I'm a total science nerd, especially Earth sciences, and especially all kinds of geography, who is to disabled to go crawling around on road cuts myself, or take most geology field classes. But thanks to people like you, I can still do learning and wallow in Earth science, and I really appreciate it.
I am totally amazed. I spent a good amount of time during in my childhood at Bumping Lake and Yakima. I do not remember ever hearing about Nile or seeing the formations. Thank You for taking us there.
What a great present Nick, 3 videos for Christmas. This is so visually integrating; talk is one thing, yet pictures give the mind some grist to work with when imagining the topics up for discussion. You are doing a magical service to our geological milieu. Thanks~!
One of the phenomena you can see in the debris flows of Illgraben that drains into the Rhône River in the Alps is debris flows that start out with massive boulder fronts, with boulders up to 150 tonnes, and then transition to periodic surging slurries of sand and gravel and clay. A flow may scour a deep channel in the bed and levee deposits during the boulder phase that refills with smaller clasts towards the end of that event, or during the next event that is different in nature due to amount of rainfall, or perhaps the side canyon that is providing the bulk of the water and debris from heavy thunderstorms that are limited in area. The Illgraben drainage dumps into the Rhône and sometimes establishes a large alluvial fan out into the main stream of the the Rhône, forcing the main stream against the opposite bank. Then the fan is re-mobilized and removed by the larger stream, or modified by subsequent flows. As the flows decrease in volume, debris is stranded in the channel as bed deposits, gravel bars and levee deposits. The next flow will re-mobilize and entrain the stranded bed load and carry it further down the drainage until it reaches the Rhône. At 13:57 the cross section of the lahar deposit is a dead ringer for the fan deposits dumped into the Rhône. On of the things that is interesting is that authorities have installed “drop structures” several meters high to reduce the velocity of flows via turbulent friction. As the boulders crash together at the bottom of the drop, in the middle of a MUD FLOW, the impact jets puffs of what appears to be ROCK DUST out of the mud flow. It would not take too many kilometers of violent transport to round the corners off of even the hardest rocks. The Alps are badly sheared “ugly” rocks that amply demonstrate the increased rates of erosion caused by tectonic increases in topographic relief and stream gradients.
We all have plans and hope for things for work and hobbies that we want to get done one day. Well Nick. You have been getting to those things done for the last few years. Aint lerning phun
Happy Christmas. Considering the paper on the car hood,: I'm glad you're not always driving a desk. But maybe a desk you can drive. Gorgeous views. Thanks Mr Zentner!
At the 35:00 minute mark, compare that deposit to what you have seen in field camps in the Mohave Desert on alluvial fans near Death Valley. Great variations in clast sizes, cross-bedding, and braided channels sweeping across the fans.
I really enjoyed this as it relates to Gary Smith's talk. Then, seeing the very interesting layers at Thorp and Nile! Whoever guessed geology could be so exciting?! (I laughed at "...I have a hammer..."). This spring...ok, Nick! 👍🏼
Another great field trip that exposes some of the beauty and geological past of this location. I am a longtime fan. I can never get tired of the field trips. This episode just seems to be too short ! 😊 As they say, "Time goes by too fast when you are having fun."
1:54 “You know the drill by now”, yes we do! You’ve taught us about the German chocolate cake many times ! Your presentation is consistent and makes perfect sense! Online nerd for 4 years in San Antonio! Luvya professor!
Merry Christmas, Nick! I was so surprised but very grateful to see you had uploaded a video today. I love your vision and have huge respect for your desire to review at older studies and question prior findings.
Really appreciate this video, much of which covers my backyard region outside of Naches. I have a few questions brewing on methods for determining lahar flow direction when originally deposited. Time to go do some reading….thanks Nick!
When you see ancient volcanic mudflows it really helps you comprehend how short the human experience has been in relation to geologic time. Thanks for taking us on a tour.
You're on the right track, now we just need to adjust those time distortions built into the foundation of GeoSci. Think real-time catastrophic cyclic events - like tree rings. Just sayin' = ) 💓LOVE your work Mr. Nick, thankU4 working towards integrating the narrative with your grounded and open-minded observations. You're my favorite teacher.
That Naches grade IS my back yard and I have some ground you could go beat on as long as you like don’t know how to contact you… I get close to the base of Mt. Clemands
Is that frothy pumice top a pyroclastic flow? I have heard that PC flows frequently have pinkish colors to them. We know that Mt. Pinatubo inter-beds pyroclastic flows with lahars especially when eruptions occur during tropical cyclones. If that pumice flow moved across the “grey sparkly sands” before it was consolidated, it could have mobilized some of the grey and barely mixed it into the bottom of the pumice flow. You need to drag Shawn Willsey up to that “random road cut!”
Can you tell the difference between a hot lahar caused by a heat event versus a coldahar of a massive mountain landslide say due to an overabundance of moisture causing liquefaction and then a lahar event? Admittedly I'm not a geologist but I'm trying to think of a way that you could transport the material in a cold state and still have the same effect meaning a volcano absorbing tons of water from an ice age and as things warm up it collapses but I can be corrected I love your videos cuz you asked so many questions it makes me start thinking about the stuff.
Long time Ellensburg native here, I do not see any mention of well logs in your videos. Seems that they would be a prime source of ground strata information. The well log for our property goes down over 300 feet. Other wells in our immediate area go down to over 700 ft. Just an idea.
Do any western rock tumblers think the force of being carried in a lahar could round off rocks freshly exploded out of a volcano in the time the lahar was moving?
This site certainly needs to be protected to make sure its geology features are not disturbed and kept as is for further studies and world heritage site.
It seems to me if that a fellow horror travels the same route multiple times in different events that it would become erosive picking up material that was already in place and carrying that onwards too. So there you get your big rounded material. I know expert on this but the heavier material and a hard would be at the bottom and they soft light stuff would be on the top and that's how you would tell if a Lahore was intact or if a subsequent heart took the top of the older off and carried it on to make a new deposit. Love to be corrected if I'm wrong
Great video! Very familiar with Nile. Quick question. When you come down the east side of 410 from the summit there is a mine shaft heading into the mountain. Any idea what they were looking for?
Lahar flows coming down off of a volcano will usually follow old creek and river beds. (the low spots) where it can pick up the rounded rocks. Not sure if a lahar flow has the time or distance needed to form any "newer" rocks into round cobbles.
@@KSparks80 I'm just an armchair geologist, K, I imagine hot material rolling down a 14k volcano and traveling tens of miles would be enough to round off some corners. IDK. Most of the bigger rocks in the second exposure, Natches, while large, none have sharp corners. These lahars are very voluminous, seemingly spreading out in an apron not just following a narrow valley. Or?
re Thorp and the Hwy 10 geology - this intersects with one of your prior talks about the east-tilted layer cake from Teanaway and towards Ellensburg. How does all this intersect (so to speak)? ua-cam.com/video/j8BFvKoabJ0/v-deo.html
Lahars seem difficult to learn about, they can pick up various rocks from wherever they go through and mix everything. So you are left with puzzle pieces, and ask yourself : where did this come from ? Answer in February 2025...
Days or weeks, months of light(ish) accumulation followed my a larger eruption covering the lighter deposits. Kind of like the last cement truck had all the big rocks. It's one pour, but not.
95% of drivers have no idea what is under foot. Great info presentation. You are a treasure. Thank you
I'm a total science nerd, especially Earth sciences, and especially all kinds of geography, who is to disabled to go crawling around on road cuts myself, or take most geology field classes. But thanks to people like you, I can still do learning and wallow in Earth science, and I really appreciate it.
I HAVE NOT SEEN THE NACHES GRADE FOR 70 YEARS SO THANKS
Merry Christmas Nick.
Just by the way.
I am totally amazed. I spent a good amount of time during in my childhood at Bumping Lake and Yakima. I do not remember ever hearing about Nile or seeing the formations. Thank You for taking us there.
What a great present Nick, 3 videos for Christmas. This is so visually integrating; talk is one thing, yet pictures give the mind some grist to work with when imagining the topics up for discussion. You are doing a magical service to our geological milieu. Thanks~!
One of the phenomena you can see in the debris flows of Illgraben that drains into the Rhône River in the Alps is debris flows that start out with massive boulder fronts, with boulders up to 150 tonnes, and then transition to periodic surging slurries of sand and gravel and clay.
A flow may scour a deep channel in the bed and levee deposits during the boulder phase that refills with smaller clasts towards the end of that event, or during the next event that is different in nature due to amount of rainfall, or perhaps the side canyon that is providing the bulk of the water and debris from heavy thunderstorms that are limited in area.
The Illgraben drainage dumps into the Rhône and sometimes establishes a large alluvial fan out into the main stream of the the Rhône, forcing the main stream against the opposite bank. Then the fan is re-mobilized and removed by the larger stream, or modified by subsequent flows.
As the flows decrease in volume, debris is stranded in the channel as bed deposits, gravel bars and levee deposits. The next flow will re-mobilize and entrain the stranded bed load and carry it further down the drainage until it reaches the Rhône. At 13:57 the cross section of the lahar deposit is a dead ringer for the fan deposits dumped into the Rhône.
On of the things that is interesting is that authorities have installed “drop structures” several meters high to reduce the velocity of flows via turbulent friction. As the boulders crash together at the bottom of the drop, in the middle of a MUD FLOW, the impact jets puffs of what appears to be ROCK DUST out of the mud flow. It would not take too many kilometers of violent transport to round the corners off of even the hardest rocks.
The Alps are badly sheared “ugly” rocks that amply demonstrate the increased rates of erosion caused by tectonic increases in topographic relief and stream gradients.
Not only a Tall Strata Volcano, major slope, but also the Volume Nick!
We all have plans and hope for things for work and hobbies that we want to get done one day. Well Nick. You have been getting to those things done for the last few years. Aint lerning phun
Thank You for reporting the formations of our Washington State terrain. ♥️🙏 Merry Christmas⛄️❄️
Nick. Thank you
What beautiful light you had! Thanks for taking us along.
I am loving this exploration.
Merry Christmas. Nice treat video.
Great stocking stuffer Nick, thank you. Merry Christmas. 🎉
Thanks Nick I have wondered too where the Thorp lahar originated from too, You sure have my attention.
Happy Christmas. Considering the paper on the car hood,: I'm glad you're not always driving a desk. But maybe a desk you can drive.
Gorgeous views. Thanks Mr Zentner!
At the 35:00 minute mark, compare that deposit to what you have seen in field camps in the Mohave Desert on alluvial fans near Death Valley. Great variations in clast sizes, cross-bedding, and braided channels sweeping across the fans.
Thank you for showing these incredible geology treasures omg. I am blown away thanks again. Merry Christmass.
Every time I go up the Rattlesnake drainage in the Nile, I marvel at the cliffs - apparently, the Ellensburg Formation. Thanks for talking about them!
I really enjoyed this as it relates to Gary Smith's talk. Then, seeing the very interesting layers at Thorp and Nile! Whoever guessed geology could be so exciting?! (I laughed at "...I have a hammer..."). This spring...ok, Nick! 👍🏼
Great Christmas present from you! Thank you!!
Right on! 😁💛 Merry Christmas and thank you for the video. 🌟
Merry Christmas and Happy New Year!!
Merry Christmas! TY NICK! Praying for a wonderful new year , health for you and yours and for the rest of this year’s A-Z! Keep em coming!
It was a really nice sunny day to see these not often talked about by anyone but geologists formations. Merry Christmas to
you Nick and family.
Merry Christmas Nick
Great video.MerryChristmas!
Another great field trip that exposes some of the beauty and geological past of this location.
I am a longtime fan. I can never get tired of the field trips. This episode just seems to be too short ! 😊
As they say, "Time goes by too fast when you are having fun."
Thanks for the wonderful field trip today.
Thank you Nick for the explanation of the Elensburg formation! Looking forward to hearing more.!!
Much better Christmas present than the model airplane I got from my wife. Thanks for everything you do Nick.
Thanks for all the hard work on these videos!
1:54 “You know the drill by now”, yes we do! You’ve taught us about the German chocolate cake many times ! Your presentation is consistent and makes perfect sense! Online nerd for 4 years in San Antonio! Luvya professor!
Thank you and Happy Christmas.
Really, really cool
Nice video for Christmas Day - Thanks
Field trip time with Nick Zentner, Merry Christmas!
Merry Christmas, Nick! I was so surprised but very grateful to see you had uploaded a video today. I love your vision and have huge respect for your desire to review at older studies and question prior findings.
Wow My Home Town Merry Christmas!!
This is a very interesting formation and story. Thank you Nick and Merry Christmas
Geology is so cool when seeing it through Nick Zentner’s eyes. 😊
Really appreciate this video, much of which covers my backyard region outside of Naches. I have a few questions brewing on methods for determining lahar flow direction when originally deposited. Time to go do some reading….thanks Nick!
Thank you for the video and Merry Christmas to you and your family 😊
Jack Powell took our YVC Geology class to the Naches Grade 30+ years ago. Amazing then and still is now!
I agree. Frothy pumice layer was floating on the lower lahar layer.
When you see ancient volcanic mudflows it really helps you comprehend how short the human experience has been in relation to geologic time. Thanks for taking us on a tour.
Happy Christmas professor Nick ❤ and family
Beautiful Vistas
You're on the right track, now we just need to adjust those time distortions built into the foundation of GeoSci.
Think real-time catastrophic cyclic events - like tree rings.
Just sayin' = )
💓LOVE your work Mr. Nick, thankU4 working towards integrating the narrative with your grounded and open-minded observations. You're my favorite teacher.
Great Christmas video
Brown upper gravel at Naches grade above pumicious sand and its frothy upper looks to be, at least in part, a debris flow.
That Naches grade IS my back yard and I have some ground you could go beat on as long as you like don’t know how to contact you… I get close to the base of Mt. Clemands
Are all the mud flows dipping East?
Yes. Let's get started.
There is always something new t o learn
Back yard Geology a new series? thank you good job.
Is that frothy pumice top a pyroclastic flow? I have heard that PC flows frequently have pinkish colors to them. We know that Mt. Pinatubo inter-beds pyroclastic flows with lahars especially when eruptions occur during tropical cyclones. If that pumice flow moved across the “grey sparkly sands” before it was consolidated, it could have mobilized some of the grey and barely mixed it into the bottom of the pumice flow.
You need to drag Shawn Willsey up to that “random road cut!”
Or, if required, a solid NEE HA! always works for me.
Can you tell the difference between a hot lahar caused by a heat event versus a coldahar of a massive mountain landslide say due to an overabundance of moisture causing liquefaction and then a lahar event? Admittedly I'm not a geologist but I'm trying to think of a way that you could transport the material in a cold state and still have the same effect meaning a volcano absorbing tons of water from an ice age and as things warm up it collapses but I can be corrected I love your videos cuz you asked so many questions it makes me start thinking about the stuff.
Interesting video Nick! So there is a secret road between Kittitas Valley and 410!
Once they're way, way back in the past, lahars are cool!
Long time Ellensburg native here, I do not see any mention of well logs in your videos. Seems that they would be a prime source of ground strata information. The well log for our property goes down over 300 feet. Other wells in our immediate area go down to over 700 ft. Just an idea.
Was slow getting to this video because I was watching the Itchy Boots stolen bike episode...
Do any western rock tumblers think the force of being carried in a lahar could round off rocks freshly exploded out of a volcano in the time the lahar was moving?
This site certainly needs to be protected to make sure its geology features are not disturbed and kept as is for further studies and
world heritage site.
With our new understanding of chemistry evidence we may be able to tie them together!
Could the frothy pumice deposit be a ash flow deposit instead of a lahar
It seems to me if that a fellow horror travels the same route multiple times in different events that it would become erosive picking up material that was already in place and carrying that onwards too. So there you get your big rounded material. I know expert on this but the heavier material and a hard would be at the bottom and they soft light stuff would be on the top and that's how you would tell if a Lahore was intact or if a subsequent heart took the top of the older off and carried it on to make a new deposit. Love to be corrected if I'm wrong
Great video! Very familiar with Nile. Quick question. When you come down the east side of 410 from the summit there is a mine shaft heading into the mountain. Any idea what they were looking for?
Why there are larg areas without trees? Too coarse land? Too acid? Forest fire? I see treeline climbing up to hill but thin line.
Dry climate east of Cascades- sagebrush and grass, not trees.
@@richarddavies7419 Pine wood do not need much water.
Seems like Ellensburg is built on old lake beds? Pretty weak material, only some basalts? How would your town react from large earthquakes
Couldn't the roiling action inside the lahar produce rounded stones?
Lahar flows coming down off of a volcano will usually follow old creek and river beds. (the low spots) where it can pick up the rounded rocks. Not sure if a lahar flow has the time or distance needed to form any "newer" rocks into round cobbles.
@@KSparks80 I'm just an armchair geologist, K, I imagine hot material rolling down a 14k volcano and traveling tens of miles would be enough to round off some corners. IDK. Most of the bigger rocks in the second exposure, Natches, while large, none have sharp corners. These lahars are very voluminous, seemingly spreading out in an apron not just following a narrow valley. Or?
re Thorp and the Hwy 10 geology - this intersects with one of your prior talks about the east-tilted layer cake from Teanaway and towards Ellensburg.
How does all this intersect (so to speak)?
ua-cam.com/video/j8BFvKoabJ0/v-deo.html
Random: can we have an episode about Bijou?
Try coordinating your HaYAH! with the hammer strike.🤣 Martial arts 101.🙃
Looks like basalt stones mixed with glacier tills.
Lahars seem difficult to learn about, they can pick up various rocks from wherever they go through and mix everything. So you are left with puzzle pieces, and ask yourself : where did this come from ? Answer in February 2025...
Days or weeks, months of light(ish) accumulation followed my a larger eruption covering the lighter deposits.
Kind of like the last cement truck had all the big rocks. It's one pour, but not.