Final answer:
The red beds of the Catskill wedge were deposited in a continental paleoenvironment during the Acadian Orogeny.
Step-by-step explanation:
The red beds of the Catskill wedge were deposited in a continental paleoenvironment. These sedimentary rocks consist of sandstone, siltstone, and shale, and are predominantly red in color due to the presence of ferric oxides. The Catskill clastic wedge, which extends from New York through Virginia and West Virginia, is part of the larger Appalachian Basin and was sourced from the Appalachian Mountains during the Acadian Orogeny. It contains evidence for three phases of the Acadian Orogeny.