In late 2013 the Arizona Geological Survey (AZGS) partnered with the Arizona Department of Water Resources (ADWR) to investigate sedimentary relationships at numerous sites along the San Pedro River in southeastern Arizona. Previously, AZGS conducted surficial geologic mapping along the San Pedro River, Aravaipa Creek, and the Babocomari River in 2007. These maps and a report are available in AZGS DM-RM-1.2. The goal of this project was to conduct site investigations along the San Pedro River to determine whether sedimentary relationships between San Pedro River and tributary alluvium are accurately represented by their mapped location on the surface. This document includes a brief summary and description of sites along the San Pedro River ...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
Most of southern and western Arizona is covered with unconsolidated basin sediments that are not map...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
The San Pedro River flows through the rugged landscape of San Pedro Valley from the U.S. – Mexico bo...
The San Pedro River is divided into upper and lower reaches based on environmental and geomorphic co...
This map depicts the geology of the Land 7 ½' Quadrangle, which is located in the upper San Pedro Va...
In 2005, the U.S. Geological Survey (USGS) began an investigation of the hydrogeology of the middle ...
The San Pedro River in southeast Arizona is by no means a major watercourse in the Southwest, but ye...
In 2010, the Arizona Geological Survey (AZGS) released a series of 1:24,000-scale geologic strip map...
This map depicts the geology of the Lewis Springs 7 ½' Quadrangle, which is located in the upper Sa...
This map depicts the geology of the Hereford and the northern part of the Stark 7 ½' quadrangles, wh...
The Saint David 7½' Quadrangle is located approximately 55 miles (88 km) west of downtown Tucson. Th...
Like most river valleys, that of the Santa Cruz River contains a complex history of erosion, deposit...
Rocks of the mountains paralleling the San Pedro River Valley in the Tres Alamos Dam Site area range...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
Most of southern and western Arizona is covered with unconsolidated basin sediments that are not map...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
The San Pedro River flows through the rugged landscape of San Pedro Valley from the U.S. – Mexico bo...
The San Pedro River is divided into upper and lower reaches based on environmental and geomorphic co...
This map depicts the geology of the Land 7 ½' Quadrangle, which is located in the upper San Pedro Va...
In 2005, the U.S. Geological Survey (USGS) began an investigation of the hydrogeology of the middle ...
The San Pedro River in southeast Arizona is by no means a major watercourse in the Southwest, but ye...
In 2010, the Arizona Geological Survey (AZGS) released a series of 1:24,000-scale geologic strip map...
This map depicts the geology of the Lewis Springs 7 ½' Quadrangle, which is located in the upper Sa...
This map depicts the geology of the Hereford and the northern part of the Stark 7 ½' quadrangles, wh...
The Saint David 7½' Quadrangle is located approximately 55 miles (88 km) west of downtown Tucson. Th...
Like most river valleys, that of the Santa Cruz River contains a complex history of erosion, deposit...
Rocks of the mountains paralleling the San Pedro River Valley in the Tres Alamos Dam Site area range...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
The purpose of these investigations is to document and map the extent of Holocene channel and floodp...
Most of southern and western Arizona is covered with unconsolidated basin sediments that are not map...