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“He may be just a tramp, a guy that likes to roam about this great country without any special aim, just to thank the Lord for these beautiful mountains.”
-B. Traven, The Treasure of the Sierra Madre
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“. . .here, where there are still the silences and the loneliness of the earth before man, . . .”
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- Matías Reyes, Santa Barbara Mission (1887)
- Indian Head Test Pattern (1939)
- About
- Return To Scene Of Lion Standoff
- Rick Sharp O’Neill Wetsuit Ad in Surfer Magazine (1975)
- The Mighty Chanterelle and the Gnarly Oak
- Sulfur Mountain Oil Seeps, Ventura County
- Fossil Falls, A Glacial Relic of the Pleistocene
- Fire Poppy (Papaver californicum)
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Latest Dispatches
- The Exceptional Sundowner Winds of Santa Barbara
- Lobster Poachers?
- Dick Smith on Forest Access
- Old Mission Sycamore Whacked Again
- Bald Eagle, Manzana Creek, San Rafael Wilderness
- When Rains Fall, Will USFS Close Our Forest? The Coming El Niño
- Language of Forest Closure; Assault on an Ancient Right
- March of the Mustard; The Spread of Noxious Weeds
- Mark of Conquest II: Benchmark and Mortar
- Save Old Mission Sycamore … __ __ __ …
- Raking the Forest: Anderson, Trump, Kuyper
- Initials of J.D. Reyes (1907)
- Last California Grizzlies Seen In Santa Barbara National Forest? (1926)
- Eccentric Artifact, San Marcos Foothills Preserve
- Fog Drip Morels
Lunar Phase
Tag Archives: Geology
Tafoni Weathered Stone
“Tafoni are ellipsoidal, pan- to bowl-shaped, natural rock cavities. These cavernous weathering features include tiny pits, softball-sized cavities, truck-sized caves, and nested and cellular honeycomb forms. Tafoni typically develop on inclined or vertical surfaces and occur in groups. These exquisite … Continue reading →
Geologic Control of Vegetation In Santa Barbara County
In certain places grass, sage brush and chaparral grow beside each other in notably separate and distinct patches. The specific place along the ground where grasses stop growing and woodier plants begin can be remarkably exact and linear in appearance … Continue reading →
