I was glad to see the blog on San Rafael Swell on Utah Astronomy. I am out of town sitting a 8,000 foot well and am forced to use web mail to respond to emails. I am coming home tonight and planned to respond when I get back, but Chuck Hards said "Calling Rodger Fry" forced me to crawl out of my shell. Here it is in a nutshell. The San Rafael Swell is a classic geologic dome or doubly plunging anticline. It was formed by tectonic east-west compressional forces during the Larimide Orogony which started about 68 million years ago. Without question, it isn't an impact crater but is a wonder in itself and I feel is Utah's best kept secret (lets keep it that way). About 68 million years ago, the Pacific crustal plate moved eastward pushing hard on the North American plate. This caused many events to occur two of which are subduction and the formation of thrust faults prevalent in Utah. and crustal compression forming features like the San Rafael Swell and the Rock Springs Uplift. In the San Rafael Swell, the youngest rocks are found on the outer ring of the swell which are the gray marine shales of the Mancos formation. Moving inward to the interior of the swell you go progressively deeper in the geologic section though older formations these including the Dakota sandstone, Morrison formation (famous for dinosaur bones), Entrata sandstone, Carmel formation, Navajo Sandstone (which forms most of the picturesque red-orange cliffs surrounding the swell), Wingate Sandstone, Chinle formation, Moencopi Sandstone and finally, the core of the swell has Permian age rocks, Paradox Formation, exposed. Other minor formations are present in this section. This is a truly remarkable place for anyone interested in geology. Many of the formations are fossil rich including Gryphea Newberri (oyster type molluscs) and Pyronocyclus Wyomingensus (large 2-foot diameter ammonites) in the Mancos Formation, Dinosaur bones in the Morrison Formation, Penticrinus (star crinoid stems-animals that lived on a stalk) in the Carmel Formation. It is a great place to just go and hang out. And for astronomy, the Wedge is located on the Western rim of the swell offers a great dark-sky site 2 1/2 hours from Salt Lake As far as Upheavel Dome. When I was in college as a geology major in the 1960's we took a field trip that included Upheavel Dome. At that time it was universally accepted that this was a salt diapir (intrusion). However, our professor offered an alternate hypothesis that it might be an impact crater which was marginally radical at the time. Many came away open to the fact that might be an impact crater me included. Since that time many studies have been conducted on this and other impact craters world wide and without a doubt, the evidence exists to support the impact crater hypothesis. As far as someone mentioning that Upheavel Dome has a central peak, keep in mind this is a very old impact crater that has been modified by erosian. Erosian has allowed resistive formations surrounding the crater to be cliff formers and the erodible formations to become valleys. The central peaks or highland areas of the dome is the evaporite rich Paradox formation of Permian age. Therefore, the central peak is an erosional feature. This has been a great blog that I have loved reading but not having easy access to email I missed out on most of the fun. I will be glad to be back in town and on-line again. Rodger Fry
I vote we plan a combined fossil hunt/star gaze sometime early or late summer (not too hot) with Roger down that way. I think it would be loads of fun. --- On Wed, 1/28/09, rcfry@comcast.net <rcfry@comcast.net> wrote:
From: rcfry@comcast.net <rcfry@comcast.net> Subject: [Utah-astronomy] San Rafael Swell To: utah-astronomy@mailman.xmission.com Date: Wednesday, January 28, 2009, 4:56 PM I was glad to see the blog on San Rafael Swell on Utah Astronomy. I am out of town sitting a 8,000 foot well and am forced to use web mail to respond to emails. I am coming home tonight and planned to respond when I get back, but Chuck Hards said "Calling Rodger Fry" forced me to crawl out of my shell.
Here it is in a nutshell. The San Rafael Swell is a classic geologic dome or doubly plunging anticline. It was formed by tectonic east-west compressional forces during the Larimide Orogony which started about 68 million years ago. Without question, it isn't an impact crater but is a wonder in itself and I feel is Utah's best kept secret (lets keep it that way).
About 68 million years ago, the Pacific crustal plate moved eastward pushing hard on the North American plate. This caused many events to occur two of which are subduction and the formation of thrust faults prevalent in Utah. and crustal compression forming features like the San Rafael Swell and the Rock Springs Uplift. In the San Rafael Swell, the youngest rocks are found on the outer ring of the swell which are the gray marine shales of the Mancos formation. Moving inward to the interior of the swell you go progressively deeper in the geologic section though older formations these including the Dakota sandstone, Morrison formation (famous for dinosaur bones), Entrata sandstone, Carmel formation, Navajo Sandstone (which forms most of the picturesque red-orange cliffs surrounding the swell), Wingate Sandstone, Chinle formation, Moencopi Sandstone and finally, the core of the swell has Permian age rocks, Paradox Formation, exposed. Other minor formations are present in this section. This is a truly remarkable place for anyone interested in geology. Many of the formations are fossil rich including Gryphea Newberri (oyster type molluscs) and Pyronocyclus Wyomingensus (large 2-foot diameter ammonites) in the Mancos Formation, Dinosaur bones in the Morrison Formation, Penticrinus (star crinoid stems-animals that lived on a stalk) in the Carmel Formation. It is a great place to just go and hang out. And for astronomy, the Wedge is located on the Western rim of the swell offers a great dark-sky site 2 1/2 hours from Salt Lake
As far as Upheavel Dome. When I was in college as a geology major in the 1960's we took a field trip that included Upheavel Dome. At that time it was universally accepted that this was a salt diapir (intrusion). However, our professor offered an alternate hypothesis that it might be an impact crater which was marginally radical at the time. Many came away open to the fact that might be an impact crater me included. Since that time many studies have been conducted on this and other impact craters world wide and without a doubt, the evidence exists to support the impact crater hypothesis. As far as someone mentioning that Upheavel Dome has a central peak, keep in mind this is a very old impact crater that has been modified by erosian. Erosian has allowed resistive formations surrounding the crater to be cliff formers and the erodible formations to become valleys. The central peaks or highland areas of the dome is the evaporite rich Paradox formation of Permian age. Therefore, the central peak is an erosional feature.
This has been a great blog that I have loved reading but not having easy access to email I missed out on most of the fun. I will be glad to be back in town and on-line again.
Rodger Fry _______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com
Let's keep our eyes open for ammonites. I was told about an area not far from Castle Dale where you can find 'em. The nice thing about shells like ammonites and the oyster beds is that it's legal to collect invertebrate fossils (within reason -- for your own enjoyment, not sale,and no more than something like 25 pounds at a time), while vertebrate fossils are off-limits. Also, if it happens to be state land you should get a collecting permit from the Division of Natural Resources. -- Joe --- On Wed, 1/28/09, Richard Tenney <retenney@yahoo.com> wrote: From: Richard Tenney <retenney@yahoo.com> Subject: Re: [Utah-astronomy] San Rafael Swell To: "Utah Astronomy" <utah-astronomy@mailman.xmission.com> Date: Wednesday, January 28, 2009, 5:03 PM I vote we plan a combined fossil hunt/star gaze sometime early or late summer (not too hot) with Roger down that way. I think it would be loads of fun. --- On Wed, 1/28/09, rcfry@comcast.net <rcfry@comcast.net> wrote:
From: rcfry@comcast.net <rcfry@comcast.net> Subject: [Utah-astronomy] San Rafael Swell To: utah-astronomy@mailman.xmission.com Date: Wednesday, January 28, 2009, 4:56 PM I was glad to see the blog on San Rafael Swell on Utah Astronomy. I am out of town sitting a 8,000 foot well and am forced to use web mail to respond to emails. I am coming home tonight and planned to respond when I get back, but Chuck Hards said "Calling Rodger Fry" forced me to crawl out of my shell.
Here it is in a nutshell. The San Rafael Swell is a classic geologic dome or doubly plunging anticline. It was formed by tectonic east-west compressional forces during the Larimide Orogony which started about 68 million years ago. Without question, it isn't an impact crater but is a wonder in itself and I feel is Utah's best kept secret (lets keep it that way).
About 68 million years ago, the Pacific crustal plate moved eastward pushing hard on the North American plate. This caused many events to occur two of which are subduction and the formation of thrust faults prevalent in Utah. and crustal compression forming features like the San Rafael Swell and the Rock Springs Uplift. In the San Rafael Swell, the youngest rocks are found on the outer ring of the swell which are the gray marine shales of the Mancos formation. Moving inward to the interior of the swell you go progressively deeper in the geologic section though older formations these including the Dakota sandstone, Morrison formation (famous for dinosaur bones), Entrata sandstone, Carmel formation, Navajo Sandstone (which forms most of the picturesque red-orange cliffs surrounding the swell), Wingate Sandstone, Chinle formation, Moencopi Sandstone and finally, the core of the swell has Permian age rocks, Paradox Formation, exposed. Other minor formations are present in this section. This is a truly remarkable place for anyone interested in geology. Many of the formations are fossil rich including Gryphea Newberri (oyster type molluscs) and Pyronocyclus Wyomingensus (large 2-foot diameter ammonites) in the Mancos Formation, Dinosaur bones in the Morrison Formation, Penticrinus (star crinoid stems-animals that lived on a stalk) in the Carmel Formation. It is a great place to just go and hang out. And for astronomy, the Wedge is located on the Western rim of the swell offers a great dark-sky site 2 1/2 hours from Salt Lake
As far as Upheavel Dome. When I was in college as a geology major in the 1960's we took a field trip that included Upheavel Dome. At that time it was universally accepted that this was a salt diapir (intrusion). However, our professor offered an alternate hypothesis that it might be an impact crater which was marginally radical at the time. Many came away open to the fact that might be an impact crater me included. Since that time many studies have been conducted on this and other impact craters world wide and without a doubt, the evidence exists to support the impact crater hypothesis. As far as someone mentioning that Upheavel Dome has a central peak, keep in mind this is a very old impact crater that has been modified by erosian. Erosian has allowed resistive formations surrounding the crater to be cliff formers and the erodible formations to become valleys. The central peaks or highland areas of the dome is the evaporite rich Paradox formation of Permian age. Therefore, the central peak is an erosional feature.
This has been a great blog that I have loved reading but not having easy access to email I missed out on most of the fun. I will be glad to be back in town and on-line again.
Rodger Fry _______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com
_______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com
As a kid, my dad used to haul me around the state looking for geological curiosities. Alas, I never picked up the interest he had, but I do remember him pointing out fossil shells in the rock formations in the canyons east of the SL valley. On Wed, Jan 28, 2009 at 6:52 PM, Joe Bauman <josephmbauman@yahoo.com> wrote:
Let's keep our eyes open for ammonites. I was told about an area not far from Castle Dale where you can find 'em. The nice thing about shells like ammonites and the oyster beds is that it's legal to collect invertebrate fossils (within reason -- for your own enjoyment, not sale,and no more than something like 25 pounds at a time), while vertebrate fossils are off-limits. Also, if it happens to be state land you should get a collecting permit from the Division of Natural Resources. -- Joe
What he said... -----Original Message----- From: utah-astronomy-bounces@mailman.xmission.com [mailto:utah-astronomy-bounces@mailman.xmission.com] On Behalf Of rcfry@comcast.net Sent: Wednesday, January 28, 2009 4:57 PM To: utah-astronomy@mailman.xmission.com Subject: [Utah-astronomy] San Rafael Swell I was glad to see the blog on San Rafael Swell on Utah Astronomy. I am out of town sitting a 8,000 foot well and am forced to use web mail to respond to emails. I am coming home tonight and planned to respond when I get back, but Chuck Hards said "Calling Rodger Fry" forced me to crawl out of my shell. Here it is in a nutshell. The San Rafael Swell is a classic geologic dome or doubly plunging anticline. It was formed by tectonic east-west compressional forces during the Larimide Orogony which started about 68 million years ago. Without question, it isn't an impact crater but is a wonder in itself and I feel is Utah's best kept secret (lets keep it that way). About 68 million years ago, the Pacific crustal plate moved eastward pushing hard on the North American plate. This caused many events to occur two of which are subduction and the formation of thrust faults prevalent in Utah. and crustal compression forming features like the San Rafael Swell and the Rock Springs Uplift. In the San Rafael Swell, the youngest rocks are found on the outer ring of the swell which are the gray marine shales of the Mancos formation. Moving inward to the interior of the swell you go progressively deeper in the geologic section though older formations these including the Dakota sandstone, Morrison formation (famous for dinosaur bones), Entrata sandstone, Carmel formation, Navajo Sandstone (which forms most of the picturesque red-orange cliffs surrounding the swell), Wingate Sandstone, Chinle formation, Moencopi Sandstone and finally, the core of the swell has Permian age rocks, Paradox Formation, exposed. Other minor formations are present in this section. This is a truly remarkable place for anyone interested in geology. Many of the formations are fossil rich including Gryphea Newberri (oyster type molluscs) and Pyronocyclus Wyomingensus (large 2-foot diameter ammonites) in the Mancos Formation, Dinosaur bones in the Morrison Formation, Penticrinus (star crinoid stems-animals that lived on a stalk) in the Carmel Formation. It is a great place to just go and hang out. And for astronomy, the Wedge is located on the Western rim of the swell offers a great dark-sky site 2 1/2 hours from Salt Lake As far as Upheavel Dome. When I was in college as a geology major in the 1960's we took a field trip that included Upheavel Dome. At that time it was universally accepted that this was a salt diapir (intrusion). However, our professor offered an alternate hypothesis that it might be an impact crater which was marginally radical at the time. Many came away open to the fact that might be an impact crater me included. Since that time many studies have been conducted on this and other impact craters world wide and without a doubt, the evidence exists to support the impact crater hypothesis. As far as someone mentioning that Upheavel Dome has a central peak, keep in mind this is a very old impact crater that has been modified by erosian. Erosian has allowed resistive formations surrounding the crater to be cliff formers and the erodible formations to become valleys. The central peaks or highland areas of the dome is the evaporite rich Paradox formation of Permian age. Therefore, the central peak is an erosional feature. This has been a great blog that I have loved reading but not having easy access to email I missed out on most of the fun. I will be glad to be back in town and on-line again. Rodger Fry _______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com No virus found in this incoming message. Checked by AVG. Version: 7.5.552 / Virus Database: 270.10.15/1921 - Release Date: 1/28/2009 6:37 AM No virus found in this outgoing message. Checked by AVG. Version: 7.5.552 / Virus Database: 270.10.15/1921 - Release Date: 1/28/2009 6:37 AM
I was just down at Café Rio and one of the workers had to break me out of my trance. I was watching the Salt Domes forming on the frying tortillas. I could see the Mexican crustal plate moved eastward pushing hard on the Gringo plate. Moving inward to the interior of the swell I could see the incline get progressively closer to the guacamole section. Then there was lettuce an salsa in the side section. Man that was awesome. Jim --- On Wed, 1/28/09, Kim <kimharch@cut.net> wrote: From: Kim <kimharch@cut.net> Subject: Re: [Utah-astronomy] San Rafael Swell To: "'Utah Astronomy'" <utah-astronomy@mailman.xmission.com> Date: Wednesday, January 28, 2009, 5:33 PM What he said... -----Original Message----- From: utah-astronomy-bounces@mailman.xmission.com [mailto:utah-astronomy-bounces@mailman.xmission.com] On Behalf Of rcfry@comcast.net Sent: Wednesday, January 28, 2009 4:57 PM To: utah-astronomy@mailman.xmission.com Subject: [Utah-astronomy] San Rafael Swell I was glad to see the blog on San Rafael Swell on Utah Astronomy. I am out of town sitting a 8,000 foot well and am forced to use web mail to respond to emails. I am coming home tonight and planned to respond when I get back, but Chuck Hards said "Calling Rodger Fry" forced me to crawl out of my shell. Here it is in a nutshell. The San Rafael Swell is a classic geologic dome or doubly plunging anticline. It was formed by tectonic east-west compressional forces during the Larimide Orogony which started about 68 million years ago. Without question, it isn't an impact crater but is a wonder in itself and I feel is Utah's best kept secret (lets keep it that way). About 68 million years ago, the Pacific crustal plate moved eastward pushing hard on the North American plate. This caused many events to occur two of which are subduction and the formation of thrust faults prevalent in Utah. and crustal compression forming features like the San Rafael Swell and the Rock Springs Uplift. In the San Rafael Swell, the youngest rocks are found on the outer ring of the swell which are the gray marine shales of the Mancos formation. Moving inward to the interior of the swell you go progressively deeper in the geologic section though older formations these including the Dakota sandstone, Morrison formation (famous for dinosaur bones), Entrata sandstone, Carmel formation, Navajo Sandstone (which forms most of the picturesque red-orange cliffs surrounding the swell), Wingate Sandstone, Chinle formation, Moencopi Sandstone and finally, the core of the swell has Permian age rocks, Paradox Formation, exposed. Other minor formations are present in this section. This is a truly remarkable place for anyone interested in geology. Many of the formations are fossil rich including Gryphea Newberri (oyster type molluscs) and Pyronocyclus Wyomingensus (large 2-foot diameter ammonites) in the Mancos Formation, Dinosaur bones in the Morrison Formation, Penticrinus (star crinoid stems-animals that lived on a stalk) in the Carmel Formation. It is a great place to just go and hang out. And for astronomy, the Wedge is located on the Western rim of the swell offers a great dark-sky site 2 1/2 hours from Salt Lake As far as Upheavel Dome. When I was in college as a geology major in the 1960's we took a field trip that included Upheavel Dome. At that time it was universally accepted that this was a salt diapir (intrusion). However, our professor offered an alternate hypothesis that it might be an impact crater which was marginally radical at the time. Many came away open to the fact that might be an impact crater me included. Since that time many studies have been conducted on this and other impact craters world wide and without a doubt, the evidence exists to support the impact crater hypothesis. As far as someone mentioning that Upheavel Dome has a central peak, keep in mind this is a very old impact crater that has been modified by erosian. Erosian has allowed resistive formations surrounding the crater to be cliff formers and the erodible formations to become valleys. The central peaks or highland areas of the dome is the evaporite rich Paradox formation of Permian age. Therefore, the central peak is an erosional feature. This has been a great blog that I have loved reading but not having easy access to email I missed out on most of the fun. I will be glad to be back in town and on-line again. Rodger Fry _______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com No virus found in this incoming message. Checked by AVG. Version: 7.5.552 / Virus Database: 270.10.15/1921 - Release Date: 1/28/2009 6:37 AM No virus found in this outgoing message. Checked by AVG. Version: 7.5.552 / Virus Database: 270.10.15/1921 - Release Date: 1/28/2009 6:37 AM _______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com
Boy Roger, I'm so glad you're on board. That's a fine explanation. My wife's uncle, Wally Hansen (a geologist in Colorado) is the one who told me the Swell was part of the Larimide Orogony. I'm glad to find out he was right, thought it would have been cool if the Reef was thrown up by a meteor. Thanks, Joe --- On Wed, 1/28/09, Kim <kimharch@cut.net> wrote: From: Kim <kimharch@cut.net> Subject: Re: [Utah-astronomy] San Rafael Swell To: "'Utah Astronomy'" <utah-astronomy@mailman.xmission.com> Date: Wednesday, January 28, 2009, 5:33 PM What he said... -----Original Message----- From: utah-astronomy-bounces@mailman.xmission.com [mailto:utah-astronomy-bounces@mailman.xmission.com] On Behalf Of rcfry@comcast.net Sent: Wednesday, January 28, 2009 4:57 PM To: utah-astronomy@mailman.xmission.com Subject: [Utah-astronomy] San Rafael Swell I was glad to see the blog on San Rafael Swell on Utah Astronomy. I am out of town sitting a 8,000 foot well and am forced to use web mail to respond to emails. I am coming home tonight and planned to respond when I get back, but Chuck Hards said "Calling Rodger Fry" forced me to crawl out of my shell. Here it is in a nutshell. The San Rafael Swell is a classic geologic dome or doubly plunging anticline. It was formed by tectonic east-west compressional forces during the Larimide Orogony which started about 68 million years ago. Without question, it isn't an impact crater but is a wonder in itself and I feel is Utah's best kept secret (lets keep it that way). About 68 million years ago, the Pacific crustal plate moved eastward pushing hard on the North American plate. This caused many events to occur two of which are subduction and the formation of thrust faults prevalent in Utah. and crustal compression forming features like the San Rafael Swell and the Rock Springs Uplift. In the San Rafael Swell, the youngest rocks are found on the outer ring of the swell which are the gray marine shales of the Mancos formation. Moving inward to the interior of the swell you go progressively deeper in the geologic section though older formations these including the Dakota sandstone, Morrison formation (famous for dinosaur bones), Entrata sandstone, Carmel formation, Navajo Sandstone (which forms most of the picturesque red-orange cliffs surrounding the swell), Wingate Sandstone, Chinle formation, Moencopi Sandstone and finally, the core of the swell has Permian age rocks, Paradox Formation, exposed. Other minor formations are present in this section. This is a truly remarkable place for anyone interested in geology. Many of the formations are fossil rich including Gryphea Newberri (oyster type molluscs) and Pyronocyclus Wyomingensus (large 2-foot diameter ammonites) in the Mancos Formation, Dinosaur bones in the Morrison Formation, Penticrinus (star crinoid stems-animals that lived on a stalk) in the Carmel Formation. It is a great place to just go and hang out. And for astronomy, the Wedge is located on the Western rim of the swell offers a great dark-sky site 2 1/2 hours from Salt Lake As far as Upheavel Dome. When I was in college as a geology major in the 1960's we took a field trip that included Upheavel Dome. At that time it was universally accepted that this was a salt diapir (intrusion). However, our professor offered an alternate hypothesis that it might be an impact crater which was marginally radical at the time. Many came away open to the fact that might be an impact crater me included. Since that time many studies have been conducted on this and other impact craters world wide and without a doubt, the evidence exists to support the impact crater hypothesis. As far as someone mentioning that Upheavel Dome has a central peak, keep in mind this is a very old impact crater that has been modified by erosian. Erosian has allowed resistive formations surrounding the crater to be cliff formers and the erodible formations to become valleys. The central peaks or highland areas of the dome is the evaporite rich Paradox formation of Permian age. Therefore, the central peak is an erosional feature. This has been a great blog that I have loved reading but not having easy access to email I missed out on most of the fun. I will be glad to be back in town and on-line again. Rodger Fry _______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com No virus found in this incoming message. Checked by AVG. Version: 7.5.552 / Virus Database: 270.10.15/1921 - Release Date: 1/28/2009 6:37 AM No virus found in this outgoing message. Checked by AVG. Version: 7.5.552 / Virus Database: 270.10.15/1921 - Release Date: 1/28/2009 6:37 AM _______________________________________________ Utah-Astronomy mailing list Utah-Astronomy@mailman.xmission.com http://mailman.xmission.com/cgi-bin/mailman/listinfo/utah-astronomy Visit the Photo Gallery: http://gallery.utahastronomy.com Visit the Wiki: http://www.utahastronomy.com
Roger and Kurt, would you consider putting all of this into a talk for a SLAS meeting? patrick
participants (7)
-
Chuck Hards -
Jim Gibson -
Joe Bauman -
Kim -
Patrick Wiggins -
rcfry＠comcast.net -
Richard Tenney