Geology of “A” Mountain and Tumamoc Hillby Jonathan DuHamel on Jan. 17, 2011, under Geology
A group of hills including Sentinel Peak (aka “A” mountain) and Tumamoc Hill lie just west of Congress Street near downtown Tucson.
Sentinel Peak sports the “A” of the University of Arizona, and Tumamoc Hill is home to the Desert Laboratory, established in 1903 to study desert ecology.
These hills, composed of volcanic rocks, have a conical shape with a low area in the middle leading some people to think it was a volcano. But the hills are really an erosional remnant of volcanic flows about 20- to 30 million years old which once extended west to the Tucson Mountains and east into the valley towards downtown Tucson. These rocks overlie other volcanic rocks about 58 million years old.
The Arizona Geological Survey has a digital geologic map (DGM-29) and short explanation of the volcanic rocks. Following is an (abridged) description of units from top to bottom. The unit symbols refer to those on the geologic map. Tumamoc Hill hikers, take a closer look at what you are walking through
The younger volcanic series forms the bulk of the hills:
Tb2 Tumamoc basaltic andesite (~23-24 Million years [Ma] old) Dark basaltic andesite lava flows with total thickness of >60 m that form the top of Tumamoc Hill and Sentinel Peak . Includes scoriaceous, vesicular, and brecciated basalt.
Tb1 Basaltic andesite (~26-28 Ma) Basaltic andesite, with olivine phenocrysts, locally vesicular to scoriaceous.
Rock quarried from the Tb1 unit went to build foundations and walls of many University of Arizona buildings.
Tc Conglomerate ( ~26-28 Ma) Pebble to cobble conglomerate, locally with boulders up to 70 cm diameter. Clasts consist primarily of mafic volcanic rocks and could all be locally derived.
Ttt Turkey Track andesite ( ~27-28 Ma) Unit contains abundant, large (2-3cm) plagioclase phenocrysts, sparse pyroxene, and rare olivine phenocrysts. Presumed to consist of lava flows; total thickness >45 m.
Note: the term “turkey track” is used to describe a texture of large white plagioclase crystals in an uncrystallized matrix similar to the photo. The age of these rocks was determined by K/Ar analysis, that is, measuring the ratio of potassium to argon. Potassium is radioactive and decays to argon.
The older volcanic series is exposed only the south flank along 22nd Street:
TKm Mafic volcanic rocks (58 Ma)—Unit includes two map units : (1) Tumamoc andesite, massive, with euhedral plagioclase phenocrysts, estimated thickness 12 m. (2) Short’s Ranch andesite, estimated thickness >39 m. Phenocrysts consist of plagioclase and biotite and possibly rare quartz.
TKt Sentinel Tuff (early Tertiary or late Cretaceous)—Tuff is 6 m thick, contains abundant plagioclase phenocrysts, minor biotite, sparse lithic fragments, and relict glass shards. Unit overlies Greasewood andesite of map unit TKm, and is overlain by Tumamoc andesite of map unit TKm, and Turkey Track ndesite.
TKg Greasewood andesite (early Tertiary or late Cretaceous)—Andesite, 10 m thick, with plagioclase and pyroxene phenocrysts, overlies sandstone of Anklam Formation.
TKtm Mission Road Tuff (early Tertiary or late Cretaceous)—Tuff containing biotite and plagioclase, sparse volcanic(?) lithic fragments, and relict glass shards. Estimated thickness 5m.
TKs Fine-grained silty sandstone and tuffaceous sandstone (early Tertiary or Cretaceous) Unit correlated with the Anklam Formation. Includes a small exposure of Mission Road andesite at the south foot of Sentinel Peak of Mission Road andesite.
If you’ve read this far, Scrabble players have many new words.
An underground ridge of these older volcanic rocks extends eastward toward the Santa Cruz River and once forced water to the surface to produce a well-watered agriculture plain east of the hills that was used for about 4,000 years up until the 1930s.
Tumamoc Hill and Sentinel Peak have a rich archaeological history. You can read a 75-page report from the University of Arizona here. (Scroll down to page 18.)