No Fires - Fire Danger EXTREME - No Fuego
No Fires in the campground, no smoking on the trails. Observe these rules to protect park resources. No se permite fumar en los senderos, tampoco se permite las fogatas en el campamento. Proteja los recursos del parque y respete las advertencias. More »
Fee Increase at Pinnacles National Park
On August 1, 2014 the 7 day entrance pass for Pinnacles National Park will increase to $10 for passenger vehicles and motorcycles; bicycle and pedestrian entry will increase to $5.00. The Pinnacles Annual Pass will increase on August 1 to $20.00. More »
The faults within the Park mark distinct boundaries in geology. The Pinnacles Fault juxtaposes granitic basement rock west of the fault and the Pinnacles Volcanic Formation east of the fault. The Chalone Creek fault juxtaposes the Pinnacles Volcanic Formation west of the fault and the Temblor Fanglomerates east of the fault.
The granitic basement is the Santa Lucia Granite and Granodiorite. These granites formed when masses of molten lava slowly cooled as they rose through the earth’s crust to a point where they completely solidified. A slow cooling process allows individual crystals to grow fairly large. Subsequent uplift from faulting and erosion of overlying material exposed these rocks at the earth’s surface. These are the oldest rocks in the park, 78-100 million years old. They form the basement upon which the rest of the rocks at the Park lie.
The Pinnacles Volcanic Formation formed approximately 23 million years ago as it was extruded and deposited atop the granitic basement. The magma that was the source of all the volcanics was rhyolitic in origin. The formation consists of rocks such as banded and massive rhyolite, some andesites and dacites and various pyroclastic units.
The High Peaks consists of a relatively strong, well-consolidated breccia. The layers of breccias are thought to have formed as the result of material slumping off the sides of the volcano near the vents causing large landslides. The volcano was likely near water and the landslides traveled as massive turbidity currents under water that spread the material considerable distances until coming to rest near distant edges of the volcano. Volcanic ash and rhyolitic lava flows are interlayered with these breccias. Subsequent burial and compaction hardened these layers into the consolidated rock we see today. Recent faulting, fracturing and erosion have sculpted these rock layers into vertical cliffs and spires sometimes several hundred feet high.
The Temblor Formation east of the Chalone Creek Fault is a fanglomerate unit (conglomerates deposited in an alluvial fan setting) composed of granitic and to a lesser extent volcanic detritus shed from the Santa Lucia granitic basement and the Pinnacles Volcanics.
Rocks of Pinnacles
The following is an annotated list of common rock types at Pinnacles:
Breccia: Reddish to grey in color, molten rock is explosively ejected with many fragments welded into a lava or tuff matrix. Breccia dominates the High Peaks and other megalithic formations.
Flow-banded Rhyolite: A viscous fine-grained lava, which develops stretch marks, analogous to pulling taffy as it cools.
Pumice Lapilli Tuff: A welded volcanic ash, made up of sand sized particles. One theory suggests that weathering of magnesium and chromium bearing minerals produces this green color. The Bear Gulch Nature Center is constructed of this rock.
Perlite: An opaque form of volcanic glass which cooled rapidly in water.
Dacite: A light colored lava containing high proportions of quartz and feldspar. At Pinnacles it is associated with dikes.
Andesite: Similar to dacite, this rock has more dark colored minerals.
Sources for Further Reading
Did You Know?
Rhyolitic breccia is the rock that the High Peaks and other rock formations at Pinnacles are made of. Rhyolite breccia is composed of lava sand, ash, and angular chunks of rock that were explosively ejected from the Pinnacles Volcano.