avalanche debris cone

简明释义

1. 倒石堆; 2. 岩崩锥;

英英释义

例句

1.The avalanche debris cone was a clear indicator of the mountain's unstable conditions.

这个雪崩残骸锥体清楚地表明了山体的不稳定状况。

2.Geologists study the formation of an avalanche debris cone to understand past avalanche activity.

地质学家研究雪崩残骸锥体的形成以了解过去的雪崩活动。

3.After the storm, the avalanche debris cone became a popular spot for photographers.

暴风雪过后，雪崩残骸锥体成为摄影师的热门拍摄地点。

4.The ski patrol marked the area near the avalanche debris cone for safety reasons.

滑雪巡逻队出于安全原因标记了靠近雪崩残骸锥体的区域。

5.Hikers should be cautious when crossing an avalanche debris cone after a recent snowfall.

徒步旅行者在最近降雪后穿越雪崩残骸锥体时应保持谨慎。

作文

In the realm of geology and natural hazards, understanding the dynamics of snow and rock movement is crucial. One significant phenomenon that captures the attention of researchers and outdoor enthusiasts alike is the avalanche. An avalanche is a rapid flow of snow, ice, and debris down a slope, often triggered by various factors such as weather conditions, terrain, and human activity. When an avalanche occurs, it can lead to the formation of what is known as an avalanche debris cone, a term that refers to the accumulation of snow, ice, and other materials at the base of a slope where the avalanche has descended. The avalanche debris cone (雪崩碎屑锥) is not just a random pile of snow; it is a structured deposit that provides insights into the characteristics of the avalanche itself.The formation of an avalanche debris cone begins with the initial release of snow and debris from a slope. As the avalanche cascades downwards, it picks up additional material, including rocks, trees, and other vegetation, which become part of the debris flow. When the avalanche reaches the bottom of the slope, the energy dissipates, causing the materials to settle and form a cone-shaped deposit. This shape is influenced by several factors, including the angle of the slope, the volume of material involved, and the speed of the avalanche. Studying avalanche debris cones is essential for understanding past avalanche activity and assessing potential risks in mountainous regions. Geologists and scientists often analyze these deposits to determine the frequency and magnitude of past avalanches, which can inform future hazard assessments. For instance, a large and well-defined avalanche debris cone may indicate a history of significant avalanche events in that area, prompting local authorities to implement safety measures for residents and visitors.Moreover, avalanche debris cones can have ecological implications as well. The materials deposited can alter the landscape, affecting the growth of vegetation and the habitats of local wildlife. The nutrient-rich debris can create fertile ground for new plant life, while the physical changes to the terrain can influence animal movement and behavior. Understanding these ecological impacts is vital for conservation efforts and land management in avalanche-prone areas.In addition to their scientific importance, avalanche debris cones also serve as a reminder of the power of nature. They illustrate the forces at play in mountainous environments and the potential dangers they pose to those who venture into these areas. Skiers, hikers, and mountaineers must be aware of the risk of avalanches and the significance of avalanche debris cones when planning their activities. Knowledge of these features can help individuals make informed decisions about their safety and the safety of others.In conclusion, the study of avalanche debris cones is a multifaceted field that encompasses geology, ecology, and safety awareness. As we continue to explore and understand the natural world, recognizing the significance of these formations will enhance our ability to navigate and appreciate the beauty and power of mountainous landscapes. By acknowledging the role of avalanche debris cones in both natural processes and human activities, we can foster a deeper respect for the environment and its inherent risks.

在地质学和自然灾害的领域中，理解雪和岩石运动的动态是至关重要的。一个引起研究人员和户外爱好者关注的重要现象是雪崩。雪崩是雪、冰和碎屑沿斜坡快速流动的现象，通常由天气条件、地形和人类活动等多种因素触发。当雪崩发生时，会导致形成所谓的avalanche debris cone（雪崩碎屑锥），这个术语指的是在雪崩下降的斜坡底部积累的雪、冰和其他材料。avalanche debris cone（雪崩碎屑锥）并不是随意堆积的雪；它是一个结构化的沉积物，提供了对雪崩特征的深入了解。avalanche debris cone（雪崩碎屑锥）的形成始于斜坡上雪和碎屑的初步释放。当雪崩向下滑落时，它会拾取额外的材料，包括岩石、树木和其他植被，这些都成为碎屑流的一部分。当雪崩到达斜坡底部时，能量消散，导致这些材料沉降并形成一个锥形沉积物。这个形状受到多个因素的影响，包括斜坡的角度、涉及的材料体积和雪崩的速度。研究avalanche debris cones（雪崩碎屑锥）对理解过去的雪崩活动和评估山区潜在风险至关重要。地质学家和科学家通常分析这些沉积物，以确定过去雪崩的频率和强度，这可以为未来的危险评估提供参考。例如，一个大型且轮廓分明的avalanche debris cone（雪崩碎屑锥）可能表明该地区有显著雪崩事件的历史，促使当地当局对居民和游客实施安全措施。此外，avalanche debris cones（雪崩碎屑锥）也可能具有生态意义。沉积的材料可以改变地形，影响植被的生长和当地野生动物的栖息地。富含营养的碎屑可以为新植物生命创造肥沃的土壤，而地形的物理变化可以影响动物的移动和行为。理解这些生态影响对于雪崩频发地区的保护工作和土地管理至关重要。除了科学的重要性，avalanche debris cones（雪崩碎屑锥）也提醒我们自然的力量。它们展示了山区环境中作用的力量以及它们对那些进入这些区域的人们可能构成的危险。滑雪者、徒步旅行者和登山者必须意识到雪崩的风险以及在计划活动时avalanche debris cones（雪崩碎屑锥）的重要性。了解这些特征可以帮助个人做出关于自身及他人安全的明智决策。总之，avalanche debris cones（雪崩碎屑锥）的研究是一个多方面的领域，涵盖了地质学、生态学和安全意识。随着我们继续探索和理解自然世界，认识到这些形成物的重要性将增强我们在山区景观中导航和欣赏美丽与力量的能力。通过承认avalanche debris cones（雪崩碎屑锥）在自然过程和人类活动中的角色，我们可以培养对环境及其固有风险的更深尊重。