University assists with Delaware GIS Day field trip


Volunteers from the University of Delaware and the UD-based Delaware Geological Survey assisted with the Delaware GIS (Geographic Information Systems) Day field trip for fifth graders held Nov. 18.

Earthquake Felt Report

Please answer every question to the best of your ability. Either fill in the blanks where called for, or check the response that best describes the event. If a question does not apply or if you don't know how to respond to a particular question, simply skip it and go on to the next. Feel free to add additional information in the Additional Comments box at the bottom of the form.

RI40 Sodium Concentrations in Water from the Piney Point Formation, Dover Area, Delaware

In the greater Dover area sodium concentrations in ground water from the glauconitic Piney Point Formation commonly exceed 100 parts per million. Investigation of chemical characteristics of the water, and statistical analyses of the results, show that these high concentrations are due to a natural ion-exchange process. Calcium in water replaces sodium in the mineral glauconite and causes the sodium enrichment in ground water.

RI34 Long-Term Chemical-Quality Changes in Selected Delaware Streams

Data from three streamflow water-quality stations were statistically analyzed to determine the relationships of the major inorganic chemical constituents to specific conductance and to stream discharge. The results show that ion concentrations varied directly with the flow and with specific conductance. A set of regression equations defining these relationships were derived for each of the three stations: Brandywine Creek at Wilmington, St. Jones River at Dover, and Nanticoke River near Bridgeville.

B17 Geological Studies of Cretaceous and Tertiary Section, Test Well Je32-04, Central Delaware

A cored well 1,422 feet (433 meters) deep drilled two miles southeast of Dover is the basis for this integrated study of the lithology and paleontology of the Cretaceous-Tertiary section in central Delaware. The section is subdivided into lithostratigraphic, biostratigraphic, chronostratigraphic, and heavy mineral units. Data and results are presented on a common base in three plates.