The soils in our part of the Sierra foothills are underlain by andesitic mudflow (lahar) deposits that poured off the higher mountains around 9-10 million years ago. The hills in the distance (and around the lake below) are metamorphic rocks of the Foothills Terrane, dating from around 200 million years ago.
We had a reasonably decent rain season, with close to 100% of average precipitation. We really needed about 120% to overcome the three years of drought, since many of the soils around the state are exceedingly dry and need to be replenished, but on this day there was plenty of water in evidence in the normally dry creekbeds and stockponds. One of our favorite stops is a little lake on Willms Road in the vicinity of Knights Ferry on the Stanislaus River. Vast numbers of birds are usually in evidence.
Since getting my first digital camera 9 years ago, I have concentrated on geological subjects, but I have been adding more plants and animals to my repertoire. There is an old adage about geological field work, that you will spend an entire field season collecting every unusual and unique rock in sight, and later come to the realization that you never collected a single specimen of the most common rock in your study area. My bird pictures are kind of like that. I have few pictures of the most common birds in our area.
The fuzzy picture above is my first photograph of a Western Meadowlark. They were very much in evidence, as their calls could be heard every place we stopped, but they were shy about being approached, so this one was taken with a 30x zoom (lest you think I have sophisticated equipment, that is optical and digital zoom together).