Maryland

OFR17 A Guide to Information on Benchmarks in Delaware

To conduct an elevation survey, a surveyor needs a starting point for which the exact elevation above mean sea level is known. These starting points are called benchmarks. State and federal agencies install benchmarks throughout every State, creating a network of elevation points which covers the entire continental United States. These benchmarks are considered to be permanent, and usually consist of a brass, bronze, or aluminum disc about 4 inches in diameter mounted in a cement post or in a drill hole in a permanent foundation.

OFR42 Catalog of Earthquakes in Delaware

The occurrences of earthquakes in northern Delaware and adjacent areas of Pennsylvania, Maryland, and New Jersey are well documented by both historical and instrumental records. Over 550 earthquakes have been documented within 150 miles of Delaware since 1677. One of the earliest known events occurred in 1737 and was felt in Philadelphia and surrounding areas. The largest known event in Delaware occurred in the Wilmington area in 1871 with an intensity of VII (Modified Mercalli Scale).

OFR40 Summary Report: The Coastal Storms of January 27-29 and February 4-6, 1998, Delaware and Maryland

In the period between January 27 and February 6, 1998, the Mid-Atlantic region experienced two significant northeasters that affected the coast of Delaware and Maryland. These storms produced heavy rains and high winds, waves, and tides that created dune washovers, flooding, wind damage, and beach erosion and migration. Coastal communities were impacted by flooding that closed roads, by beach erosion that affected structures, streets and boardwalks, and by high winds that damaged structures and trees.

B3 Marine Upper Cretaceous Formations of the Chesapeake and Delaware Canal

In the Coastal Plain of Delaware, the non-marine Cretaceous sands and clays are separated from the Tertiary formations by a series of marine formations of Upper Cretaceous age. The sedimentary and hydrologic characteristics of these formations deserve detailed study because some of them are water-bearing beds. whereas others act as confining beds. A clear understanding of their relative age. and the presence or absence of unconformities is needed for proper correlation with formations found in wells throughout the State. as well as in Maryland and New Jersey.