The sandstones of the formation were deposited in a fluvialenvironment. The formation has an estimated thickness of 460 metres (1,510 ft) and overlies the Anita Formation, while it is overlain by the La Irene Formation.[4] These formations are considered Campanian and Maastrichtian in age, respectively,[4][3] making the Cerro Fortaleza Formation aged between them.
Several isolated teeth, including two anteriormost, probably premaxillary teeth, left manual phalanx I-1, right, nearly complete fibula, and right ungual.
^Sickmann, Zachary T.; Schwartz, Theresa M.; Graham, Stephan A. (2018). "Refining stratigraphy and tectonic history using detrital zircon maximum depositional age: An example from the Cerro Fortaleza Formation, Austral Basin, southern Patagonia". Basin Research. 30 (4): 708–729. Bibcode:2018BasR...30..708S. doi:10.1111/bre.12272.
^Novas, Fernando E.; Ezcurra, Martín D.; Lecuona, Agustina (June 2008). "Orkoraptor burkei nov. gen. et sp., a large theropod from the Maastrichtian Pari Aike Formation, Southern Patagonia, Argentina". Cretaceous Research. 29 (3): 468–480. Bibcode:2008CrRes..29..468N. doi:10.1016/j.cretres.2008.01.001.
^Agnolín, Federico L.; Álvarez Herrera, Gerardo; Rolando, Mauro Aranciaga; Motta, Matías; Rozadilla, Sebastián; Verdiquio, Lucía; D'Angelo, Julia S.; Moyano-Paz, Damián; Varela, Augusto N.; Sterli, Juliana; Bogan, Sergio; Miner, Santiago; Moreno Rodríguez, Ana; Muñoz, Gonzalo; Isasi, Marcelo P.; Novas, Fernando E. (February 2024). "Fossil vertebrates from the Cerro Fortaleza Formation (Upper Cretaceous), Santa Cruz Province, Argentina". Cretaceous Research. 154: 105735. Bibcode:2024CrRes.15405735A. doi:10.1016/j.cretres.2023.105735.