Note 2 — THE GEOLOGY OF D.A.R. STATE PARK

This is one of the three major rock groups or families. The first consists of igneous rocks, including granite, syenite, and basalt, which were formed by solidification of molten rock-material. The igneous rocks are ancestors of the other two rock families; they form over 90 percent of the outer 10 miles of the Earth’s crust. The second family, consisting of sedimentary or layered rocks including shale, sandstone and limestone, is composed of pieces and grains and other materials from all the families of rocks. In addition, sedimentary rocks are formed also from lime secreted by marine plants and animals or chemically precipitated from sea water, or by the accumulations of shells. The third family, metamorphic rocks, including gneiss, schist, slate and marble, were igneous or sedimentary rocks that have been subjected to heat and pressure in the presence of mineral-forming solutions. Metamorphic rocks generally look different from the rocks from which they formed, because the original minerals of the rock have been changed and reoriented.