Thursday, January 25, 2007
Turtle Head Peak
A view of turtle head peak. It's a fun hike in Red Rock Park, with some steep, rocky trails, but the view from the top is worth it. -Wendi
Tuesday, January 23, 2007
Monday, January 22, 2007
Wednesday, January 17, 2007
Vegas Valley
Monday, January 15, 2007
Friday, January 12, 2007
Duck Creek II
Thursday, January 11, 2007
Duck Creek
I went out to the Duck Creek trailhead, which is next to the wetlands park this week. It is located at the end of Tropicana on the east side of town, next to the UNLV stadium. The water district is reclamating the land, so they are revegitating the area. It was a haven for birds. It was a warm, beautiful day! -Wendi
Wednesday, January 10, 2007
Anniversary Narrows II
Tuesday, January 09, 2007
Anniversary Narrows
This picture is a play off of the pic Wendi took up at ice box canyon, just this one is in Anniversary Narrows. You can really see the different layers of sandstone, especially the green. I think the green is actually pumice, because I found a small fragment of pumice the same color further upstream. -Dave
Monday, January 08, 2007
Abandoned Mine
Hello Friends and LVDP viewers! We apologize for the great delay in a post! With the days being shortened, leaving town for the holidays, and both Christy and I being working women we have found it hard to take some picts! Our friend Dave also a local Las Vegan, has offered to help get some posts up! Thanks Dave!
This photo is of an abandoned mine shaft near Anniversary Narrows at Lake Mead. They used to mine for Borox and Calcite along with other minerals around this area. Note the how the layers of the earth are almost perpendicular to the ground! That is caused by major faulting in the area. The area around the shaft is mostly clay, but there are igneous intrusions (Where lava flowed up into cracks in the earth) and deposited calcite veins all through the hill. -Dave
This photo is of an abandoned mine shaft near Anniversary Narrows at Lake Mead. They used to mine for Borox and Calcite along with other minerals around this area. Note the how the layers of the earth are almost perpendicular to the ground! That is caused by major faulting in the area. The area around the shaft is mostly clay, but there are igneous intrusions (Where lava flowed up into cracks in the earth) and deposited calcite veins all through the hill. -Dave
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