The relationship between stress and strain in these entities is modeled by the Glen-Nye flow law. The equilibrium line altitude is the long term balan
The relationship between stress and strain in these entities is modeled by the Glen-Nye flow law. The equilibrium line altitude is the long term balance point along one of these, and a tower on one of these is known as a serac.A type of particles created by these entities, when blown by the wind, are known as loess. The Malaspina one of these is an example of the Piedmont variety of these objects. Sharp ridges formed by these are called arêtes, and material deposited directly from these structures is known as a till, while material removed from these objects by mass wasting can form a cirque. Two main types of these are contintental and alpine, and whale shaped hills formed by these are known as drumlins. Leaving behind debris accumulations calle moraines, for 10 points, name these large masses of ice.
The relationship between stress and strain in these entities is modeled by the Glen-Nye flow law.
Glaciers