Question: Which geologic formation is found in the northern edge of Patagonia?

Context articles: Pari Aike Formation
Caleta Herradura Formation
Santa Marta Formation
Río Negro Province
Britton Formation
Portezuelo Formation
Becraft Formation
Bajo de la Carpa Formation
Pan de Azúcar Formation
Chattanooga Shale

The Pari Aike Formation is a Late Cretaceous geologic formation of Cenomanian (formerly believed to be Maastrichtian) age in southern Patagonia, Argentina.
 The giant titanosaur "Puertasaurus", the megaraptoran "Orkoraptor", and the ornithopod "Talenkauen" have been recovered from the formation alongside turtles and crocodiles.
Caleta Herradura Formation (Spanish: "Formación Caleta Herradura" ) is a geologic formation of Miocene age located in Mejillones Peninsula in northern Chile.
 The erosion at the Coastal Cliff of northern Chile have created particularly good exposures of Caleta Herradura Formation.
 The formation deposited in a half graben within Mejillones Peninsula.
 The formation rests nonconformably on the Jorgino Formation.
The Santa Marta Formation is a geologic formation in Antarctica.
 It, along with the Hanson Formation and the Snow Hill Island Formation, are the only formations yet known on the continent where dinosaur fossils have been found.
 The formation outcrops on James Ross Island off the coast of the northern tip of the Antarctic Peninsula.
 In its entirety, the Santa Marta Formation is on average one kilometer thick.
Río Negro (] , "Black River") is a province of Argentina, located at the northern edge of Patagonia.
 Neighboring provinces are from the south clockwise Chubut, Neuquén, Mendoza, La Pampa and Buenos Aires.
 To the east lies the Atlantic Ocean.
The Britton Formation is a geologic formation deposited during the Middle Cenomanian to the Early Turonian ages of the Late Cretaceous in modern-day East Texas.
 It forms the lower half of the Eagle Ford Group in the northern portion of East Texas.
 The formation was named by W. L. Moreman in 1932 for outcrops on Mountain Creek near the small town of Britton, south of Dallas.
 In the Dallas area it has been subdivided into the Six Flags Limestone, Turner Park Member, and Camp Wisdom Member.
 The Six Flags Limestone is a 3 ft (1 m) thick fossiliferous calcarenite made up of pieces (prisms) of "Inoceramus" clams.
 The Turner Park and Camp Wisdom Members were subdivided based on the numerous volcanic ash beds (bentonites) found in the Turner Park, and the common occurrence of concretions in the Camp Wisdom.
 They are approximately 120 ft (37 m) (Turner Park) and 250 ft (76 m) (Camp Wisdom) thick in the Dallas area.
 Thin sandstones known as the Templeton Member are found in Grayson County, north of Dallas, that are age equivalent to the lower part of the Turner Park Member.
 The Templeton Member was originally described as a part of the Woodbine, but it was recently placed in the Britton Formation of the Eagle Ford Group based on its age as derived by ammonites.
The Portezuelo Formation is a geologic formation outcropping in the Mendoza, Río Negro and Neuquén provinces of Argentina.
 It is the fourth-oldest formation in the Neuquén Group and the older of the two formations in the Río Neuquén Subgroup.
 Formerly, that subgroup was treated as a formation, and the Portezuelo Formation was known as the Portezuelo Member.
The Becraft Formation is a geologic formation of marine sedimentary rock found in New York State.
 The Becraft is a part of the lower Devonian Helderberg Group and conformably overlies the New Scotland Formation and is overlain by the Alsen Formation throughout the lower Hudson Valley of New York State.
 The formation is Gedinnian in age.
 Outcrops of the formation are found from the New York-New Jersey border to the Helderbergs of Albany County, New York and as far west as Schoharie County, New York.
 The thickness of the formation varies from around 3 meters in Canajoharie to 8 meters thick in Albany and swells to 27 meters near Kingston.
 The Becraft Formation is named for Becraft Mountain in western Columbia County, New York where it prominently crops out.
The Bajo de la Carpa Formation is a geologic formation that outcrops in Patagonia, in the provinces of Río Negro and Neuquén, Argentina.
 It is the first of two formations belonging to the Río Colorado Subgroup within the Neuquén Group.
 Formerly that subgroup was treated as a formation, and the Bajo de la Carpa Formation was known as the Bajo de la Carpa Member.
Pan de Azúcar Formation (Spanish: "Formación Pan de Azúcar" , "Sugar-loaf formation") is a geologic formation of Hettangian–Sinemurian (Jurassic) age made up of chiefly by sandstone, tuff, mudstone and limestone.
 The formation is located in the Coast Range of northern Chile.
 The formation interdigitates and is coeval with the Posada de los Hidalgo Formation.
 It concordantly overlies the Cifuncho Formation and is overlain by the La Negra Formation.
The Chattanooga Shale is a geologic formation in Kentucky, Missouri and Tennessee.
 It preserves conodont fossils dating to the Devonian Period.
 It occurs mostly as a subsurface geologic formation composed of layers of shale.
 It is located in Eastern Tennessee and also extends into southeastern Kentucky, northeastern Georgia, and northern Alabama.
 This part of Alabama is part of the Black Warrior Basin.