South View of Sonora Peak and the PCT from Sonora Pass
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Snow in the meadows on the PCT toward Sonora Pass
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Walking on the snow down the Pacific Crest Trail toward Sonora Pass
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Snow wall blocking the Pacific Coast Trail. I had to crawl below the patch of snow...
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Igneous rocks on the Sonoma Peak south-east ridge
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South east ridge of Sonora Peak
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Igneous rocks on the Sonoma Peak south-east ridge
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Path down to the PCT on the Sonoma Peak south-east ridge
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Lichens and volcanic rocks at the top of Sonora Peak
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Butterfly at the top of Sonora Peak
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Stanislaus Peak and North-west ridge of Sonora Peak
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South-east ridge of Sonora Peak
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South View from Sonora Peak. CA-108 on the right
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Selfie at the top of Sonora Peak
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View of Stanislaus Peak from Sonora Peak
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Nort View from Sonora Peak's top
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East View from Sonora Peak's top
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South-east View from Sonora Peak's top
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South View from Sonora Peak's top
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View of Stanislaus Peak from Sonora Peak. The rock pile is one of the rock bunker made to protect the hikers from the wind at the top
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Mandatory Selfie at the top of Sonora Peak
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Mandatory Selfie at the top of Sonora Peak
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Sonora Peak top: 'murican flag and logbook
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Sonora Peak via St Mary's Pass and PCT
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Sonora Peak via St Mary's Pass and PCT
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Sonora Peak via St Mary's Pass and PCT
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Sonora Peak via St Mary's Pass and PCT
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Sonora Peak via St Mary's Pass and PCT
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Sonora Pass fromSt Mary's Pass. You can see CA-108 in the center of the picture
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Stanislas Peak from St Mary's Pass
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The trail to the summit can be seen on the left.
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Sonora Peak South side, with a hollow rock
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Sonora Peak via St Mary's Pass and PCT
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Stanislaus National Forest - Horses near Kennedy Meadows on CA-108
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Eureka Valley Campground
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Eureka Valley Campground
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Eureka Valley Campground
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Eureka Valley Campground
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Stanislaus National Forest - Herring Creek Road
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Stanislaus National Forest - Herring Creek Road
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Stanislaus National Forest - Herring Creek Road
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Stanislaus National Forest - Herring Creek Road
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small creek below the columns, flowing to Stanislaus River.
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These are rock formatons made 150,000 years ago after basalt lava flows cooled down slowly, forming columns with regular geometric shapes (mostly hexagons. Their diameter varies from 10 to 40 cm.
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These are rock formatons made 150,000 years ago after basalt lava flows cooled down slowly, forming columns with regular geometric shapes (mostly hexagons. Their diameter varies from 10 to 40 cm.
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These are rock formatons made 150,000 years ago after basalt lava flows cooled down slowly, forming columns with regular geometric shapes (mostly hexagons. Their diameter varies from 10 to 40 cm.
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These are rock formatons made 150,000 years ago after basalt lava flows cooled down slowly, forming columns with regular geometric shapes (mostly hexagons. Their diameter varies from 10 to 40 cm.
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These are rock formatons made 150,000 years ago after basalt lava flows cooled down slowly, forming columns with regular geometric shapes (mostly hexagons. Their diameter varies from 10 to 40 cm.
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