Cangshan Ximatan Ropeway
Dali, Yunnan Province

Ascend to the Clouds: The Ultimate Vertical Journey at Cangshan Ximatan Ropeway

Altitude:3,920m

🏔️ High Altitude Notice

This location is at 3,920m elevation. Mild altitude sickness may occur. Stay hydrated and avoid strenuous activity on your first day.

About This Attraction

Location & Nearby Attractions

📍 Showing 10 nearby attractions within 50km

📍 Dali, Yunnan Province • 🏔️ 3920m elevation

Frequently Asked Questions - Cangshan Ximatan Ropeway Travel Guide

Where is the Ximatan Ropeway located?
It is located west of Dali Ancient City, with the lower station near the Tianlongbabu Film City.
What is the best time to visit?
The best time is from April to June to see the azaleas, or September to November for clear skies and better visibility of Erhai Lake. Winter offers snow scenes but can be very cold.
Is it safe for people with altitude sickness?
The top station is at 3,920 meters. Altitude sickness is possible. It is recommended to bring portable oxygen, walk slowly, and avoid strenuous exercise.
What should I wear?
The temperature at the top is significantly lower than at the bottom. Even in summer, it can be cold and windy. Bring a windbreaker, warm layers, and sun protection (hat, sunglasses) due to high UV rays.
How long does the ride take?
The ropeway ride takes approximately 40 minutes one way.

✨ Why Visit Cangshan Ximatan Ropeway

World-Class Vertical Drop: Experience one of the world's longest ropeways with a vertical drop of 1,648 meters, ascending from subtropical vegetation to alpine glaciers.
Ximatan Alpine Lake: Visit the legendary "Washing Horse Pond" at 3,920 meters, a glacial moraine lake known for its crystal-clear water and historical legends,.
Azalea Sea: Visit in May and June to see the mountainside erupt into a spectacular display of blooming alpine azaleas.
Panoramic Erhai Views: Enjoy a bird's-eye view of Erhai Lake, Dali Ancient City, and the surrounding villages from the cable car and observation decks.
Geological Wonders: Observe the distinct vertical vegetation belts and traces of Quaternary glaciation on the rocky peaks.

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