back intermontane basin

简明释义

后山间盆地;

英英释义

A back intermontane basin refers to a geological feature that is a low-lying area situated between mountain ranges, typically formed by tectonic processes, where sediment can accumulate over time.

后间山盆地是指一种地质特征,它是位于山脉之间的低洼地区,通常由构造过程形成,在这里沉积物可以随着时间的推移而积累。

例句

1.Researchers studied the sediment layers in the back intermontane basin 后间山盆地 to understand its historical climate changes.

研究人员研究了back intermontane basin 后间山盆地中的沉积层,以了解其历史气候变化。

2.The geological survey revealed that the region was primarily a back intermontane basin 后间山盆地 formed during the late Miocene.

地质调查显示,该地区主要是一个在晚中新世形成的back intermontane basin 后间山盆地

3.The back intermontane basin 后间山盆地 serves as a crucial habitat for various endemic species.

back intermontane basin 后间山盆地是多种特有物种的重要栖息地。

4.During the field trip, we explored the unique geological features of the back intermontane basin 后间山盆地 which were formed by tectonic activities.

在实地考察中,我们探索了由构造活动形成的back intermontane basin 后间山盆地独特地质特征。

5.The hydrology of the back intermontane basin 后间山盆地 is influenced by both snowmelt and rainfall patterns.

back intermontane basin 后间山盆地的水文情况受到雪融水和降雨模式的影响。

作文

The term back intermontane basin refers to a geological feature that is typically found in mountainous regions. These basins are situated behind mountain ranges and are often characterized by their unique topography and sedimentary deposits. Understanding the formation and significance of back intermontane basins is essential for geologists and environmental scientists, as they play a crucial role in the study of Earth's history and ecology.Geologically, back intermontane basins are formed through a combination of tectonic activity, erosion, and sedimentation. As tectonic plates shift, they can create uplifted areas that form mountains. The regions behind these uplifted areas often experience subsidence, leading to the creation of basins. Over time, rivers and streams transport sediments into these basins, filling them with materials that can provide valuable insights into past environmental conditions.One of the most notable examples of a back intermontane basin is the Great Basin in the United States. This expansive area is surrounded by several mountain ranges, including the Sierra Nevada and the Wasatch Range. The Great Basin exhibits many characteristics typical of back intermontane basins, such as arid conditions and unique ecosystems. The study of this basin has revealed important information about climate change, water resources, and biodiversity.The ecological significance of back intermontane basins cannot be overstated. These areas often serve as critical habitats for various plant and animal species. The unique climatic conditions found within these basins can lead to the development of endemic species that are not found anywhere else. Additionally, back intermontane basins can act as natural reservoirs for water, making them vital for both wildlife and human populations.In terms of human impact, back intermontane basins can be both beneficial and detrimental. On one hand, they can provide fertile land for agriculture and support local economies. On the other hand, increased development and resource extraction in these areas can lead to habitat destruction and environmental degradation. It is crucial for policymakers and conservationists to understand the delicate balance that exists within these ecosystems.In conclusion, the term back intermontane basin encompasses a fascinating aspect of geology and ecology. These basins not only reveal the dynamic processes that shape our planet but also highlight the importance of preserving unique ecosystems. As we continue to study and explore these regions, we must remain mindful of our impact on the environment and strive to protect these vital landscapes for future generations.

back intermontane basin”这个术语指的是一种地质特征,通常在山区发现。这些盆地位于山脉的后面,通常以其独特的地形和沉积物特征而著称。理解back intermontane basin的形成及其重要性对于地质学家和环境科学家至关重要,因为它们在研究地球的历史和生态中发挥着关键作用。从地质角度来看,back intermontane basin是通过构造活动、侵蚀和沉积的组合形成的。当构造板块移动时,它们可以形成隆起的区域,形成山脉。这些隆起区域后面的地区往往经历沉降,导致盆地的形成。随着时间的推移,河流和溪流将沉积物运输到这些盆地中,使其充满材料,这些材料可以提供有关过去环境条件的重要信息。美国大盆地是back intermontane basin最显著的例子之一。这个广阔的地区被多个山脉环绕,包括内华达山脉和华达奇山脉。大盆地展现了许多典型的back intermontane basins特征,如干旱气候和独特的生态系统。对该盆地的研究揭示了有关气候变化、水资源和生物多样性的重要信息。back intermontane basins的生态意义不容小觑。这些地区常常作为各种植物和动物物种的关键栖息地。在这些盆地内发现的独特气候条件可以导致发展出仅在此处存在的特有物种。此外,back intermontane basins可以作为水的自然储存库,使其对野生动物和人类都至关重要。在人类影响方面,back intermontane basins既可以是有益的,也可能是有害的。一方面,它们可以为农业提供肥沃的土地,并支持地方经济。另一方面,这些地区的开发和资源开采增加可能导致栖息地破坏和环境退化。政策制定者和保护主义者必须理解这些生态系统中存在的微妙平衡。总之,术语back intermontane basin涵盖了地质和生态学中的一个迷人方面。这些盆地不仅揭示了塑造我们星球的动态过程,还突显了保护独特生态系统的重要性。随着我们继续研究和探索这些地区,我们必须时刻关注我们对环境的影响,并努力保护这些对未来世代至关重要的景观。

相关单词

intermontane

intermontane详解:怎么读、什么意思、用法

basin

basin详解:怎么读、什么意思、用法