meltwater

Proglacial Glaciofluvial Landforms

Introduction to Proglacial Glaciofluvial Landforms | Outwash Plains | Kame and Kettle Topography | Kames | Kettles What are proglacial glaciofluvial landforms? Glaciofluvial landforms are created by glacial meltwater processes, occurring in supraglacial (on top of the glacier), englacial (within the glacier), subglacial (beneath the glacier) and proglacial (in front and beyond glacial margins) environments1. …

Proglacial Glaciofluvial Landforms Read More »

Shrinking glaciers in Bhutan

By Alex Hyde The sub-tropical glaciers of Bhutan Bhutan is a small mountainous nation located in the Eastern Himalaya, with a population of around 727 000 people (Figure 1). The country has a sub-tropical climate in its south, where it borders lowland plains, and a Himalayan subalpine climate to the north where it meets the …

Shrinking glaciers in Bhutan Read More »

Meltwater channels

What are meltwater channels? Each year, glaciers melt. Meltwater channels are erosional features, cut into rock and sediment by flowing water beneath or close to ice-sheet margins1,2. They can cut sizeable troughs, meaning that they are very visual indicators of the location of the former ice margin. Meltwater channels can therefore be used to work …

Meltwater channels Read More »

This site uses cookies. Find out more about this site’s cookies.