[Google Groups told me I need an editor by not allowing me to send my previous post, so here is a shorter version]:
This past summer we found some lovely rocks (that are very similar to yours, Lisa) on the bank of the Mary's River. We also found some gorgeous crystals in some gravel we purchased from a nearby quarry, and due to an accident with a 4-year-old, a dishwasher, and these crystals, we were able to link the two! The first image attached is some rocks before cleaning (BC), and the second is after dishwasher (AD).
I now had another excuse to do a little internet 'digging' for rock origins (because it's a global pandemic and I have 2 small kids at home, and few other creative outlets).
This is what we came up with for our specimens: Oregon Coast zeolite. They are filamentous sodium calcium alumino-silicate crystals (which I just-so-happened to know LOTS about because we had just removed 65 garbage bags of asbestos-containing vermiculite removed from our new house, and I thought it prudent to know about zeolites). I can't pin down a more precise name, unfortunately, as these look like mesolite, thomsonite, and natrolite. (Despite being well-versed in biological taxonomy, the taxonomy of rocks completely eludes me.)
Regardless, as near as I can tell, they are formed by lower-temperature crystallization between bubbles made when underwater volcanoes burp up lava.
Here is a lovely picture of some zeolites in their native basalt up on Mary's Peak, which is exactly like what my gravel looks like (except in larger pieces). The pillow basalt they are cradled between is beautiful as well! The pillow basalt is from the Eocene
Siletz River Volcanics, which is an interesting bit all it's own. However,
one avenue of current thinking attributes these lava bubbles to a mantle plume, possibly the Yellowstone Hotspot! I'm rather excited that we managed to move to one of the few places where the Siletz terrane pokes up out of the ground for viewing, and that it's origin is still under active research. :)
It's a little surprising there isn't more about our pretty zeolites on the internet - they are so interesting looking. And no one we've asked (ok, we are still new here and know probably 4 people) seems to have noticed them?!? We may have to join the online show-and-tell 'Geology Rocks' meeting of GSOC (
Geological Society of the Oregon Country) this weekend. Or one of these days.
Lisa, I'm not sure this is what you have, but I thought I'd share.
All the best,
Tanya