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Hypothetical Neoarchaean supercontinent from about 2.8 billion years ago
Kenorland is a hypothetical Neoarchean supercontinent. If it existed, it would have been one of the earliest known supercontinents on Earth. It is thought
Kenorland
First period of the Paleoproterozoic Era
activity in this period revolved around the breakup of the supercontinent Kenorland. While this event mainly occurred in the North American craton, volcanic
Siderian
Fourth era of the Archean Eon
During this era, the supercontinent Kenorland is proposed to have formed about 2.7 billion years ago. Kenorland is of particular interest due to it containing
Neoarchean
Landmass comprising more than one continental core, or craton
two separate supercontinents existed comprising Vaalbara and Kenorland, with Kenorland comprising Superia and Sclavia. These parts of Neoarchean age
Supercontinent
Ocean that surrounds a supercontinent
Pannotia and Columbia, along with landmasses before Columbia (such as Ur and Kenorland), were also surrounded by superoceans. As surface water moves unobstructed
Superocean
Majority of lands of the Western Hemisphere
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
New_World
History of Earth 4600–539 million years ago
750–600 million years ago. Map of Kenorland supercontinent 2.5 billion years ago[citation needed] Map of Kenorland breaking up 2.3 billion years ago[citation
Precambrian
Craton forming the geological core of North America
Arctica was part of the supercontinent Kenorland.[clarification needed] Around 2.1 to 1.84 Ga, when Kenorland broke apart, the Arctican craton was part
Laurentia
Landmass corresponding to Afro–Eurasia
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
Old_World
Fictional island in Plato's works
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
Atlantis
Ancient continent in the Neoarchean era
of Arctica was the Canadian Shield, which Williams et al. 1991 named Kenorland. They argued that this continent formed around 2.5 Ga and then rifted
Arctica
Large geographical region identified by convention
the world's cratons or continental cores. These have included Vaalbara, Kenorland, Columbia, Rodinia, Pannotia, and Pangaea. Over time, these supercontinents
Continent
Mostly submerged continental crust area in Oceania
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
Zealandia
Failed microcontinent between Greenland and Canada
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
Davis Strait proto-microcontinent
Davis_Strait_proto-microcontinent
Topics referred to by the same term
Zealand, New Caledonia, and some Australian islands. Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Arctica Asiamerica
Forgotten_continent
Geologic province
consumed the Superior province's oceanic crust. Fragmentation of the Kenorland supercontinent began 2,450 million years ago and was completed by 2,100
Great_Lakes_tectonic_zone
Hypothetical continent
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
Terra_Australis
Mountain-building event in North America
least three former major supercontinents, including Laurasia, Pangaea and Kenorland (ca. 2.7 Ga), and contain parts of some of the oldest cratonic continental
Trans-Hudson_orogeny
City in Ontario, Canada
today's continents, predating Pangaea by 2.4 billion years, has been termed Kenorland by geologists, named after the Kenoran orogeny (also called the Algoman
Kenora
Late Archean supercraton
configuration of the Archean supercraton from which they were derived is unknown. Kenorland, a proposed supercontinent, is a "one-piece" alternative to three separate
Sclavia_Craton
Late Archaean episode of mountain building in what is now North America
with the Sask and Wyoming cratons to form the first supercontinent, the Kenorland supercontinent. Through most of the Archean Eon, the Earth had a heat
Algoman_orogeny
Repeated joining and separation of Earth's continents
supercontinents: starting with Vaalbara (3.6 to 2.8 Ga); Ur (c. 3 Ga); Kenorland (2.7 to 2.1 Ga); Columbia (1.8 to 1.5 Ga); Rodinia (1.25 Ga to 750 Ma);
Supercontinent_cycle
Records of Earth's development
in a process known as abiogenesis. The continents of Ur, Vaalbara and Kenorland may have existed around this time. The atmosphere is composed of volcanic
History_of_Earth
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
List of sovereign states and dependent territories by continent
List_of_sovereign_states_and_dependent_territories_by_continent
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
List_of_Indigenous_peoples
Cratonic rock body which makes up most of the continent Antarctica
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
East_Antarctic_Shield
Archean era volcano in western Quebec, Canada
collapse of a broad subaqueous shield volcano. "Hunter Project" (PDF). Kenorland Minerals. Retrieved 2022-06-30.[dead link] "Physical volcanology of volcanogenic
Normetal_caldera
supercontinent India Continent Kalahari Craton Kazakhstania Continent Kenorland 2720 Neoarchean Supercontinent Alternatively, landmasses may have grouped
List_of_paleocontinents
Image Reference Vaalbara Eoarchean 3.6-2.7 Ga Ur Paleoarchean 3.1 Ga Kenorland Neoarchean 2.7 Ga Arctica Neoarchean 2.565 Ga Columbia Paleoproterozoic
Chronology_of_continents
terranes of existing continental crust. c. 2,900 Ma – Assembly of the Kenorland supercontinent, based upon the core of the Baltic shield, formed at c
Timeline_of_Earth
Americas Eurasia Oceania Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents
List of sovereign states and dependent territories by continent (data file)
List_of_sovereign_states_and_dependent_territories_by_continent_(data_file)
Archean era volcano in western Quebec, Canada
regionally extensive and temporally early exhalite. "Hunter Project" (PDF). Kenorland Minerals. Retrieved 2022-06-30.[dead link] "The Selbaie Zn-Cu-Ag deposits
Selbaie_caldera
Archean era volcano in western Quebec, Canada
subaerial in origin. List of volcanoes in Canada "Hunter Project" (PDF). Kenorland Minerals. Retrieved 2022-06-30. Mueller, W.U.; Stix, J.; Corcoran, P.L
Gemini_caldera
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Las_Juntas_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Sabana_Formation
Science of analyzing the age of zircons
Ga (Figure 6) may correlate the break-up of Rodinia and supercontinent Kenorland respectively. Apart from the detrital zircon age abundance, difference
Detrital_zircon_geochronology
Geologic formation in South America
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
La_Quinta_Formation
Geological group in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Honda_Group,_Colombia
Geological Formation of the Western and Eastern Ranges of the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Santa_Teresa_Formation
Geologic formation in Northeastern Ontario, Canada
7 billion years old, dates back to the formation of the supercontinent Kenorland between 2.8 and 2.6 billion years ago. This large landmass consisted of
Temagami_Greenstone_Belt
Hierarchical outline list of articles related to plate tectonics
of redirect targets Gondwana – Neoproterozoic to Cretaceous landmass Kenorland – Hypothetical Neoarchaean supercontinent from about 2.8 billion years
Outline_of_plate_tectonics
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Chipaque_Formation
Geological formation in Bogotá, Colombia
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Bogotá_Formation
Sedimentary basin in Colombia
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Llanos_Basin
Geologic formation in the Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Rosablanca_Formation
Early Jurassic geological formation in northern Colombia
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Noreán_Formation
Early Cretaceous geologic formation of central Colombia
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Paja_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Venado_Formation
Geological formation of the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Regadera_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Guaduas_Formation
Geological group in the Venezuelan Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Río_Cachirí_Group
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Loma_Gorda_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Cuche_Formation
Geologic formation in Colombia
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Macanal_Formation
Geological Formation
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Une_Formation
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Guadalupe_Group
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Usme_Formation
Geological formation in Colombia
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Caballos_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Marichuela_Formation
Geological formation in South America
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Subachoque_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Fómeque_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Floresta_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Arcabuco_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Soatá_Formation
Geological formation in the Colombian Andes
pre-Garzón 1800 Tapajós orogeny Mitú (1800) 1950 Transamazonic orogeny pre-Mitú 2200 Columbia 2530 Archean Carajas-Imataca orogeny 3100 Kenorland Sources
Barzalosa_Formation
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