Rattlesnake Ridge Interbed at Webber Canyon
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- Опубликовано: 29 авг 2024
- What the heck's an interbed? It's a geological layer between two other geologic units. In this case, it's a clay and silt layer sandwiched between two of the Columbia River Flood Basalts. It's full of cool soft-sediment deformation features and peperite! Pepperite? However you want to spell it.
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Very cool! Good video. Fun to see this ripple effect from the Pop-Up event. Thanks Patrick.
Thanks, Nick! Too bad about the Pop-Up broadcast issues, but what I could watch was interesting as usual. I hope to attend in person one of these days!
Thanks for your video and excellent description.
A nice addition to the story of Columbia flood basalt.
Every video you make is so educational. You and Jared from currently rockhounding, are so great at explaining and educating. And of course, you share a love of basalt! Thank you for all of your videos, and explaining what geological events, has left these cool features, we see today! Awesome!
Great video! The Rattlesnake interbed looks similarly brecciated at Gable Mountain on the Hanford Site. Palagonite/peperite, too. See Fecht (1978) "Geology of Gable Mtn - Gable Butte Area". The free PDF is online. Same invasion of Elephant Mtn basalt might also occur at Saddle Mts crest, a few miles east of Sentinel Pk. Tem there is overlain by an odd gray, slope-forming unit.
There must be some awesome agates sprinkled in that basalt. I was just waiting for you to find a nodule. I have seen some beautiful rocks from Saddle Mountain. Thank you for sharing.
This is awesome! Love the mini columns. Well done!
Thanks, your videos look interesting, too! Checking out the Crystal Cove one now.
nice video - subscribed and will check out your catalog.
Great Video
I would be interested to hear your interpretations of the basalts on my volcano. There is not an abundance of research to turn to, so one must use a lot of visual clues. I know it was a lacustrine environment and after hearing your explanations here, I see many similarities in the tumultuous basalt formations I see. I thought much of it to be pyroclastic, but perhaps some is peperite. Informative.
Neat. Do you ever find macro-fossils in the interbeds of clay?
Haven't looked, actually! This is a good teaching spot so I wouldn't want to mine out the clay. But there could be something. There was a rhino that got buried by flood basalts a bit further north.