It wasn't until around 34 million years ago that the first
small glaciers formed on the tops of Antarctica's mountains.
Not exact matches
Serve
small portions to children explaining that the blue is the icy center of a
glacier (a mass of ice
formed by compacted snow) and the white on top is snow with silt (fine bits of sand and clay) in it.
Further down along the coast, the mountains get
smaller and more rounded, and their lush green
forms poke over beautiful tidewater
glaciers.
My hunch is the few large
glaciers draw from the central ice mass through «gateways» and the many
smaller glaciers instead
form mostly from snowfall on the outside of the ring of mountains around the icecap.
Land ice includes any
form of ice that lasts longer than a year on land, such as mountain
glaciers, ice sheets, ice caps and ice fields (both similar to but
smaller than an ice sheet), and frozen ground or permafrost.