dripstone

简明释义

英[ˈdrɪpˌstoʊn]美[ˈdrɪpˌstoʊn]

n. [建] 滴水石；石笋

英英释义

单词用法

同义词

反义词

例句

1.There is a small broken dripstone formation near the entrance.

入口附近有一个小的破滴水石。

2.There is a small broken dripstone formation near the entrance.

入口附近有一个小的破滴水石。

3.The cave was adorned with beautiful dripstone, which formed over thousands of years.

这个洞穴装饰着美丽的滴水石，它们经过数千年的形成。

4.During our spelunking trip, we marveled at the stunning dripstone formations hanging from the ceiling.

在我们的洞穴探险中，我们惊叹于从天花板上悬挂的壮观滴水石形态。

5.The dripstone in the grotto resembled a frozen waterfall.

洞穴中的滴水石看起来像是一座冰冻的瀑布。

6.Geologists study dripstone to understand the history of water flow in caves.

地质学家研究滴水石以了解洞穴中水流的历史。

7.The dripstone formations created a magical atmosphere in the underground chamber.

这些滴水石形态在地下室内营造出一种神奇的氛围。

作文

Dripstone formations are one of nature's most fascinating geological wonders. These structures, often found in caves, are primarily made of calcium carbonate and result from the slow dripping of mineral-rich water over time. The process begins when rainwater absorbs carbon dioxide from the atmosphere and soil, forming a weak carbonic acid solution. As this acidic water seeps through the ground and into caves, it dissolves limestone, a sedimentary rock composed mainly of calcium carbonate. When this water drips from the ceiling of a cave, it leaves behind deposits of calcium carbonate, which accumulate over thousands of years to create stunning features known as dripstone (滴水石). The two main types of dripstone (滴水石) formations are stalactites and stalagmites. Stalactites hang from the ceiling of caves, resembling icicles, while stalagmites grow upward from the cave floor. The formation of these structures is a slow process, with some stalactites and stalagmites growing only a few centimeters over a century. This gradual buildup is what makes them so unique and beautiful. Visitors to caves are often awestruck by the intricate shapes and sizes of dripstone (滴水石) formations, which can range from delicate, thin strands to massive columns that reach the height of the cave itself. One of the most famous cave systems known for its spectacular dripstone (滴水石) formations is Carlsbad Caverns in New Mexico, USA. This national park features over 119 caves, with the main cavern showcasing an impressive array of stalactites and stalagmites. The sheer scale and beauty of these formations draw tourists from all over the world, eager to witness the natural artistry created by the slow passage of time. In addition to their aesthetic appeal, dripstone (滴水石) formations also provide valuable insights into the geological history of our planet. Scientists study these formations to understand past climate conditions, as the rate of deposition can indicate changes in temperature and precipitation over millennia. Furthermore, the presence of certain minerals within dripstone (滴水石) can reveal information about the surrounding environment and the processes that shaped it. Protecting these natural wonders is crucial, as they are sensitive to environmental changes and human activity. Pollution, changes in water flow, and even the mere presence of visitors can impact the delicate balance required for dripstone (滴水石) growth. Conservation efforts in various regions aim to preserve these unique ecosystems, ensuring that future generations can appreciate the beauty and significance of dripstone (滴水石) formations. In conclusion, dripstone (滴水石) formations are not only breathtaking natural sculptures but also vital indicators of geological and environmental history. Their slow formation process teaches us about patience and the power of nature to create beauty over time. As we continue to explore and learn from these magnificent structures, it is essential to prioritize their conservation, allowing us to cherish and protect the wonders of the earth for years to come.

滴水石（dripstone）是自然界中最迷人的地质奇观之一。这些结构通常出现在洞穴中，主要由碳酸钙构成，源于富含矿物质的水缓慢滴落的过程。这个过程开始于雨水从大气和土壤中吸收二氧化碳，形成一种弱碳酸溶液。当这种酸性水渗透到地下并进入洞穴时，它会溶解石灰岩，这是一种主要由碳酸钙组成的沉积岩。当这水滴落在洞穴的天花板上时，它留下了碳酸钙的沉积物，这些沉积物经过数千年的积累，形成了被称为滴水石（dripstone）的惊人特征。 滴水石（dripstone）形成的两种主要类型是钟乳石和石笋。钟乳石悬挂在洞穴的天花板上，形状像冰柱，而石笋则向上生长，从洞穴地面向上延伸。这些结构的形成是一个缓慢的过程，一些钟乳石和石笋在一个世纪内只增长几厘米。这种逐渐的积累使它们变得独特而美丽。访问洞穴的游客常常对滴水石（dripstone）形成的复杂形状和大小感到惊叹，这些结构可以从细腻的细丝到高达洞穴本身高度的巨大柱子不等。 美国新墨西哥州的卡尔斯巴德洞穴国家公园是以其壮观的滴水石（dripstone）形成而闻名的最著名的洞穴系统之一。这个国家公园拥有119个以上的洞穴，主洞展示了一系列令人印象深刻的钟乳石和石笋。这些结构的规模和美丽吸引了来自世界各地的游客，渴望见证时间缓慢流逝所创造的自然艺术。 除了其美学吸引力外，滴水石（dripstone）形成还提供了对我们星球地质历史的宝贵见解。科学家研究这些形成，以了解过去的气候条件，因为沉积速率可以指示千年来温度和降水的变化。此外，滴水石（dripstone）中的某些矿物的存在可以揭示周围环境及其形成过程的信息。 保护这些自然奇观至关重要，因为它们对环境变化和人类活动非常敏感。污染、水流变化，甚至游客的存在都可能影响滴水石（dripstone）生长所需的微妙平衡。各地区的保护工作旨在保护这些独特的生态系统，确保未来的世代能够欣赏到滴水石（dripstone）形成的美丽和重要性。 总之，滴水石（dripstone）形成不仅是令人惊叹的自然雕塑，而且是地质和环境历史的重要指示器。它们缓慢的形成过程教会我们耐心和自然创造美的力量。随着我们继续探索和学习这些壮丽的结构，优先考虑它们的保护至关重要，让我们能够珍惜和保护地球的奇观，直到未来的岁月。