Groundwater Subareas: Carneros, Jameson/American Canyon, and Napa River Marshes

The geology of the Carneros Subarea is marked by the extensive presence of the generally low permeability Huichica Formation with minor occurrences of volcanic rocks and alluvial deposits. The alluvial deposits tend to be thin and found in the vicinity of Carneros and Huichica Creeks. Based on limited available data the Jameson/American Canyon and Napa River Marshes Subareas have fine-grained alluvial deposits present at the surface at lower elevations. Higher elevation areas of the Jameson/American Canyon Subarea also include outcropped sedimentary rocks.

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View animation of conceptualized
sub-surface geology

 

Legend of sub-surface geologic layers

 

In 2017, twelve groundwater level monitoring sites were located in the Carneros Subarea. The longest period of record among them extended back to October 2011. All monitored wells are located in the southern half of the subarea at land surface elevations between 100 feet and 15 feet. Patterns of groundwater level fluctuations in these wells have shown annual variations of approximately 5 feet from spring to fall, though several wells saw spring 2017 water levels rise more than 10 feet relative to levels in spring 2016 and spring 2015. Groundwater elevations range from about 30 feet to -5 feet. Depths to groundwater below ground surface have varied more widely from 5 feet to 100 feet. Groundwater levels have been stable to increasing in 10 of the currently monitored wells.

In the Jameson/American Canyon Subarea the only current groundwater level data are from one well recently volunteered for monitoring. Spring and fall measurements recorded in that well between 2014 and 2017 found shallow depths to groundwater ranging from 3 feet in the spring to 14 feet in the fall.

Subareas south of the Napa Valley Floor may be susceptible to seawater intrusion originating from San Pablo Bay. In the Carneros Subarea, where long-term records are available, two wells have shown increasing Total Dissolved Solids (TDS) trends, though all four wells with long-term records were initially at or above the secondary Maximum Contaminant Levels (MCL). Nitrate concentrations have been stable to decreasing in all five wells with long-term records in the Carneros Subarea and Napa-Sonoma Lowlands Subbasin.

Construction information for wells with groundwater quality data in the three subareas south of the Napa Valley Floor are limited, making it difficult to determine the source and distribution of the elevated TDS and salinity values. For example, it is not clear whether high salinity groundwater in the Carneros Subarea is a result of saltwater intrusion or interaction of groundwater with the geologic units present in and around the subarea.

Groundwater Map - Carneros, Jameson/American Canyon, and Napa River Marshes Subarea

Using the map below, click on specific areas to find more information and links to subarea groundwater monitoring results, levels and trends. Enter your address, city or zip in the legend area to zoom to an area of specific interest.

To navigate to other Groundwater subarea pages, use the links below.

Angwin and Pope Valley | Carneros, Jameson/American Canyon, and Napa River Marshes | Eastern Mountains and Western Mountains | Napa Valley Floor – Milliken-Sarco-Tulucay | Napa Valley Floor – Yountville and Napa | Napa Valley Floor – Calistoga and St. Helena