---
title: "Columns of the Giants — Basalt Columns on Highway 108 | Arnold Haven"
description: "The Columns of the Giants from Arnold: hexagonal basalt pillars, a flat quarter-mile interpretive trail, and ice that survives the summer."
lang: en
json-ld:
---

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![Columns of the Giants](/assets/columns-basalt-DPQdkXqN.jpg)

Explore Arnold

# Columns of the Giants

A cliff of hexagonal basalt columns beside Highway 108, with a short interpretive walk to their base and an ice field that survives the summer in the rubble. Fifteen minutes, and the best geology stop on the corridor.

[Check availability](/cabins)[See the cabins](/cabins)

First things first

## First things first

The Columns are the exposed face of a basalt flow that filled this canyon roughly 150,000 years ago and cooled into tall, near-perfect hexagonal pillars. Frost has been prising them loose ever since, so the base is a talus slope of broken columns lying like felled timber. 

They stand immediately beside Highway 108 near Pigeon Flat, about two hours from the cabins by way of Sonora. A flat quarter-mile interpretive trail crosses the Middle Fork Stanislaus and leads to the foot of the cliff. 

![A cliff of tall hexagonal basalt columns above a talus slope and a clear creek](/assets/columns-basalt-DPQdkXqN.jpg)

Geography

## Where Columns of the Giants sits

![Illustrated antique-style map of California inside the United States with a gold marker on the Columns of the Giants near Pigeon Flat, with an engraved cliff of hexagonal basalt columns beside a river](/assets/columns-of-the-giants-qZvqlAGe.jpg)

Illustrated locator map — for orientation, not navigation.

The Columns are the exposed face of a basalt flow that filled this canyon roughly 150,000 years ago and cooled into hexagonal pillars, later cut and polished by glaciers.

A patch of ice usually survives the summer in the shaded talus at their base, insulated by the broken rock.

It is about 80 miles from Chalet Bruin and Koda Loft via Sonora — roughly two hours.

Region

Central Sierra Nevada, upper Highway 108

County

Tuolumne County

Elevation

About 6,300 ft

Nearest town

Kennedy Meadows in season; Strawberry for services

Getting there

Highway 108 east near Pigeon Flat, with a quarter-mile interpretive trail

02 

## The walk and what to look for

The path is short, level and suitable for almost anyone, with signs explaining the flow, the columns and the glaciation that cut the canyon and exposed them. Look for the polished, striated rock surfaces where ice ground across the top of the flow, and for the way the columns curve where the lava cooled unevenly. 

In the shaded rubble at the base, a patch of ice usually survives all summer — insulated by rock, fed by winter snow, and cold enough that the air pouring out of the talus is noticeably chilly on a hot afternoon. It is a good trick to spring on children who have been in the car too long. 

![A flat gravel interpretive path through pines toward a wall of columnar basalt](/assets/columns-walk-Dn0eL5ka.jpg)

![Broken basalt columns in a talus slope with a patch of ice surviving in the shade](/assets/columns-talus-CSNBEFfK.jpg)

03 

## Practicalities

There is a small parking area, a picnic spot and a campground close by, with toilets seasonally. No water, no shop, and patchy or absent phone signal — the nearest services are back down at Strawberry or Kennedy Meadows in season. 

Do not climb on the talus. The blocks are loose, some weigh tons, and the slope is actively shedding new ones. Stay on the path, keep children in sight and admire the columns from the base. 

04 

## Season

Highway 108 is plowed to Kennedy Meadows in winter, but the stop itself is snowbound and the parking area unmaintained in the cold months. Late May through October is the practical window, and the ice patch is at its most surprising in July and August. 

This is one of a string of short stops on the way to Sonora Pass — pair it with Donnells Vista, Kennedy Meadows and the pass itself for a full day out of Arnold. 

![A cliff of tall hexagonal basalt columns above a talus slope and a clear creek](/assets/columns-basalt-DPQdkXqN.jpg)

05 

## Where to stay for a Highway 108 day

Everything above Strawberry is forest, water and rock, with almost nowhere to sleep. Basing in Arnold puts the whole corridor within a day's reach and gives you a kitchen and a hot tub at the end of it. 

-   [CHALET BRUIN — 12 guests, 5 bedrooms→ ](/cabins/chalet-bruin)
-   [KODA LOFT — 4 guests, 2 bedrooms→ ](/cabins/koda-loft)

Nearby

## Keep exploring

[

![Sonora Pass](/assets/sonora-pass-summit-BV_ZHJdT.jpg)

### Sonora Pass

Twenty minutes further up the same road, and 3,000 feet higher.

Discover ↗ 

](/explore/sonora-pass)

[

![Donnells Vista](/assets/donnells-overlook-Cucw-WT_.jpg)

### Donnells Vista

The two-thousand-foot granite gorge, a short drive back down the highway.

Discover ↗ 

](/explore/donnells-vista)

[

![Emigrant Wilderness](/assets/emigrant-lake-basin-6UGQOT6V.jpg)

### Emigrant Wilderness

The walk-in lake country entered from trailheads on this stretch of road.

Discover ↗ 

](/explore/emigrant-wilderness)

Good to know

## Frequently asked questions

How long is the trail at the Columns of the Giants? + 

About a quarter of a mile, flat, from the highway parking area to the base of the cliff. Fifteen to thirty minutes is plenty.

Is there really ice in summer? + 

Usually, yes — a patch survives in the shaded talus at the base, insulated by the rock, and the air coming out of the rubble is noticeably cold.

Can you climb the columns? + 

No. The talus is loose and actively shedding blocks, some weighing tons. Stay on the path and view them from the base.

When is it accessible? + 

Roughly late May through October. The stop is snowbound in winter even though the highway is plowed as far as Kennedy Meadows.

![](/__l5e/assets-v1/84bf9984-9cf8-406b-aaf5-dbde0a9f8c6a/arnold-haven-mark-white.png)

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