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Ryumon Falls
Ryumon Falls
Ryumon Falls
Ryumon Falls
Ryumon Falls

Ryumon Falls

GardenTourist Attraction

4.4

(28)

Ryumon Falls is a small, tranquil waterfall located within the grounds of Kinkaku-ji Temple in Kyoto. It offers a quiet contrast to the temple's main, more ornate structures. The waterfall's design and the surrounding garden are deeply symbolic, drawing from a Chinese legend about a carp transforming into a dragon.

Address

Kinkakujicho, Kita Ward, Kyoto, 603-8361, Japan

Opening Hours

9:00 AM – 5:00 PM (Sun)

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Worth it?

Worth it if you appreciate subtle, symbolic beauty and a peaceful atmosphere

Skip if you're only looking for grand, dramatic waterfalls

Reviewers appreciate the peaceful and powerful scenery, which stands in contrast to the more flamboyant main temple.2 mentions

Location

Kinkakujicho, Kita Ward, Kyoto, 603-8361, Japan

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Highlights

The "Carp Stone" (鯉魚石) at the base of the falls is a key feature, representing the carp from the legend that leaps the dragon gate to become a dragon.

The area around Ryumon Falls is generally less crowded than other parts of Kinkaku-ji, making it a good spot to pause and take in the garden's depth.

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Who it's for

Solo
Couples
No wheelchair entrance
No accessible parking

Travelers interested in Japanese garden philosophy and those seeking a moment of quiet reflection away from the main crowds at Kinkaku-ji. It's also meaningful for anyone interested in symbols of perseverance and success.

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Reviews

4.4

Very good

5 Reviews

Visitors find Ryumon Falls to be a quiet, impressive spot within Kinkaku-ji, offering a deeper, more philosophical experience than just viewing the temple's main hall. Many note that understanding its symbolic meaning enhances the visit.

Fun facts

The waterfall's name and the "Carp Stone" are inspired by the Chinese legend of "Toryumon," where a carp that climbs a waterfall becomes a dragon, symbolizing effort and success.

Historical records suggest that in the Kamakura period, the waterfall was much taller, around 15 meters, before geological changes reduced it to its current size.


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