Jostedalsbreen

Of all Jostedalsbreen’s tongues, this is the one most people mean when they say they have seen the glacier. It sits at the head of Briksdalen, a short side-valley off the longer Oldedalen, and it earns its reputation honestly: no other arm puts a visitor this close to moving ice for this little effort. The walk in follows the valley floor upward, the ground getting rockier and barer as you go, until the trees give out and the ice comes into full view — a broken, blue-white wall filling the head of the valley. It ends, as glacier tongues here tend to, in its own small lake, fed directly by meltwater running off the ice front. That lake sits a little over three hundred metres above sea level, low enough that the walk to reach it never feels like mountaineering, high enough that the valley below still catches every bit of cold air draining off the ice above. What you are looking at is not a fixed thing. The position of that ice front creeps forward or pulls back year to year, a slow bookkeeping of how much snow fell on the ice cap’s interior against how much the following summer took away. The lake, the bare rock apron, the exact line of the ice — none of it is where it was a generation ago, and none of it will stay where it is now.

Nigardsbreen drains the eastern side of the same ice cap that feeds Briksdalsbreen on the far side of the park, and standing at either one it is easy to forget they are fed by the same body of ice at all. That is the trick of a glacier this size: from any single valley you only ever meet one finger of it, reaching down through whichever gap in the mountains offers the easiest gradient, looking for all the world like a glacier of its own. The national park around it protects roughly thirteen hundred square kilometres of high country, and the ice itself covers well over half of that — yet no viewpoint anywhere in the park shows you more than a sliver of the whole. What you can read here, up close, is the glacier’s most recent business: a churned, milky stream running off the ice, carrying rock ground to powder under the moving mass; and beyond the current ice edge, a band of bare, scraped rock, smoothed and sometimes faintly scratched, marking ground the ice let go of not long ago.

Bøyabreen is a smaller, lower arm of the same ice cap, and it is worth visiting for one thing in particular: the color. Look at the ice where it is thickest and freshest — not the dirty, broken surface near the front, but a crevasse wall or a clean fractured face — and it reads distinctly blue, not white. That is not a trick of light or reflection off the sky. Glacier ice is old, compressed snow that has had the air squeezed out of it over years of burial under new snow above; without trapped air bubbles to scatter light in every direction, the ice instead absorbs red wavelengths and lets blue pass through and bounce back, the same basic physics that makes deep water look blue rather than clear. Fresh snow, full of air, looks white for the opposite reason. The color is a rough, honest gauge of age and density: the bluer the ice, the longer it has sat under the weight of everything that fell on it since, patiently turning from snow into something closer to rock.

Kjenndalsbreen is a fourth face of the same ice cap, tucked into its own valley, and the most useful thing to do here is not just look at the ice but look for what it left behind. A glacier tongue’s front is never still for long; it advances in cold, snowy years and retreats in warm ones, and every position it holds for any length of time leaves a low ridge of dumped rock and gravel at its edge — a terminal moraine — before the ice moves on and abandons it. Walk the ground between the current ice front and the valley’s tree line and you are walking across a rough timeline, each low ridge a season or a run of seasons when the glacier paused. None of it is ancient. Most of what you are standing on here was still buried under moving ice within living memory, and some of the freshest ground has barely had time to grow anything at all.

Lodalskåpa is the highest point in this entire stretch of mountains, standing a little over two thousand metres above the sea — taller than every summit the glacier actually covers — and that fact is the whole reason it belongs in a note about ice. A nunatak is a peak that stands clear of an ice cap even at the ice’s fullest extent nearby: not because it escaped the glacier by luck of position, but because it is simply tall enough that the ice surface, thick as it is, never rose to meet its summit. Everywhere around Lodalskåpa, ridgelines and lower peaks disappear under moving ice; here, the summit rock has stood in open air the entire time, weathered by frost and wind rather than ground down by a glacier’s passage. That difference is visible in the rock itself if you know to look for it: ice-scoured stone tends to be smoothed and rounded, its edges softened by centuries of moving ice and grit; rock a glacier never reached keeps a sharper, more broken, frost-shattered character. Reaching the summit means climbing well above where the ice cap’s own surface tops out, a serious undertaking in high, exposed terrain rather than a short walk from any road. The reward is a vantage very few glacier viewpoints offer: the ice cap seen from above and beside, rather than from below and in front of it.

Brenibba is Lodalskåpa’s quieter counterpart, another summit standing higher than the ice cap’s own highest ice yet never buried by it. Where Lodalskåpa rewards the climb with distance and scale, Brenibba sits closer to the ice cap’s working arms, close enough that from its summit several of the glacier’s separate tongues become visible at once, laid out below like fingers of a single hand rather than the isolated glaciers each looks like from its own valley floor. That is the view this note has been building toward at every stop: not one glacier here and another there, but a single mass of ice sending itself down through whatever gaps in the mountains lie lowest, watched over by a handful of summits it was never quite tall enough to reach. Like its higher neighbor, reaching Brenibba means committing to remote, high terrain well above any road or maintained path — this is not a detour on the way to somewhere else, but a destination worth planning as one.

Not every stop needs to put you at the ice’s edge. This one is named plainly for what it does: it gives you the ice cap as a single object, rather than as one arm glimpsed from the bottom of one valley. From here the scale sorts itself out in a way it can’t from underneath a glacier tongue — you are looking at a broad white mass filling the high country as far as the ridgelines allow, the largest glacier on mainland Europe reduced, from this distance, to something you can actually take in with one look. Pick out the darker lines running down through the white and you are seeing the glacier’s own structure: bands where debris and older, dirtier ice have folded into the moving mass, tracing the paths ice takes as it flows downhill under its own weight, the same way water finds its channel. It is a useful corrective after visiting the arms up close, where the ice fills your whole view and reveals nothing of its shape. From a distance, for once, the whole thing holds still long enough to actually see.