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We arrived in Phoenix on 02/21/02, and drove up to Sedona:
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Our first rest stop |
Movin right along |
Our first sighting of the red mts. I thought this was how the all looked. |
We made it to Sedona! The mountains are getting redder. |
A Tour Around Sedona
Sedona's famous formations have been slowly created for over 350
million years. From oceans to deserts to volcanic eruptions, Sedona's
geological events have been quite active, all contributing to the fascinating
vistas we see today. There are about ten various layers of sedimentary
rock signifying different geological events. Sedona's exceptional scarlet
color comes from the red iron-oxide stains formed when flood plain deposits of
iron minerals mixed with available oxygen at the time. Faulting helped the
creek waters to break through the lava cap and carve magnificent canyons.
We unpacked and went searching. |
It was hard to keep your eyes on the road |
Now that is red! This one is called Bell Rock. |
Joe had his conference so I ventured alone. I stopped when I saw this bridge and went the other way! |
McDonald's is not allowed to use their yellow arches, so they compromised. |
This is up at the Sedona airport. Looking out from the Masonic Temple. |
This is still from the airport. |
This is a Catholic church that is built into the red mountains |
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This is off to the right of the church. The column is called Madonna and Son |
![]() Close-up of Madonna and Son |
Site off of the left of the church |
![]() Rocks to the left back of the church. The eagle is a natural phenomium |
![]() Close-up of the eagle. |
Inside view of church looking at the alter. |
Our new home in the Red Rocks! |
DUH..... |
Back to the airport to watch the sunset. |
Isn't it gorgeous |
The sun goes down |
Go to Grand Canyon |
Did you know?
The sun shines an average of over 300 days of the year in Sedona, Arizona. More sunshine than Florida!
Arizona has more National Parks and National Monuments than any other state.
Sedona and Arizona have more mountainous countryside than Switzerland.
Sedona is located in the southern part of the largest stand of Ponderosa pines in the world.