 The Basins, or desert valleys of about 2,500 feet elevation, alternate with the Ranges, mountains of about 9,000 - 10,000 feet elevation. A colorful phrase credited to Major C.E. Dutton, an early explorer of the West, describes the mountain ranges as an "army
of caterpillars crawling northward out of Mexico." (King, 1977)
Unlike northern and central Arizona, these mountain ranges have formed by a geologic process known as block faulting, caused by stretching of the earth's crust in this region in the last 15 million years. The result is the mountains are isolated from each other. The mountains have been called sky islands, or mountain islands, surrounded by a vast sea of desert. The isolated flora and fauna on one mountain have had an opportunity to evolve differently than related flora and fauna on neighboring mountains. An example is the Mt. Graham red squirrel, which is somewhat different from the red squirrel of central Arizona. This small population of squirrels, occupying a tiny region on the top of Mt. Graham in the Pinalenos Mountains, almost threatened to wipe out the University of Arizona's plans to build a complex of telescopes on the mountain. In the end, the University won, and it is the Mt. Graham red squirrel that may be wiped out.
We visited Mt. Lemmon, in the Catalina Mountain range north of Tucson. Mt. Lemmon has its own isolated population of squirrels; the Arizona Gray squirrel here and in the Rincon Mountains differs slightly from the Arizona Gray squirrel in the Santa Rita, Huachuca, and Patagonia Mountains. In order to visit each other, the squirrels would have had to scamper down their respective mountains and across twenty miles of hot desert. The last time their populations might have intermingled might have been during the last glaciation, 11,000 years ago, when cooler temperatures might have lead to expanded forests and a grassland, instead of a desert, divide.
On a weekend in February, we did what the squirrels could not: we traveled from the desert around Tucson to the top of Mount Lemmon. Along the way, we traveled through four different life zones (as classified by Merriam): from desert upland, we traveled through
desert grassland-chaparral, oak woodland, Ponderosa pine forest, and mixed conifer forest.
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Beginning the drive up Mt. Lemmon Highway, we ascended through thick stands of saguaros until we reached the turnoff at Molino Basin at about 4000 feet. Getting out, we found a trail meandering among ocotillo, sotol, cane cholla, agave and yucca. There is a little more water in grassland-chaparral biomes than in pure desert-- about 12 to 15 inches a year-- but the rocky soil inhibits dense grass growth. Grasslands and chaparral burn periodically from fires caused by lightning strikes. Grasses recover quickly
by resprouting from their roots. The chaparral community, dominated by shrubs growing close together, have small, leathery, resinous leaves to inhibit water loss, and the resins make the plants extremely flammable. The shrubs are adapted to periodic fires; the seeds of many chaparral plants cannot germinate until they have been scorched by fire or at least baked in full sun in barren soil. Here at Molino basin, the chaparral shrubs are scrub oak, manzanita, turpentine bush, and Agave lechugilla (the evil Shin Dagger). We heard more birds than we saw, but I would guess the ones we heard were Mourning Dove, Curve-billed Thrasher, Say's Phoebe, and Cactus Wren. I spotted a whiptail lizard, one of the few that comes out in the middle of the day.
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