Hakusan Onsen-kyo

白山温泉郷 · Ishikawa

Hakusan Onsen-kyo (白山温泉郷) is a nationally designated onsen town in Ishikawa. We measured how much snow its winters bring, using the same method as for the 3,108 ski areas on this site.

Snowfall in winter

Per season 263 cm
Rank 15 of 77 ranked onsen
Against the median of 77 +144 cm median 119 cm
Season to season 168 cm 187–355 cm across three winters

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We do not link to an official site. We have not verified URLs for all 79 towns, and guessing would send you somewhere wrong. They will be added once checked.

How this place came to be

A group of springs at the foot of Mount Haku (2,702 m) in Ishikawa — Chugu, Iwama, Ichirino and Tedori among them.

Chugu claims twelve centuries. The story is that Taicho Daishi, the monk who opened Mount Haku to religious practice, found an injured white dove by a stream and noticed hot water rising nearby. But there is a second version, in which villagers who had gone deep into the mountains to farm found the dove instead. Both agree that a white dove showed the way; they disagree only about who was watching.

The first bathhouse was built in 1574. Chugu has long been regarded as water for the stomach and gut, and people still come to stay and soak.

The mountain itself is the point. The Hakusan festival, held in mid-July, traces its origin to Taicho's opening of the peak.

Sources: 環境省 白山温泉郷 国民保養温泉地計画書 · 石川県白山自然保護センター『白山の自然誌44 白山の秘湯・中宮温泉の歴史』

Ski areas nearby

Up to five within 40 km, straight-line, nearest first. Quality rank is out of the 395 Japanese ski areas.

Ski areaDistanceQuality rank
Hakusan Senjo Onsen Seymour Ski Area 4 km 241 of 395
SAM Hakusan Ichirino Ski Resort 10 km 215 of 395
Ookuradake Kogen Ski Area 11 km 367 of 395
Kanazawa Municipal Ski Resort 24 km 295 of 395
IOX-AROSA 25 km 278 of 395

About these snowfall figures

The snowfall shown here is an estimate produced by a weather model, not a record of what actually fell.

We compared it against 63 Japan Meteorological Agency weather stations to see how far off it is. On average it comes to about six tenths of the real figure — it runs low. And it runs low by different amounts in different places: some read barely a third of what was measured, others match almost exactly. Mountains tend to read lowest.

We tried scaling everything up by a fixed amount to correct for it. It barely helped, because the error differs from place to place.

So treat these numbers as a guide to roughly where somewhere sits, not a precise figure. There is no meaning in the gap between first and second, or between 30th and 35th. Large differences between regions are real and can be read as they are.

We are working on replacing these estimates with observed values.

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