PLACE GUIDE

Asihatu Stone Formations 阿斯哈图石阵

Asihatu Shizhen

Asihatu's granite stone formations rise on Beida Mountain in northeastern Hexigten Banner, at a meeting point of mountain meadow and woodland.

Asihatu Stone Formations (阿斯哈图石阵)
Asihatu Stone Formations · 阿斯哈图石阵 · Source photographer · License not provided
Photo adjustments

EXIF orientation normalized; resized without changing aspect ratio; converted to WebP. No subject edits.

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About Asihatu Stone Formations

The rock is cut by near-vertical and near-horizontal joints. These intersecting fractures help explain the formations' divided, layered appearance, with columns, walls, overhangs and narrow passages producing a range of shapes rather than a uniform field of pinnacles.

The surrounding vegetation is part of the scene: mountain grassland meets woodland around the stone formations. Summer greenery and autumn foliage change the contrast between the exposed granite and its setting, while the rock shapes remain the central feature.

What to look for

  • Granite columns and wall-like formations crossed by horizontal joints.
  • Rock shelters, fissures and narrow passages between the formations.
  • The mountain meadow and woodland surrounding the stone array.

Location & getting there

Getting to Asihatu Stone Formations

Use an authorised visitor route. Cave sections, geological sites and access roads can close independently, so confirm the area that your ticket covers.

  • Search for 阿斯哈图石阵 with 赤峰市 and 克什克腾旗.
General visit reminders

Use an authorised visitor route. Cave sections, geological sites and access roads can close independently, so confirm the area that your ticket covers.

Landforms & caves · 地貌/洞穴 →

Find Asihatu Stone Formations

阿斯哈图石阵 · 克什克腾旗

No reliable map pin yet: search by the Chinese name.

Sources & visit information

The linked sources support the identity and background described in this introduction. Opening hours, admission, activity availability and exact arrival arrangements have not been comprehensively checked. Confirm current visitor information with the venue; the original catalogue locality and editorial review flag are retained.