Alpine orogeny

简明释义

阿尔卑斯造山运动;

英英释义

例句

1.Geologists study the Alpine orogeny to understand mountain-building processes better.

地质学家研究阿尔卑斯造山运动以更好地理解造山过程。

2.Many features of the European landscape can be traced back to the effects of the Alpine orogeny.

欧洲景观的许多特征可以追溯到阿尔卑斯造山运动的影响。

3.The Alpine orogeny was a significant event in the geological history of Europe.

阿尔卑斯造山运动是欧洲地质历史上的一个重要事件。

4.The rocks found in the Alps provide evidence of the Alpine orogeny that occurred millions of years ago.

阿尔卑斯山发现的岩石提供了数百万年前发生的阿尔卑斯造山运动的证据。

5.The formation of the Alps is primarily attributed to the processes involved in the Alpine orogeny.

阿尔卑斯山的形成主要归因于阿尔卑斯造山运动中涉及的过程。

作文

The term Alpine orogeny refers to a significant geological event that took place during the late Mesozoic and early Cenozoic eras, resulting in the formation of mountain ranges, particularly in Europe and Asia. This orogeny is characterized by the collision of tectonic plates, which led to the uplift of the Alps and other connected mountain systems. Understanding the Alpine orogeny is crucial for geologists as it provides insights into the processes that shape our planet's surface. The collision between the African and Eurasian plates initiated this dramatic transformation, causing extensive folding, faulting, and volcanic activity in the region. As these plates converged, they created immense pressure that altered the existing rock formations, leading to the rise of new mountains and the reshaping of the landscape.Geologically, the Alpine orogeny is not just about the physical elevation of land; it also involves a complex interplay of various geological processes. For instance, sedimentation occurred in the foreland basins, where sediments accumulated over millions of years before being thrust upwards during the orogeny. This process has left behind a rich record of sedimentary rocks that tell the story of Earth's history. Additionally, the Alpine orogeny significantly influenced the climate in the region, creating barriers that altered wind and precipitation patterns. This climatic shift has had lasting effects on the biodiversity and ecosystem development in the surrounding areas.The implications of the Alpine orogeny extend beyond geology; they also affect human activities. The Alps, as a direct result of this orogenic event, have become a vital area for tourism, agriculture, and even hydroelectric power generation. The unique landscapes formed by the orogeny attract millions of visitors each year, contributing to local economies. Furthermore, understanding the geological history of the Alps can inform future developments, especially in terms of natural disaster preparedness. Given that the region is prone to landslides and avalanches, knowledge derived from the Alpine orogeny can aid in creating safer infrastructures.In conclusion, the Alpine orogeny represents a pivotal moment in Earth's geological history, marked by the dramatic uplift of mountain ranges due to tectonic plate interactions. Its study not only enhances our understanding of geological processes but also informs various aspects of human life, from environmental management to economic development. The legacy of the Alpine orogeny is evident in the breathtaking landscapes we see today, serving as a reminder of the dynamic nature of our planet and the forces that continue to shape it.

“阿尔卑斯造山运动”是指发生在中生代晚期和新生代早期的一个重要地质事件，导致了山脉的形成，特别是在欧洲和亚洲。这个造山运动的特征是构造板块的碰撞，导致阿尔卑斯山和其他相连山系的隆起。理解“阿尔卑斯造山运动”对地质学家至关重要，因为它提供了关于塑造我们星球表面的过程的见解。非洲板块与欧亚板块的碰撞引发了这一戏剧性的变化，造成了该地区的广泛褶皱、断层和火山活动。随着这些板块的汇聚，产生了巨大的压力，改变了现有的岩石构造，导致新山的崛起和地形的重塑。从地质学角度来看，“阿尔卑斯造山运动”不仅仅是土地的物理升高；它还涉及多种地质过程的复杂相互作用。例如，沉积作用发生在前缘盆地，沉积物在数百万年间积累，然后在造山运动期间被推升。这一过程留下了丰富的沉积岩记录，讲述了地球历史的故事。此外，“阿尔卑斯造山运动”显著影响了该地区的气候，形成了改变风和降水模式的屏障。这一气候变化对周围地区的生物多样性和生态系统发展产生了持久影响。“阿尔卑斯造山运动”的影响超越了地质学，它们也影响着人类活动。阿尔卑斯山作为这一造山事件的直接结果，已成为旅游、农业甚至水电发电的重要区域。由造山运动形成的独特景观每年吸引数百万游客，为当地经济做出了贡献。此外，了解阿尔卑斯山的地质历史可以为未来的发展提供信息，特别是在自然灾害准备方面。考虑到该地区容易发生山体滑坡和雪崩，从“阿尔卑斯造山运动”获得的知识可以帮助创建更安全的基础设施。总之，“阿尔卑斯造山运动”代表了地球地质历史中的一个关键时刻，其特征是由于构造板块相互作用而导致的山脉剧烈隆起。它的研究不仅增强了我们对地质过程的理解，还为人类生活的各个方面提供了信息，从环境管理到经济发展。“阿尔卑斯造山运动”的遗产在我们今天看到的令人叹为观止的景观中显而易见，提醒我们我们星球的动态性质及其持续塑造的力量。