salt glacier造句

• Salt glaciers on average may only advance a few meters per year.
• Salt glaciers may also leave behind features such as moraines.
• Salt domes and salt glaciers are a common feature of the Zagros Mountains.
• The Kuh-e-Namak salt glacier is located in southeast Iran.
• The sources of salt glaciers are salt deposits.
• The structure of a salt glacier is much like that of an ice glacier.
• If the rising salt diapir breaches the surface, it can become a flowing salt glacier.
• Salt glaciers move faster as precipitation increases; however too much precipitation may dissolve the salt.
• Piercing the overburden is crucial for salt glaciers to form, and can occur in three ways.
• Southern Iran hosts the majority of salt glaciers and the most active salt glacier in the world.
• Southern Iran hosts the majority of salt glaciers and the most active salt glacier in the world.
• Salt glaciers exist in arid Iran where the salt has broken through the surface at high elevation and flows downhill.
• Salt glaciers are mostly found in arid areas, where they will be preserved due to the dry climatic conditions.
• New studies of salt glaciers can help improve the understanding how salt tectonics work and how they influence the surrounding landscape.
• Late Triassic salt glaciers repeatedly flowed onto a basin in Germany and were buried with sediment to create a series of preserved glaciers.
• This salt feature is composed of two salt glaciers and the larger one is 50 100 m thick and 3, 000 m long.
• Salt glaciers provide observable and tangible evidence demonstrating salt movement which allows scientists to further understand movement that occurs beneath the Earth s surface.
• The salt glaciers of the Zagros Mountains in Iran are halite while the salt glacier of L黱eburg Kalkberg, Germany is composed of gypsum and carbonate minerals.
• The salt glaciers of the Zagros Mountains in Iran are halite while the salt glacier of L黱eburg Kalkberg, Germany is composed of gypsum and carbonate minerals.
• Salt glaciers are a frequent topic in salt tectonics, which is the study of salt causing deformation and its leading cause is differential loading ( an unevenly distributed load ).