Mount Rainier

The first time Mount Rainier appeared to me I was doing seventy on I-5 south of Tacoma, having convinced myself I understood the scale of the Pacific Northwest after four days in Seattle. Then a break in the clouds came and there it was — not in the distance but somehow occupying a part of the sky that no mountain has any right to occupy, a white bulk so disproportionate to everything around it that I genuinely checked if I was misidentifying something. I pulled off at the next exit. I stood by a chain-link fence on a suburban service road, craning my neck, and I took a photograph that managed to convey none of it.

Mount Rainier is 4,392 metres and sits entirely alone, unconnected to a ridge or a range in any meaningful way — a volcanic cone that rose from the lowlands like an argument. It generates its own weather. Clouds form around its summit in the morning regardless of what the rest of the sky is doing, and by afternoon it is often entirely swallowed. The locals have a phrase: “the mountain is out.” This is said with the reverence you might reserve for news of a remarkable visitor.

The Paradise area — and whoever named it had no modesty but also was not wrong — sits at around 1,650 metres on Rainier’s south slope, and in late July it is one of the most extravagant displays of alpine wildflowers I have seen anywhere on the continent. The Skyline Trail winds through meadows of lupine, paintbrush, and avalanche lily, with glaciers visible above and the Tatoosh Range running across the horizon to the south. I hiked it alone one Thursday morning in August and passed perhaps twelve other people in four hours. This seemed impossible given what the meadows looked like. If these flowers existed in Europe they would be administered with a ticket system.

Higher up, the Muir snowfield begins — a vast apron of permanent snow that the summit climbers cross at night by headlamp to hit the crater rim at dawn. I am not a technical climber and I have no summit story to offer. But I sat at Camp Muir at 3,100 metres on a clear afternoon and watched the clouds build over the lowlands far below while the summit above me hummed with the particular silence of very high, very cold, very serious places. The coffee I’d brought in a thermos had gone cold. It didn’t matter.

The Carbon River entrance on the park’s northwest side is the road not taken by most visitors, and it rewards the detour. Here the rainforest meets the mountain — temperate jungle at the base, then the subalpine forests, then snowfields, all within a few miles of driving. The Carbon Glacier comes lower than almost any glacier in the contiguous United States, its snout sitting at around 400 metres, dark with rock flour. You can hear it groaning if you sit quietly enough.

When to go: July and August give access to the high trails and the full wildflower bloom at Paradise. The mountain is accessible year-round but the upper roads close from roughly October to May. For solitude and autumn colours in the lower forests, October is underrated — the overnight crowds thin dramatically after Labor Day.