Baltimore Gneiss McKeldin Area Patapsco Valley State Park 2016

The Baltimore Gneiss is a

Precambrian The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the ...

geological formation in the Piedmont region of Maryland, Pennsylvania, and Delaware.

Characteristics

At least 95 percent of the Baltimore Gneiss can be described as quartzo-feldspathic gneiss of granodioritic to granitic composition, with the remaining 5 percent consisting of

amphibolite Amphibolite () is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase feldspar, but with little or no quartz. It is typically dark-colored and dense, with a weakly foliated or schistose (flaky ...

. The age of the Baltimore Gneiss has been constrained to 1.0-1.1 Ga.

Members

The Gneiss is homogeneous overall, but is recognized as having four subdivisions. These are the ''layered gneiss member'', the ''augen gneiss member'', the ''streaked-augen gneiss member'', and the ''hornblende gneiss member''. Additionally, the Baltimore Gneiss outcrops into three discrete masses of uniform, well-foliated to massive granitic gneiss referred to as the ''Slaughterhouse Gneiss''. The layered gneiss member consists of dark and light layers of gneiss bearing

biotite Biotite is a common group of phyllosilicate minerals within the mica group, with the approximate chemical formula . It is primarily a solid-solution series between the iron-endmember annite, and the magnesium-endmember phlogopite; more alumino ...

, microcline, quartz, and plagioclase, varying from biotite schist to quartzo-feldspathic granofels interlayered on a centimeter to decimeter scale. The augen gneiss member consists of two belts of fine to medium grained gneiss bearing biotite, microcline, quartz, and plagioclase, with abundant large ovoids (

augen Augen (from German "eyes") are large, lenticular eye-shaped mineral grains or mineral aggregates visible in some foliated metamorphic rocks. In cross section they have the shape of an eye. Feldspar, quartz, and garnet are common minerals whic ...

) consisting of microcline and/or quartz. The streaked-augen gneiss member consists of uniform, medium-grained biotite-microcline-quartz-plagioclase gneiss, with augen that have a "stretched" or "streaked" appearance. The hornblende gneiss member is similar to the layered gneiss member, but with hornblende-bearing dark gneiss accounting for about half of the outcrop area. The Slaughterhouse Gneiss weathers to a pinkish to orange color, and consists of relatively uniform, medium-grained microcline-quartz-plagioclase gneiss with muscovite, biotite, or both.

Structure

Gneiss inclusion in granite Fig26 Keyes 1895

The Phoenix, Texas, Chattalolanee, and Towson gneiss anticlines in the Baltimore, Maryland area are all part of a refolded nappe system beneath the Towson anticline. The cores of these nappes consist of the Baltimore Gneiss. The Baltimore Gneiss has been affected by three deformation periods: the Grenvillian, known from radiometric age data, for which nearly all resulting structural features where destroyed or obstructed by later tectonic deformation; the Taconic-

Acadian The Acadians (french: Acadiens , ) are an ethnic group descended from the French who settled in the New France colony of Acadia during the 17th and 18th centuries. Most Acadians live in the region of Acadia, as it is the region where the de ...

, which involved three phases of folding,

facies metamorphism, local migmatization, and the development of the gneiss's pervasive structural elements; and the Alleghanian- Palisades, which resulted in predominantly brittle faulting and open folding. The cause of the Grenvillian deformation is uncertain. The Taconic-Acadian deformation was caused by the collision of an ocean floor/island arc terrane with a continental margin or fringing microcontinent in the early Paleozoic. The Alleghanian-Pallisades deformation was caused by continental rifting in the early Mesozoic, and possibly late-Paleozoic trans-current plate motions.

History

The name Baltimore Gneiss was first used by George Huntington Williams in 1892 to describe the variety of widely distributed gneisses in the Baltimore area.

Usage

The Baltimore Gneiss has been used in the past as

building stone Building material is material used for construction. Many naturally occurring substances, such as clay, rock (geology), rocks, sand, wood, and even twigs and leaves, have been used to construct buildings. Apart from naturally occurring materia ...

in the Baltimore area. It is thought that some of the first buildings built in Baltimore in the 1700s were constructed of gneiss quarried from Jones Falls. In addition to use in buildings, gneiss from Jones Falls and Gwynn Falls quarries was used for foundations, roads, and curbstones in Baltimore. Some quarrymen referred to the gneiss as "blue stone" due to the blue-gray color of its fresh surface. The last building stone quarry in Baltimore closed in 1958.

Type localities

The type locality of the Baltimore Gneiss as described by William Patrick Crowley of the Maryland Geological Survey in 1976 is defined as outcrops along

Towson Run Towson Run is a tributary of Jones Falls, a stream in Baltimore County, Maryland, in the United States. The stream runs north through Sheppard Pratt and Towson University, near the communities of Rodgers Forge and Armagh Village. Geology The ...

from Bellona Avenue to Towsontown Boulevard. Formerly, the type locality was considered as referring to layered gneisses which outcrop along Jones Falls and Gwynns Falls in Baltimore City, however, chemical and textural analysis followed by zircon age measurements determined that these gneisses represent a distinct younger geologic unit. The type locality of the layered gneiss member includes stream cuts along

Herring Run The Herring Run is an U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed April 1, 2011 tributary of the Back River located in Baltimore, Maryland. Geography The watershed has its head ...

for 255 meters on either side of Arlington Avenue bridge near Morgan State University. The type locality of the augen gneiss member includes outcrops along Long Green Creek 385 meters southeast of Glenarm Road bridge. The type locality of the streaked-augen gneiss member includes outcrops along Merryman Branch 125 meters upstream from the Dulaney Valley Road bridge. The type locality of the hornblende gneiss member includes outcrops along an unnamed stream between Malvern Avenue and Boyce Avenue. The type locality of the Slaughterhouse Gneiss outcrops along the

Slaughterhouse Branch A slaughterhouse, also called abattoir (), is a facility where animals are slaughtered to provide food. Slaughterhouses supply meat, which then becomes the responsibility of a packaging facility. Slaughterhouses that produce meat that is no ...

southeast of the

Baltimore Beltway Baltimore ( , locally: or ) is the most populous city in the U.S. state of Maryland, fourth most populous city in the Mid-Atlantic, and the 30th most populous city in the United States with a population of 585,708 in 2020. Baltimore was d ...

(I-695).

Notable outcrops

Some notable exposures of the Baltimore Gneiss in addition to the type localities mentioned above include outcrops along the Rapids Trail in the McKeldin Area of Patapsco Valley State Park and along roads around the Loch Raven Reservoir.

References

{{reflist Geology of Maryland Geology of Pennsylvania Geology of Delaware Precambrian United States Gneiss