This was a fabulous interview. I love hearing Jamie talk. He’s so good at explaining difficult melts etc. thanks for having him. Learned a lot
@deborahferguson116312 күн бұрын
Agree!!!
@inqwit113 күн бұрын
This was awesome. I could almost follow what Jamie was saying.
@adamchaffee653613 күн бұрын
Jamie is fun and funny, and what a knack for explaining things simply! And this is meant to be a compliment to Nick for giving us more like him. Thank you.
@mikelouis938913 күн бұрын
The Pacific northwest is infinitely complex and thus, attracts the best geologists. Fantastic interview!
@joannekellam19113 күн бұрын
Fabulous convo with Jamie! He’s a real treat to listen to, so engaging and knowledgeable!
@kenmunozatmmrrailroad685313 күн бұрын
THIS WAS EXCELLENT Nick; he's as descriptive and easy to understand as you. Hopefully back again in the future!
@amacuro12 күн бұрын
Ok Jamie has become my new favorite guest. He likes to explain the basics, which is SOOOOO helpful!!! Thank you Jamie!! You gotta visit us more! Thanks for having Jamie, Nick, that was so interesting.
@garypaull938212 күн бұрын
What a ride! So much in this interview. I had no idea Persis spanned upwards of 10 million years. Glad to see Fuller Mtn make an appearance!
@hjumper823812 күн бұрын
As the fog I face slowly begins to clear, my feeling of understanding comforts my mind. Thank you, Nick and Jamie! Now I get to watch the next live broadcast N, Early Days of Cascades.
@charleymitchell546113 күн бұрын
Thanks to PBS, KSPS- Spokane for letting me find you years ago. Always great.
@jonathanblubaugh504912 күн бұрын
As always thank you for presenting Dr. MacDonald again. Home run, Nick. 🏆🏆
@_Michiel_12 күн бұрын
I love Jamie. He is só knowledgeable, has a knack of explaining complex subjects in understandable language without talking down and adds so many interesting details! I guess we all learnt a lot today! Thank you Jamie and Nick! ❤
@elainejones510913 күн бұрын
“Partially melted mantle makes mafic magma.” Great mnemonic!
@robmagee10013 күн бұрын
Oooo… fascinating discussion and mineralogy! Really enjoyed this. For a moment I had the feeling that I grasped how “paraluminous” minerals form in those particular environments. Ok, I heard Garnet, and I’m easily distracted by pretty, sparkly things… Still, it’s important as part of the complex interactions that were and are building our Pacific Northwest.
@OkkiePepernoot12 күн бұрын
What a great conversation! Very, very enjoyable and informative! Thank you, gentlemen!
@PlayNowWorkLater12 күн бұрын
Jamie is fantastic! I love the chemistry between you and him throughout this video. Thank you Nick. Hope to see more of Nick and Jamie videos in the future
@MellnikMary12 күн бұрын
Thanks Jamie! And Nick. So much enrichment in my life.
@lorrainewaters618913 күн бұрын
This is absolutely great! I am still trying to figure out adakites, and he is really helping. I gotta make dinner, so I'll be sure to watch the rest later. To get us exposed to more of these geologists is a true gift that you offer, Nick. thanks again
@kaywischkaemper425913 күн бұрын
So fired up to see the video with Jamie MacDonald. His GSA 2003 field trip guide of the Ingalls Ophiolite was so great to do when i visited you in 2023. You guys really had a great KZbin talking about the conditions for the presence of various rocks like the aluminum rich magmas and the Kay’rocks.
@chayachaya42012 күн бұрын
Wonderful discussion! So helpful in understanding adakites and the formation of igneous rocks in general. Thank you, Jamie and Nick!
@vugmeister91811 күн бұрын
As a mineral collector, I absolutely loved listening to this. The Persis Andesites are host to fabulous calcite and quartz crystals, zeolites, as well as petrified wood and jasper.
@dancooper855110 күн бұрын
Great interview! Put Jamie on your go to geochem list.
@donnparis13713 күн бұрын
Great video! May be my favorite of this recent series.
@judischarns450912 күн бұрын
Great interview! I hope to hear from him some more in the future.
@grandparocky13 күн бұрын
Thanks so much for your input Jamie!
@raenbow6613 күн бұрын
I always enjoy Jamie. It's great to see you both. I feel like I could follow and understand this discussion. Thank you very much.
@kban7713 күн бұрын
He speaks well
@ryanmarshall875813 күн бұрын
The melting mantle due to volatiles/flux description was eye opening for me. Good speaker Mr MacDonald
@ryanmarshall875813 күн бұрын
+slab subduction angle effects moving the volcanics geographicly💡
@yukigatlin935813 күн бұрын
That was very interesting!😃✨I got sucked in as Jamie spoke, thanks!!😆💞💛
@wiregold893013 күн бұрын
At least they didn't find peraluminous rocks on Chuginadak ... although Chuginadakite sounds like a heck of a drinking game.
@sharonseal915013 күн бұрын
What fun! I love these nice lively geology discussions and getting to know new geologists. The synergy is palpable when two minds meet to tackle an idea. Looking forward to where the alphabet is taking us nex, and learning new things! Thanks Nick and Jamie.
@Steviepinhead13 күн бұрын
Sensational stuff! Possibly worth creating a table of the different kind of melts and the suspected scenarios that relate to each: ridge, arc, subducting ridge, hotspot, etc.
@xwiick13 күн бұрын
Thanks for all the hard work on these videos!
@davec924413 күн бұрын
thank you both good job!
@ms_khoff13 күн бұрын
This video was incredibly engaging, interesting, and informative. I learned a lot! Thank you, both.
@jonathanblubaugh504912 күн бұрын
Fine. Mt. Persis volcanics 36-47MA. The subduction of the spreading center will naturally lead to a widening slab window, maybe faster than usual due to Kula/Resurrection northward sprint. Asthenospheric melting due to decompression is admitted. Thus the real question is how can NTM magma or Adakite genesis distinguished between spreading center subduction, a slab window, or slab breakoff?
@cyndikarp336812 күн бұрын
Jamie talk left me wanting to know more. He reviewed complex formations and transition to help solve complexities.
@pmgn844413 күн бұрын
Thanks Jamie and Nick. Very interesting as always. Ah yes, thought I've in WA for the last 30+ years, I lived in central FL in the late 70s to late 80s. So I understand Jamie's definition of 'cold.' I still laugh at it, but I understand it! 😁
@JoshExmoor13 күн бұрын
The Mt. Persis volcanics have intrigued me ever since I found the Maltby quadrant map which shows that essentially all of Lord Hill Regional Park near Monroe is exposed Persis rock including several visible dikes. This rock is easily viewed for those willing to walk around the park, but also visible from HWY 522 just east of the Snohomish river crossing on the north side of the road. It seems fairly unusual to have volcanic deposits this far west and the fact that they're so exposed in an area where glacial till is the norm also opens up some questions. I'd hoped to email you some photos in advance of you covering this topic, but I haven't had time to get out there this week and I'm thinking you'll probably beat me to the punch.
@susanwymer691212 күн бұрын
Finally, I have a better understanding of adakites and the relationship to the mantle and the plates! Thank you, Jamie! So in summation we have a melange of magma types as time goes forward. Could one say that?????
@jonathanblubaugh504912 күн бұрын
33:56 OK. so the slab angle is changing back an forth based on the surface expression of the arc. could that be due to folding of the lower slab as it makes ribbon candy? Or is that not relevant because Cascadia hugs the continental margin? or are we still too shallow and brittle?
@montejarvis13 күн бұрын
great interview! doesn't seem possible that as the ridge subducts it would continue to produce signatures of a ridge subduction as it goes on, while other areas like hanson lakes would have a slab beneath it. in otherwords both slab and no slab would be right next to each other and that window would last until the ridge stopped ridging.
@charlesflorian175813 күн бұрын
Two in one day, Thanks May have to watch replay. Woke to freezing fog this morning. Tri-Cites roads were a mess.
@KSparks8013 күн бұрын
Thx, Nick.
@kban7713 күн бұрын
Can the slab window just simply be a spreading ridge which also implies transform boundary parts as well. Divereg-transform-diveregw-etc
@janetcollins112913 күн бұрын
"that guy " great guest :) thk u
@Dragrath17 күн бұрын
The Mendocino triple Junction hmm does Lassen Peak have any of this Adakite chemistry? I did find that the Clear Lake volcanic field has Adakites soo I guess its a question of how far from the trench do the Adakites from the slab window reach? For the arc migration I can't help but think of Camp's Yellowstone hot spot slab break and associated rollback Shoshonite huh that is what Vesuvius and Campei Flegrei's primitive melts appear to be I think those typically come from oceanic arcs typically right? Do we know why those settings tend to produce alkaline and more specifically potassium rich alkaline melts?
@ms_khoff13 күн бұрын
Jamie, don’t feel bad-I wear layers or sweatshirts anytime it is cooler than 70-deg F (I am in Belvedere, CA and went to college in FL at ERAU) 😎
@kban7713 күн бұрын
How does this compare to volcanic patterns in places like, indonesia for example?
@montanawardog13 күн бұрын
Well, we get two extra credit conversations today!!
@ssgtmole861012 күн бұрын
"Melt a mafic magma" - sounds like a tongue twister. 😅
@williamwood994813 күн бұрын
"Flux"! Damn, this is good coffee!
@lauram947813 күн бұрын
❤❤
@guytowers923613 күн бұрын
Wow, a petrologic nerd. Jamie has a Tesla level infatuation with rock formation that rubs off, I think I just had a 301 level class in rock chemistry
@BLSKYZ13 күн бұрын
So true! I felt the same and I haven’t taken geology coarses!
@johnplong364413 күн бұрын
What 2 videos in one day?? I haven’t even watched the first one with Erin Donaghy