Geology of Benson Lk. map published and free
- mokelumnekid
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Geology of Benson Lk. map published and free
See this link:
http://www.geosociety.org/maps/2012-DMCH013/" onclick="window.open(this.href);return false;
http://www.geosociety.org/maps/2012-DMCH013/" onclick="window.open(this.href);return false;
- rlown
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Re: Geology of Benson Lk. map published and free
Oh great wizard, I've looked at the map. Now explain it to us in layman's terms. I read the notes, but I love personal narration. Is this subduction process in the past and what is Ma?
Does the intense amount of Kyvg to the west mean we've been pretty inactive lately, geologically speaking? Is there a timeline from A to B?
inquiring minds..
Russ
PS: I love these topics. I never know what I'm walking on sometimes..
Does the intense amount of Kyvg to the west mean we've been pretty inactive lately, geologically speaking? Is there a timeline from A to B?
inquiring minds..
Russ
PS: I love these topics. I never know what I'm walking on sometimes..
- mokelumnekid
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Re: Geology of Benson Lk. map published and free
Hi Russ:
As far as not knowing what we are walking in, that goes for all of us! The piece of the map that has all the interesting details around Benson Lk. is older than the "granites" that we are accustomed to. They represent packages of much older sedimentary rocks that may have been translated northward from the Mojave area along a fault system that was subsequently obliterated by the intrusion of all the granitic rocks. So if nothing else, when visiting Benson marvel at how they are different from the typical flavors of granite that we normally see. "Ma" refers to millions of years. These dates are new and based on cutting edge techniques that are much more accurate than the previous methods.
One interesting debate is what the mapped extent granite bodies mean. They represent vast bodies of molten rock, but the issue is was the surface expression of this typical volcanoes like Shasta, or large calderas like Long Valley caldera that extends from east of Mammoth Lakes south to almost Bishop? Or perhaps even more like the huge caldera systems that one sees in the Altiplano-Puna regiuon of northern Chile today? My research has suggested the latter, but there is a lot we don't yet understand.
Most all the Sierra granitic rocks are old, from about 86 to over 100 million years old. The youngest ones are typically at the easternmost, higher part of the range and form distinct suites that all seem to have the diagnostic occurrence of those large pink feldspar crystals (climbers call them chicken heads'). There are at least four that have been called out:
1) The so-called granodiorite of Topaz Lake that has those big pink crystals extending from Topaz Lake well south from Sonora Pass and are well exposed in places in the deep heart of Ebbetts Pass and along eastern side of Monitor Passes and esp along Sonora pass Hwy near the top,
2) The so-called Cathedral Peak granodiorite that is well exposed through Tuolumne Meadows but actually goes all the way from Tower Peak to well south of Tuolumne, it is enormous.
3) Mono recesses, there is another unit in that area with the big pink crystals of feldspar
4) Mt Whitney area, again another enormous contiguous body with the same characteristics.
These are some of the largest distinct bodies of granite in the range and some of the youngest.
So the map from Benson Lake illustrates some of the complexity- a "raft" of older metamorphic rock surrounded by younger granitic bodies of disparate ages. One of the challenges in trying to sort out the detailed history is that the intrusion of the big granite bodies pretty much obliterates all that has gone before....
As far as not knowing what we are walking in, that goes for all of us! The piece of the map that has all the interesting details around Benson Lk. is older than the "granites" that we are accustomed to. They represent packages of much older sedimentary rocks that may have been translated northward from the Mojave area along a fault system that was subsequently obliterated by the intrusion of all the granitic rocks. So if nothing else, when visiting Benson marvel at how they are different from the typical flavors of granite that we normally see. "Ma" refers to millions of years. These dates are new and based on cutting edge techniques that are much more accurate than the previous methods.
One interesting debate is what the mapped extent granite bodies mean. They represent vast bodies of molten rock, but the issue is was the surface expression of this typical volcanoes like Shasta, or large calderas like Long Valley caldera that extends from east of Mammoth Lakes south to almost Bishop? Or perhaps even more like the huge caldera systems that one sees in the Altiplano-Puna regiuon of northern Chile today? My research has suggested the latter, but there is a lot we don't yet understand.
Most all the Sierra granitic rocks are old, from about 86 to over 100 million years old. The youngest ones are typically at the easternmost, higher part of the range and form distinct suites that all seem to have the diagnostic occurrence of those large pink feldspar crystals (climbers call them chicken heads'). There are at least four that have been called out:
1) The so-called granodiorite of Topaz Lake that has those big pink crystals extending from Topaz Lake well south from Sonora Pass and are well exposed in places in the deep heart of Ebbetts Pass and along eastern side of Monitor Passes and esp along Sonora pass Hwy near the top,
2) The so-called Cathedral Peak granodiorite that is well exposed through Tuolumne Meadows but actually goes all the way from Tower Peak to well south of Tuolumne, it is enormous.
3) Mono recesses, there is another unit in that area with the big pink crystals of feldspar
4) Mt Whitney area, again another enormous contiguous body with the same characteristics.
These are some of the largest distinct bodies of granite in the range and some of the youngest.
So the map from Benson Lake illustrates some of the complexity- a "raft" of older metamorphic rock surrounded by younger granitic bodies of disparate ages. One of the challenges in trying to sort out the detailed history is that the intrusion of the big granite bodies pretty much obliterates all that has gone before....
- chrisdiercks
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Re: Geology of Benson Lk. map published and free
I really enjoyed going over your map. Thanks for making it available. I had some questions earlier but was hesitant to ask at the time. Is the anticline easily observed from the lake, or do you really need to know what you are looking for. And I noticed your roof pendant contained andalusite, sillimanite (sometimes after andalusite), and cordierite in the mineral assemblages. I think we used to call this a shallow Abakuma-type metamorphism (I suppose I am showing my old college professors' bias but do they still call it that?), and can you recognize any lower to higher metamorphic grade patterns? After that I won't pester you. My hero back when was Hans Cloose; I really loved the highly deformed rocks. Really cool stuff. Nothing like getting paid to get some exercise.
old wannabe geologist
old wannabe geologist
- giantbrookie
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Re: Geology of Benson Lk. map published and free
Wow, what a nifty map. Vali, Scott et al. have much better field discipline than I do. A lot of potential field mapping time of mine would have been spent trying to see how large a fish I could catch out of Benson. Perhaps that is why I map in those terrible places with poison oak and ticks and all that. No distractions until I leave the field for those pints of IPA.
Since my fishing (etc.) website is still down, you can be distracted by geology stuff at: http://www.fresnostate.edu/csm/ees/facu ... ayshi.html" onclick="window.open(this.href);return false;
- mokelumnekid
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Re: Geology of Benson Lk. map published and free
GB knows more than he lets on! (BTW GB, Scott has the advantage on us that eh doesn't fish or drink).
These "roof pendants" like the one at Benson Lake have created quite a stir some years ago, as they suggested a previously unknown strike-slip fault that translated packages from (perhaps) as far south as the Mojave northward, although I have heard rumblings lately about some modification to that interpretation. In any event both GB and I can recommend additional reading but it will be of a rather technical nature. Just give a shout if interested.
These "roof pendants" like the one at Benson Lake have created quite a stir some years ago, as they suggested a previously unknown strike-slip fault that translated packages from (perhaps) as far south as the Mojave northward, although I have heard rumblings lately about some modification to that interpretation. In any event both GB and I can recommend additional reading but it will be of a rather technical nature. Just give a shout if interested.
- rlown
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Re: Geology of Benson Lk. map published and free
The more info you post that is free, the more we know and then you can answer our dullard questions. Tried getting to some papers before but they're all locked behind fees. All one can see is half of an abstract, on average.
It was very nice to get some background on what lies beneath our feet. Thanks!
Russ
It was very nice to get some background on what lies beneath our feet. Thanks!
Russ
- chrisdiercks
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Re: Geology of Benson Lk. map published and free
I would be very interested in something current discussing metamorphic facies and grades in that area or the Sierra in general. It's funny, I woke up last night thinking amphibolite. I'm with Russ in that I like to know what's under my feet and a bit about it.
- Troutdog 59
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Re: Geology of Benson Lk. map published and free
Thanks for posting the map Moke. Very nice indeed. I have always enjoyed the different rock types we travel through while backpacking. It was a significant factor in choosing geology as a major in college. While my business card calls me a Geologist, I am very much out of the loop these days with mapping, structural geology, and current lines of geologic thinking as I have been working in water quality for 20 years. That said, I did my undergrad thesis on the roof pendants further south around Bald Mountain in the Sequia National Forest and the Golden Trout Wilderness so I do understand this stuff, just rusty. Lots of calc silcate stuff down that way with some very nice garnets along the contacts and within the pendant itself. My first paying job as a Geo included alot of field mapping in the Santa Monica Mountains and we saw alot of nice fossil assembledges and faulting. While I loved being outside logging borings (downhole) and test pits, I didnt really enjoy the fact that the field work I was doing was leading to the increasing development of the area, so I swithched over to the water quality side of things. Very nice to get back to some real geology. Think I might even bring my hand lens and brunton with me on an inspection I have to do today .
Once in a while you can get shown the light
In the strangest places if you look at it right.
The Grateful Dead
In the strangest places if you look at it right.
The Grateful Dead
- sekihiker
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Re: Geology of Benson Lk. map published and free
Cool map. Having spent a summer field session mapping part of the Log Cabin Mine pendant, I know how difficult it was putting together something that coherent.
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