Skip to content

Our Shopify store delivers the heritage and craftsmanship of Japanese stone artisans to gardens across the globe, with secure international shipping and reliable customer support.

Stone products available for purchase in the cart will be shipped by air freight. Larger stone products that are not available in the cart will be shipped via pallet transport, exclusively for B2B customers.

Mount Fuji - World Heritage Geology, White Slopes Explained, Eruptions

Mount Fuji - World Heritage Geology, White Slopes Explained, Eruptions

Mount Fuji (3,776 m), listed in 2013 as a UNESCO World Cultural Heritage site.
Mount Fuji from Yamanashi side, photographed on Jan 24, 2017
On January 24, 2017I took this photo of Mount Fuji from the Yamanashi Prefecture side.

Rising to 3,776 m (12,388 ft), Mount Fuji is Japan’s most iconic volcano. Its smooth cone looks different by season. The slopes can appear white because of snow, light-colored volcanic ash, and weathered rock.

In 2013, UNESCO listed Fujisan as “a sacred place and a source of artistic inspiration.” The World Heritage property includes the summit area and 25 cultural sites around the base, such as Sengen shrines, pilgrim lodgings, lakes, and lava-shaped landscapes.

Brief Timeline

Year Event
Jōmon–historic Repeated eruptions lay down wide lava fields
AD 864–866 Jōgan eruption: lava flows help form today’s Lakes Sai & Shōji. Aokigahara forest later grows on the flows.
AD 1707–1708 Hōei eruption: a crater opens on the SE flank. Ash reaches Edo (about 100 km away).
2013 UNESCO listing as a cultural landscape (Criteria iii, vi)
2024 Yoshida Trail crowd controls begin (daily cap and night restrictions). A fee starts on the Yamanashi side.
2025 A ¥4,000 hiking fee applies on all trails. Rules are refined for safety and conservation.

At a glance

UNESCO inscription 2013
UNESCO ID 1418
Criteria (iii), (vi) — sacred tradition & artistic inspiration
Property Summit zone + 25 component sites around the base
Type Cultural Landscape
Elevation 3,776 m (12,388 ft)

How Mount Fuji Became a World Heritage Landscape

Era From 12th-century mountain practice, through Edo-period Fuji-kō pilgrimages, to modern conservation
Patrons & Stewards Sengen shrine networks, oshi (pilgrim guides), local governments, and Japan’s environment agencies
Place Yamanashi & Shizuoka Prefectures, about 100 km southwest of Tokyo
People Pilgrims and mountain practitioners; artists such as Hokusai & Hiroshige
Plan Routes and rituals linked with lakes, springs, waterfalls, and volcanic features
“Construction” Fuji formed naturally from lava, ash, and scoria. Later, people shaped the pilgrim routes, huts, and shrines.

World Heritage Facts & Visitor Numbers

Item Current detail Notes
Climbing season Typically July 1 – early September Trails can close anytime due to weather
Daily cap (Yoshida Trail) 4,000 people/day Gate controls at 5th Station; hut reservations may allow entry during restricted hours
Gate hours (Yoshida) Restrictions 14:00–03:00 To reduce unsafe “bullet climbing”
Entrance / hiking fee ¥4,000 per person (all trails, 2025–) Online reservation is recommended
Total climbers 2023 ≈ 221,322 Environment Ministry figure
Total climbers 2024 ≈ 204,316 A decline after new controls

Materials

Category Mount Fuji Notes
Main stone Basalt Basalt lava built the main cone
Secondary Scoria, ash, lapilli, pumice Layered volcanic deposits on the slopes
Core/Backing Volcanic edifice A natural mountain body, not a built core
Inlay / dark stone for script Not applicable
Metals Not applicable
Granite as primary material Not used Fuji is a basalt volcano, not a granite mountain

Why Basalt, Not Granite?

Granite forms deep underground and cools very slowly. That is why it is strong and widely used in temples, gardens, and stone lanterns.

Mount Fuji is different. Fuji was built mainly by basalt lava that erupted at the surface and cooled quickly. Over time, ash, scoria, and weathering shaped the slopes.

The mountain can look white in some seasons. The main reasons are snow, light volcanic deposits, and sunlight on weathered rock. In other seasons, the darker basalt becomes more visible.

Legends — Myth vs Fact

Theme Myth & Faith What the record shows
Deity Asama no Ōkami resides at the summit Summit shrines and ohachimeguri show long worship at the top
Purification Water rites at lakes and springs The Five Lakes and springs were used for cleansing before climbs
Artistic icon Fuji as the perfect cone Ukiyo-e by Hokusai and Hiroshige shaped how the world sees Fuji

Care, Time, and the Color of Memory

Today, Fuji faces overtourism and safety risks. That is why authorities limit entry on busy routes and restrict late-night climbing. A ¥4,000 fee (from 2025) supports safer management and better conservation.

My Personal Pledge — Returning to the Summit

When I was about ten, I tried to climb Mount Fuji. But I had to turn back. The feeling stayed with me for years.

I want to finish what I started. I will climb Fuji again, take my own summit photos, and publish the story on this blog.

FAQ

  • Is Fuji made of granite? No. It is mainly basalt, with layers of ash, scoria, and pumice.
  • Why do Fuji’s slopes look white? Mostly snow, light ash, and weathered rock reflecting sunlight.
  • Do I need to reserve? Online reservations are recommended on busy trails.
  • What is the fee? ¥4,000 per person (all trails, per climb) during the season.
  • Best timing? Early-season weekdays or quieter windows after Obon. Always check for closures.

Internal Links

Last updated (JST): January 5, 2026

Back to blog