geyserite

简明释义

英[ˈɡiːzəraɪt]美[ˈɡaɪzəˌraɪt]

n. [矿物] 硅华，间歇泉周围的沉积物

英英释义

单词用法

同义词

反义词

例句

1.The fact that the geyserite Cs-deposit is discovered only in Tibet has relation with the modern tectogenetic movement of the Tibet plateau by all appearances.

为什么硅华铯矿目前仅在青藏高原发现，别的地方尚未见报导，显然跟青藏高原在近期的构造运动有关。

2.The geyserite Cs-deposit is discovered in Tibet.

硅华铯矿在青藏高原发现。

3.The fact that the geyserite Cs-deposit is discovered only in Tibet has relation with the modern tectogenetic movement of the Tibet plateau by all appearances.

为什么硅华铯矿目前仅在青藏高原发现，别的地方尚未见报导，显然跟青藏高原在近期的构造运动有关。

4.Geologists study geyserite to understand the history of volcanic activity.

地质学家研究间歇泉矿以了解火山活动的历史。

5.The unique formations of geyserite highlight the geothermal activity in the area.

独特的间歇泉矿形态突显了该地区的地热活动。

6.The bright colors of geyserite can indicate different mineral compositions.

不同矿物成分的间歇泉矿可以显示出鲜艳的颜色。

7.After the eruption, new layers of geyserite formed quickly in the basin.

喷发后，盆地中迅速形成了新的间歇泉矿层。

8.Visitors to the national park were amazed by the large deposits of geyserite around the hot springs.

国家公园的游客对温泉周围的大量间歇泉矿沉积物感到惊讶。

作文

Geysers are one of nature's most fascinating phenomena, captivating the attention of scientists and tourists alike. They are natural hot springs that intermittently spout jets of steam and hot water into the air. One of the intriguing byproducts of geyser activity is a mineral called geyserite, which is formed from the deposition of silica and other minerals as the hot water cools. Understanding geyserite not only deepens our appreciation for geothermal systems but also provides insights into the geological processes that shape our planet.When we think of geysers, many people picture iconic locations such as Yellowstone National Park in the United States. Here, the Old Faithful geyser erupts regularly, attracting thousands of visitors each year. However, what many may not realize is that the area surrounding these geysers is often rich in geyserite. This soft, white or grayish mineral can be found in various forms, including sinter deposits and silica formations. The process of geyserite formation begins when geothermal water rises to the surface, carrying dissolved silica. As the water reaches the cooler surface, the silica precipitates out, leading to the accumulation of this unique mineral.The presence of geyserite serves as a valuable indicator of past geothermal activity. By studying these deposits, geologists can reconstruct the history of geyser fields and understand how they have changed over time. This information is crucial for predicting future geothermal activity and assessing the potential for harnessing geothermal energy. In regions where geysers are prevalent, geyserite can also play a role in the local ecosystem, influencing plant growth and habitat conditions.Moreover, geyserite has practical applications beyond its geological significance. For instance, it is sometimes used in the production of ceramics and glass due to its high silica content. Artists and craftsmen may incorporate geyserite into their work, creating unique pieces that reflect the beauty of geothermal landscapes. Additionally, the study of geyserite can contribute to our understanding of silica-rich environments, which is essential in various industrial processes.In summary, the mineral geyserite is a remarkable product of geothermal activity, offering insights into both the natural world and human industry. As we continue to explore and appreciate the wonders of geysers, it is important to recognize the role of geyserite in this dynamic system. Whether through scientific research or artistic expression, geyserite remains a testament to the intricate connections between geology, ecology, and culture. By fostering a deeper understanding of this mineral, we can better appreciate the natural processes that shape our environment and the resources that emerge from them.

间歇泉是大自然最迷人的现象之一，吸引着科学家和游客的注意。它们是自然热泉，间歇性地喷出蒸汽和热水的喷射。间歇泉活动的一个有趣副产品是称为geyserite的矿物，它是由二氧化硅和其他矿物在热水冷却时沉积而形成的。理解geyserite不仅加深了我们对地热系统的欣赏，还提供了对塑造我们星球的地质过程的深入见解。当我们想到间歇泉时，许多人会想到美国黄石国家公园等标志性地点。在这里，老忠实间歇泉定期喷发，每年吸引成千上万的游客。然而，许多人可能没有意识到，这些间歇泉周围的地区通常富含geyserite。这种柔软的白色或灰色矿物可以以各种形式存在，包括沉积物和二氧化硅的形成。geyserite的形成过程始于地热水上升到表面，携带溶解的二氧化硅。当水到达较冷的表面时，二氧化硅沉淀出来，导致这种独特矿物的积累。geyserite的存在作为过去地热活动的宝贵指示。通过研究这些沉积物，地质学家可以重建间歇泉区域的历史，了解它们随时间的变化。这些信息对于预测未来的地热活动和评估开发地热能源的潜力至关重要。在间歇泉盛行的地区，geyserite也可能在当地生态系统中发挥作用，影响植物生长和栖息条件。此外，geyserite在其地质重要性之外还有实际应用。例如，由于其高二氧化硅含量，有时用于陶瓷和玻璃的生产。艺术家和工匠可能会将geyserite融入他们的作品中，创造出反映地热景观之美的独特作品。此外，对geyserite的研究可以帮助我们理解富含二氧化硅的环境，这对于各种工业过程至关重要。总之，矿物geyserite是地热活动的显著产物，提供了对自然世界和人类工业的见解。当我们继续探索和欣赏间歇泉的奇迹时，认识到geyserite在这一动态系统中的作用是非常重要的。无论是通过科学研究还是艺术表达，geyserite仍然是地质、生态和文化之间复杂联系的证明。通过加深对这种矿物的理解，我们可以更好地欣赏塑造我们环境的自然过程以及从中产生的资源。