测结果:海底扩张和大陆漂移。

岩石圈可以分为大板块及小板块,两板块相接触的部份则可依其相对运动来分为分离板块边缘、聚合板块边缘及转形断层。在板块边缘常会出现地震、火山、造山运动及海沟。每年的相对运动距离约在0至100 mm不等。

英语百科

Plate tectonics 板块构造论

(重定向自Plate boundaries)
The tectonic plates of the world were mapped in the second half of the 20th century.
Remnants of the Farallon Plate, deep in Earth's mantle. It is thought that much of the plate initially went under North America (particularly the western United States and southwest Canada) at a very shallow angle, creating much of the mountainous terrain in the area (particularly the southern Rocky Mountains).
Three types of plate boundary.
Plate motion based on Global Positioning System (GPS) satellite data from NASA JPL. The vectors show direction and magnitude of motion.

Plate tectonics (from the Late Latin tectonicus, from the Greek:τεκτονικός "pertaining to building") is a scientific theory that describes the large-scale motion of Earth's lithosphere. This theoretical model builds on the concept of continental drift which was developed during the first few decades of the 20th century. The geoscientific community accepted plate-tectonic theory after seafloor spreading was validated in the late 1950s and early 1960s.

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更新时间:2025/6/18 8:40:31