The Making of Mt. San Jacinto
When the ground shakes the landscape moves up, down or sideways, or a combination of these. How did the granitic rocks of these mountains move up from perhaps 10 miles deep in the earth’s crusts to over 10,000 feet above sea level? What factors together did it and continue the uplift even as weathering and erosion tear them down. (see schedule for Part 2, The Destruction of the San Jacinto Mountains, September 8,) How much higher may San Jacinto peak be resulting from the inevitable “big one” on the southern San Andreas Fault? It could be none, to perhaps, 10 inches or more? I am betting it will be much more than “0”. There is recent precedence for such crustal uplift nearby. Are you ready for that one!? After the slideshow talk, we will check out some of the landforms in plain sight that tell us what has been happening over at least the last 5 million years when the earth shakes. It’s hardly an exaggeration to say it has changed everything. Find out how!
Date: Saturday, September 1
Time: 9:00 a.m. to about 12:00 p.m. First trams departs at 8 a.m. Arrive early.
Place: Tram mountain station, Nichols Room, two levels down from the tram exit to the ground floor on the left of the picnic patio.
Difficulty Level: easy to moderate
Distance: about 2 miles round trip
Destination: Grubb’s View and Long Valley
Preparation: It will be about 30 degrees cooler than the desert floor, dress accordingly. Bring water and consider snacks
Any questions please contact us at email@example.com
Present your NHA membership card and receive a 20% ticket discount on tram fare and 10% on food.
Booking: A reservation is required. Only one booking is permitted at a time. For more than one, simply fill out the form again with the information for each additional enrollee and submit. Overbookings will be waitlisted and if space becomes available enrollee will be notified in order of priority.