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หน้าแรก/จังหวัดโออิตะ/Bungo-ono/Harajiri Falls

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จังหวัดโออิตะ· Bungo-ono
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Harajiri Falls

Little knownBarely documented in English. This is the kind of place the site exists for.

ค้นคว้าและเขียนโดย

waterfallNiagarawide fallsfarmlandtufa
Harajiri Falls

Photo: daisymind / Wikimedia Commons (CC BY 4.0) · original

Harajiri Falls (原尻の滝) is a 120-meter-wide, 20-meter-high waterfall that drops in a perfect curtain across the Ogata River — earning its nickname 'Niagara of Japan.' Unlike most Japanese waterfalls hidden in mountain gorges, Harajiri is located in flat farmland, creating an unexpected visual drama where the river simply vanishes over a cliff edge into a wide basin below.

The falls can be viewed from multiple angles: above from the surrounding farmland, at eye-level from a suspension bridge, and below from the basin floor. The surrounding tufa cliffs (created by volcanic mineral deposits) add geological interest.

ข้อมูลสำคัญ

เวลาเปิดทำการ

24/7 (illuminated at night). Suspension bridge and trail: daylight hours.

วันหยุด: Open year-round. Trail may close after heavy rain.

ค่าเข้าชม

Free. Parking free.

ฤดูที่ดีที่สุด

April for cherry blossoms framing the falls; July–August for highest water volume; winter for ice formations on cliff face

ระยะเวลาเที่ยวชม

45 minutes for full 2km circuit trail; 20 minutes for main viewpoint and suspension bridge only

การเดินทางไป

ข้อมูลการเดินทาง

Ogata-machi, Bungo-ono City. A drive from Bungo-ono IC (Oita Expressway). Free parking. Hours: 24/7 (illuminated at night). Viewing areas accessible year-round.

คู่มือจากคนใน

**Best viewing season:** April (cherry blossoms frame the falls) and July–August (highest water volume from summer rains). Winter sees reduced flow and occasional ice formations on the cliff face. **Walking circuit:** A 2km trail loops the falls basin, crossing the suspension bridge (吊り橋) and descending stairs to the base for spray-zone views. The full circuit takes 45 minutes. The trail can be muddy after rain — wear appropriate footwear. **Tufa cliffs explanation:** The stepped cliff formation is tufa (travertine) — calcium carbonate deposited by mineral-rich water. The geology creates natural terraces and small cave formations visible from the suspension bridge.
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