31 May 2016
Near Wilson Creek, Washington, we beheld a bright orange stripe on the cliff:
It’s a bold color, and it begs the question: What’s going on here?
Laterite, a tropical soil, has a similar color scheme, and I’ve seen laterite horizons sandwiched between lava flows before (e.g., at the Giant’s Causeway in northern Ireland). But when I zoomed in on this orange layer, it appeared to be vesicular basalt:
Can a basalt flow contact metamorphose an older basalt flow?
Maybe weathering is the key: So the story recorded here could therefore be: lava erupts, lava cools to basalt, basalt weathers from the top down, producing clay and rust-rich saprolite, new lava erupts, cooks weathered basalt beneath, baking it orange.
Other thoughts? Chime in.