Ice shelves (the floating
front edges of glaciers that extend tens to hundreds of miles offshore) melt more because of contact with ocean water below them than they do because of sunlight.
Research published last spring in Nature Climate Change made a convincing case that that trek is now engaged in a 40 km retreat, a movement that will only continue to accelerate as warm water laps at the shallow
leading edge of the glacier and as the glacier very slowly increases its angle of descent off of the continent's land shelf.
Southeast of where I live, water from the
melting edge of the glacier flowed over the landscape, depositing layers of sand and silt and leaving behind areas with names such as Flatbush and Flatlands.
In 2007, researchers were collecting long - frozen plant samples from the
receding edges of the glacier when they noticed some bryophytes — plants which include mosses and mosslike liverworts — sprouting new parts (as seen in the main image).
First, increasing snowfall since the mid-1990s caused snow to pile up and start working its way toward the
front edge of the glaciers (a process known as surging).
As melting ice from these glaciers formed streams and rivers along
the edge of the glaciers, thick sequences of sand and gravels were deposited.
The study shows that it's plausible, even if Mars was generally frozen over, that peak daily temperatures in summer might sneak above freezing just enough to cause melting at
the edges of glaciers.
If Sir Edmund Hillary and Tenzing Norgay were to set out to conquer Mount Everest today, they would have to hike an extra two hours to reach
the edge of the glacier that once sat close to their base camp.
Icebergs that have calved off
the edge of the glacier are visible floating out to sea — but so are cracks hundreds of kilometers inland from Jakobshavn, on what would otherwise be a flat expanse of ice.
The slope was
the edge of the glacier, but now we were walking on solid ground.
The coastline itself —
the edge of the glacier ice — appears as a faint white line.
Professor Poinar continues, «Mammoths were much better at adapting to new habitats than we first thought — we suspect that subgroups of mammoths evolved to deal with local conditions, but maintained genetic continuity by encountering and potentially interbreeding with each other where their two different habitats met, such as at
the edge of glaciers and ice sheets.»
The highlighted area shows a dense concentration of crevasses along one
edge of the glacier.
Some are far away, like the swirling blue meltwater that laps
the edges of a glacier, while others lurk just under our feet, like an ant waving a leaf like a victory banner.
Each measurement transect on Columbia Glacier begins and ends at a fixed location at
the edge of the glacier.
It is showing the approximate former locations of the glacier margin (aka «the toe»; aka where
the edge of the glacier used to be) measured at different points in time.
Now that the glaciers have melted, the land beneath where they were located is now rising, while the land at where
the edges of the glaciers were located is sinking, i.e., subsiding.
Glaciers during the last ice age were so thick and heavy that their weight caused the land immediately beneath them to sink, while the land at
the edges of the glaciers rose.