松仙園登山道

ぬかるみ。時期や場所によっては、深い水たまりがある（登山口～二ノ沼の区間）

わかりにくい道（特に雪解け直後の開葉前）、岩場。開通後であっても雪が多い年は雪渓トラバースになる（二ノ沼～四ノ沼の区間）

A muddy section; there may be deep puddles, depending on the period or location. (Section between the trailhead and Nino-numa Pond)

Unclear trail and rock section (particularly just after the snow has melted, before the leaves have sprouted.) In years with heavy snowfall, it may be necessary to traverse snow gullies (the section between Nino-numa Pond and Yonno-numa Pond)

大きな岩の段差（登山口～二ノ沼の区間）

Large rock steps (the section between the trailhead and Nino-numa Pond)

滑りやすい急斜面（登山口～二ノ沼の区間）

Steep, slippery slopes (the section between the trailhead and Nino-numa Pond)

溶岩台地上に広がる湿原の向こうに、大雪山の主峰・旭岳がそびえる風景は松仙園ならではです。夏の湿原では、ツルコケモモ、ヒメシャクナゲ、ヒツジグサ、ワタスゲといった湿原特有の植物がみられます。

The scenery in which the highest peak in the Daisetsuzan Mountain Range, Mt. Asahidake rises in the background of the wetland that covers the lava plateau is unique to Shosenen. In summer, wetland-specific vegetation such as cranberry, bog rosemary, pygmy waterlilies, hare's-tail cottongrass and the like can be seen there.

日本で一番早い紅葉と言われる大雪山。針葉樹の緑と落葉広葉樹の朱色や黄色など、微妙に異なる色が折り重なる中に、空の色を映す池塘（ちとう）が点在する様子は松仙園ならではの絶景です。運が良ければ初冠雪と紅葉を同時に見ることができるかもしれません。

The Daisetsuzan Mountain Range are said to be where Japan's earliest autumn foliage can be seen. Amid the subtle changes in the greens of the conifers and the vermilion and yellows of the deciduous hardwood trees, the color of the sky reflects in ponds that are doted around, producing landscapes unique to Shosenen. If you are lucky, you may even see the summit of the mountain covered in the first snow of the season, at the same as the surrounding autumn foliage.

登山口から樹林帯を抜けて溶岩台地の上に出ると、背の低い変わった形をしたアカエゾマツが点在しています。これは吹き付ける強い風の影響を受けて、幹や枝が風向きに沿うように風下側へ傾いたり曲がったりしたものです。厳しい環境の下でアカエゾマツは必死に生き続け、中には樹齢数百年を数えるものもあります。

The scenery in which the highest peak in the Daisetsuzan Mountain Range, Mt. Asahidake rises in the background of the wetland that covers the lava plateau is unique to Shosenen. In summer, wetland-specific vegetation such as cranberry, bog rosemary, pygmy waterlilies, hare's-tail cottongrass and the like can be seen there.

四ノ沼の展望地から見える湿原の縞模様は、等高線に沿って帯状に並んだ湿原の表面の凹凸によって形作られています。泥炭でできた帯状の凸地をケルミ、凹地をシュレンケと呼び、凹凸が一体となっていることからケルミ・シュレンケ複合体とも呼ばれています。このような湿原の縞模様は、大雪山ではこの場所でしか見ることができません。

The striped pattern of the wetland, which can be seen from the Yonno-numa Pond viewpoint, is the result of the undulating surface of the wetland formed by the contours of the land. The peat hillocks are known as string, while the concave depressions are known as flark, with the undulations collectively known as string-flark. In the Taisetsu Mountains, such patterns can only be seen in this location.