We also viewed a full-size replica of the White House Oval Office, the office in which President Reagan never took off his suit jacket. Len even stepped up to the podium and threw his hat in the ring for the next president. We also ate lunch at the Regan Country Café, good burgers and garlic fries, while we were visiting the library.
One day we took a drive to the Devil's Punchbowl, The most conspicuous features of the park are geological. The Punchbowl is a deep canyon cut by the runoff of large quantities of water from the higher San Gabriel Mountains occurring over a long period of time. These mountain peaks above the park are 8,000 feet in elevation while the Nature Center is located at 4,740 feet above sea level. The Punchbowl Canyon is 300 feet deep at the vista point. The peculiar up tilted rock formations to be seen in the entire area are layers of sedimentary rocks that were formed long ago by the depositing of loose material in horizontal layers by water. Later they were squeezed into their present steeply-tilted form by the continuing action of uplift along the Punchbowl and Pinyon Faults and pressures along the San Andreas Fault. The Punchbowl Fault is to the south of the rock formation while the Pinyon and San Andreas Faults are to the north.
Along the way we stop to view the Joshua's trees that were in bloom, there is a totally different look to the desert when it is in bloom. I find it beautiful.
Tuesday will be another moving day, stay tune to our next stop.
One day we took a drive to the Devil's Punchbowl, The most conspicuous features of the park are geological. The Punchbowl is a deep canyon cut by the runoff of large quantities of water from the higher San Gabriel Mountains occurring over a long period of time. These mountain peaks above the park are 8,000 feet in elevation while the Nature Center is located at 4,740 feet above sea level. The Punchbowl Canyon is 300 feet deep at the vista point. The peculiar up tilted rock formations to be seen in the entire area are layers of sedimentary rocks that were formed long ago by the depositing of loose material in horizontal layers by water. Later they were squeezed into their present steeply-tilted form by the continuing action of uplift along the Punchbowl and Pinyon Faults and pressures along the San Andreas Fault. The Punchbowl Fault is to the south of the rock formation while the Pinyon and San Andreas Faults are to the north.
Along the way we stop to view the Joshua's trees that were in bloom, there is a totally different look to the desert when it is in bloom. I find it beautiful.
Tuesday will be another moving day, stay tune to our next stop.
