What the app shows you
Full FogCast score, fog type, chase-or-skip verdict, and 10-day outlook — all in the app.
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Know before you drive: FogCast checks the conditions that produce photogenic fog
Get more than a snapshot of current conditions. The LightCast app unlocks everything to plan ahead
Humidity alone isn't enough. Wind alone isn't enough. Cloud cover alone isn't enough. Photogenic valley fog requires several conditions to line up at once, and most weather apps don't read them together.
Set a FogCast threshold once. The app will alert you when conditions at your saved locations look promising, so you're not manually checking at 4am.
Don't waste a sunrise drive. Check FogCast before you leave.
Download on the App StoreSmith Rock State Park in central Oregon rises from the high desert plateau above the Crooked River canyon, with volcanic tuff formations towering over 150 meters above the river. The park sits on the dry east side of the Cascades, which means fog here is a rarity rather than a daily occurrence — but that rarity makes it all the more dramatic. When temperature inversions trap moisture from the Crooked River in the canyon on cold autumn mornings, a thin fog layer fills the canyon floor while the orange and red rock formations stand brilliantly above it.
The Misery Ridge viewpoint and the canyon rim above the Crooked River bend give above-fog perspectives when the canyon is filled. The river-level trail between Monkey Face and Asterisk Pass is the best location to be inside the fog layer when it's thin and moving — the rock walls emerging from ground-level mist are extraordinary. October and November are the most reliable months, when overnight temperatures in the canyon can drop to near freezing with sufficient river moisture. Fog events here rarely last past 9am before the high desert sun burns through completely.
Smith Rock fog is almost exclusively river canyon radiation fog. The Crooked River provides moisture to the canyon bottom, and on still, clear autumn nights when temperatures drop to near 0°C, that moisture condenses into ground fog that fills the canyon to about 30–50 meters depth. The surrounding high desert plateau stays clear and cold above the inversion. Wind of any kind kills the fog entirely — even 5 km/h is enough to mix the canyon air. Completely calm conditions at sunset are the clearest predictor of morning canyon fog.