PA Geology & Rocks

Rock Types of Pennsylvania

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Rocks And Minerals of Pennsylvania


Common Fossils of Pennsylvania


Rocks are divided into three basic groups: sedimentary, igneous, and metamorphic. Sedimentary rocks, the most common rocks at the surface in Pennsylvania, form by either the deposition of individual grains that have eroded from older rocks and have been transported by water or wind (clastic sedimentary rocks); or by the precipitation of dissolved minerals from water or organic deposition (nonclastic sedimentary rocks). The naming of sedimentary rocks is based mostly on grain size (clastic) and/or chemical composition (nonclastic). Common clastic sedimentary rocks in Pennsylvania are conglomerate, sandstone, siltstone, claystone, and shale. Common nonclastic sedimentary rocks are limestone and dolomite.

Igneous rocks are formed by the cooling of molten material, either lava (above ground) or magma (underground). They are classified by what minerals they contain and the grain size of the minerals (coarse enough to be seen with the naked eye, or too fine to be seen). Rocks containing the same minerals, but having different grain sizes have different names. Likewise, igneous rocks of the same grain size, but of different mineral composition will have different names. Pennsylvania has had a variety of igneous rocks; however, most of these have undergone metamorphism. On the maps, they are classified simply as dark or light-colored. The color is a reflection of the minerals present in the rock.

Metamorphic rocks are those formed by altering igneous, sedimentary, or other metamorphic rocks by heat and/or pressure. The heat and pressure cause changes in the minerals present, as well as rearranging the minerals in the rocks. Metamorphic rock names are based on grain size, organization of minerals into layers (foliation), and composition. Pennsylvania has gneiss, schist, phyllite, slate, marble, and quartzite.

Crystalline rocks refers to either igneous or metamorphic rocks.

Much more information about the rocks in general, rocks of Pennsylvania, and the minerals of which they are composed, can be found in our publication ES1: Rocks and Minerals of Pennsylvania. The 1982 publication, EG1, Engineering characteristics of the rocks of Pennsylvania by A. R. Geyer and J. P. Wilshusen, (300 p.) also provides information on the rocks of Pennsylvania by geologic unit.

Map 63 delineated 19 different rock types or groups of rock types for Pennsylvania. The county maps show these rock types. The following descriptions are modified from Map 63. The numbers in the list match the rock type numbers on the maps. A glossary follows.

  • Dark-colored igneous and metamorphic (crystalline) rocks. Includes dark-colored gneiss and diabase (and kimberlite, if it is shown on the map). Also includes all dikes, thereby lumping pegmatite, a light-colored rock that is limited in extent, with the much more common diabase dikes.
  • Light-colored metamorphic (crystalline) rocks. Includes light-colored gneiss and pegmatite.
  • Schist, including minor amounts of gneiss, quartzite, and phyllite.
  • Marble.
  • Quartzite.
  • Unconsolidated sediments. Includes coastal-plain deposits, Delaware River gravel, and sand at Presque Isle. Does not include glacial deposits.
  • Red sedimentary rocks. Includes sandstone, siltstone, shale, and some conglomerate. Some non-red rocks may be included.
  • Limestone.
  • Dolomite.
  • Mixed limestone and dolomite.
  • Limestone or dolomite mixed with sandstone, shale, or chert.
  • Slate.
  • Shale and siltstone.
  • Sandstone and minor amounts of shale or siltstone.
  • Shale or siltstone, and minor amounts of sandstone.
  • Sandstone and/or conglomerate.
  • Mixed sandstone and conglomerate, with coal, shale, and siltstone. Includes anthracite seams in eastern Pennsylvania.
  • Mixture of sandstone, siltstone, shale, claystone, limestone, and coal.
  • Mixture of siltstone, shale, sandstone, limestone, claystone, and coal. Includes the most economically important bituminous coal seams.

The State Fossil

Most Pennsylvanians know that Mountain Laurel is the state flower and Ruffed Grouse is the state game bird. Some of the keystone state’s official symbols, however, are not as widely recognized by Commonwealth citizens. These latter tokens include Whitetail Deer (the state animal), the Great Dane (state dog), Brook Trout (the state fish), and Hemlock (the state tree). A few of Pennsylvania’s official symbols actually border on the esoteric. The firefly, for example is the state insect, milk is the state beverage, and the restored replica of Admiral Perry’s famous flagship, the brig Niagara, is the official flagship of Pennsylvania. Pennsylvania also has an authorized “beautification and conservation plant” – crownvetch, and this plant is, ironically enough, the bane of both professional and amateur geology enthusiasts because its dense growth can hide the rocks that contain what might be the state’s least known symbol, the state fossil, Phacops rana.

Phacops rana is a fossil organism known as a trilobite (pronounced “tri-lobe-ite”). Trilobites are an extinct category of jointed-legged animals related to crabs, lobsters, shrimp, spiders, insects, and so on. This group of creatures, called arthropods, are among the most complex of all the animals without backbones and trilobites are no exception. They had well-developed nervous systems and large antennae. Trilobites had many appendages for swimming, walking, or feeding. Although these appendages are relatively rare in most groups of trilobite fossils. Phacops is one of four genera for which they are fairly well known and studied. Trilobites also had a hard outer skeleton composed of chitin, a complex organic protein, and the mineral apatite (calcium phosphate).


Many trilobites had large eyes. They are, in fact, the first organisms on earth known to have eyes. The trilobites had compound eyes, composed of many individual lenses, like those of insects. Trilobites possess the most ancient visual system known to scientists and thus they provided some of the best direct evidence of eye evolution.

Trilobites are a common fossil in many of the early to middle Paleozoic rocks of central Pennsylvania, i.e., rocks that are between 570 and 365 million years old. Complete fossil specimens are rare because the animals were composed of rigid outer skeletal segments joined by flexible organic connections that decayed on the death of the animal. Currents, scavengers, and molting all served to separate skeletal parts, which comprise the most common trilobite fossils in Pennsylvania. This common abundance of trilobite parts in the fossil record, in fact, was enhanced by the fact that the animals grew by casting off their outer skeleton in a series of molt stages. One animal probably produced ten to twelve potentially preservable skeletons in its lifetime.

An interest in trilobites is not restricted to scientists and geological dilettantes. They are prized by jewelry and curio collectors. This interest is a long-standing one. Trilobites were found on necklaces belonging to the prehistoric inhabitants of 15,000 year old rock shelters of Europe. The Ute Indians of the western United States fashioned trilobites into amulets. The Ute name for these fossils was, “timpe khanitza pachavee” which means “little water but like stone house in.”

Phacops rana is found in Pennsylvania’s Devonian-age rocks (rocks between 405 and 365 million years old). A publicly available location for finding fossil specimens of this fascinating creature is described in Pennsylvania Trail of Geology, Park Guide 16. This is a site where you can collect Phacops rana and other fossils.



Calcareous – Contains calcium carbonate (calcite) or calcium-magnesium carbonate (dolomite). Will fizz when dilute hydrochloric acid (HCl) is placed on a sample. Calcite will fizz vigorously. Dolomite will fizz gently. Limestone, dolomite, and marble are common calcareous rocks. Other rocks may also be calcareous.

Claystone – A sedimentary rock in which more than 50 percent of the particles are less than 0.00015 inches in diameter. Grains are too small to be visible as individuals, giving the rock a smooth appearance. It looks like clay that has been hardened into rock. It does not have the fine layering of shale.

Coal – A black, relatively lightweight rock composed of accumulations of plant matter converted by pressure and heat.

Conglomerate – A sedimentary rock with rounded pebbles that are greater than 0.08 inches in diameter. It has an appearance somewhat like concrete, with pebbles cemented together by finer-grained material.

Dolomite – A sedimentary rock composed of magnesium (Mg), calcium (Ca) and carbonate (CO3). Also called dolostone. It reacts to dilute hydrochloric acid, but not as vigorously as will limestone or marble. Surfaces that have been powdered by scratching (or by scraping during drilling) may react more readily. Dolomite is generally gray or tan in color. Grain size ranges from small, visible crystals to grains that are too small to see individually.

Dike – A tabular body of igneous rock that cuts across the bedding or foliation of the surrounding rock. Most dikes in Pennsylvania are composed of diabase, a dark-colored igneous rock.

Foliated – A property of metamorphic rocks where a planar feature exists, either due to the orientation of platy grains, or the separation of different minerals into bands. Foliated rocks include slate, phyllite, schist, and gneiss.

Gneiss – A metamorphic rock characterized by alternating light and dark-colored bands. Color is determined by the minerals present in each layer. One color usually predominates, such that a gneiss can be categorized as either a light crystalline rock or a dark crystalline rock. The mineral grains in a gneiss are large enough to be easily visible. Most of the grains are relatively equidimensional, meaning that they are more like little chunks than like plates or sheets.

Limestone – A sedimentary rock composed of calcium (Ca) and carbonate (CO3). Its most obvious defining characteristic is that it reacts vigorously to dilute hydrochloric acid. Limestone is generally gray or tan in color, although they can be dark gray or black. Grain size ranges from small, visible crystals to grains that are too small to see individually. Limestone may contain fragments of fossil shells.

Marble – Metamorphosed limestone and dolomite. Marble is composed of large crystals of calcite or dolomite that sparkle when light reflects off of their flat surfaces. In Pennsylvania, marble is white or very light gray, and generally contains flakes of golden-brown or white mica. It reacts to dilute hydrochloric acid. Marble can be scratched by a knife.

Mica – A series of minerals that form thin sheets. Mica is found as layers in schist, phyllite, and some gneisses, and as flakes in marble and some sandstones. Several varieties that are common in Pennsylvania are white (usually appears silver-gray), black, or golden-brown. Mica has a glassy or metallic appearance.

Phyllite – A fine-to-medium grained, layered metamorphic rock. Mica grains are just large enough to be visible. Rock surfaces are smooth and have a satiny sheen. Layers tend to be fairly planar, and the rock splits easily along them. The most common colors are silvery gray or greenish gray.

Quartzite – A very hard rock composed almost entirely of quartz. In the metamorphic variety, quartz grains are interlocked like puzzle pieces. Grains are usually relatively large. In the sedimentary variety, sand-sized quartz grains are cemented together by fine-grained material of the same composition. Quartzite is generally white or beige. Quartzite is harder than steel and cannot be scratched by a knife.

Sandstone – A sedimentary rock in which more than 50 percent of its particles are sand-sized (0.002–0.08 inches in diameter). It looks like sand held together by cement. Sandstones can be found in a variety of shades of white, red, green, and gray.

Schist – A metamorphic rock dominated by coarse-grained mica arranged in layers. The layers tend to be wavy or bumpy, and separated by granular layers usually dominated by quartz. Large crystals of other minerals are common. One of these other minerals is garnet – dark red, rounded, pinhead- to pea-sized or larger. Rock surfaces have a shiny, sparkly, or sequined appearance. Schist usually appears silver-gray due to the abundant mica.

Shale – A finely layered sedimentary rock similar in grain size to claystone, but that breaks out into thin sheets or plates parallel to the layers. Shale is found in many shades of gray, black, red, and green.

Siltstone – A sedimentary rock in which more than 50 percent of its particles are silt-size (0.00015–0.002 inches in diameter). Visually indistinguishable from shale and claystone, it feels slightly gritty between the teeth.

Slate – A very fine-grained layered metamorphic rock that splits into thin sheets. Grains are too small to be individually visible, giving the rock a smooth appearance. Surfaces are dull and tend to be absolutely flat. The most common colors are black and shades of gray. Slate is commonly used for roofing and pavers. In Pennsylvania, slate is found ONLY in the southeastern quarter of the state. The most important locations are in Lehigh, Northampton, York, and Lancaster Counties. Lesser occurrences are in Adams, Berks, Carbon, Dauphin, and Lebanon Counties.

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