Saturday, April 22, 2006

Palo Verde and Rhyolite Tuff

The rhyolite Tuff in the background is from the same event as the stripe on Pass Mountain, I'm told. Rhyolite like this stuff forms when an explosive eruption hurls lava high into the atmosphere. If it's still hot enough when it falls, it welds together and forms "tuff" (which is fairly soft rock).

The Palo Verde blooms bright yellow if there's enough water around. Posted by Picasa

Salt River Canyon

The narrow canyon cut by the Salt River through the Goldfield Mountains made for a long skinny lake. In the narrower parts the rock goes into the water straight down 80 or 90 feet. Posted by Picasa

Four Peaks from Saguaro Lake

Saguaro Lake is the westernmost in a string of four reservoirs along the Salt River east of Phoenix. The other three, west to east, are Canyon, Apache and Roosevelt.

Roosevelt Lake was once the largest man-made lake in the world, and had the tallest masonry dam. To travel from Canyon to Roosevelt, you must drive the Apache Trail, which is a one-lane dirt road much of the way.

The string of lakes provides both power and water for the Phoenix area. Posted by Picasa

Wednesday, April 12, 2006

Palo Verde and Saguaro

The tree in full bloom is a Palo Verde. They are interesting trees in that they have green bark. If there's a lack of water, they drop all their leaves and do photosynthiesis through their bark. Posted by Picasa

Cactus Gone Wonky

I think this is a "cristate" form, like the crested saguaro I posted a while back. This one is in the Park of the Canals in Mesa. Posted by Picasa

Papago Park Pool

Taken from the Hole in the Rock. Tempe is the town in the background. Posted by Picasa