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Hypothetical Neoproterozoic supercontinent
Rodinia (from the Russian родина, rodina, meaning "motherland, birthplace"[page needed]) was a Mesoproterozoic and Neoproterozoic supercontinent that
Rodinia
Landmass comprising more than one continental core, or craton
masses, forming Rodinia. Between ~825 and 750 Ma Rodinia broke apart. However, before completely breaking up, some fragments of Rodinia had already come
Supercontinent
Mountain range in eastern North America
continents of Laurentia and Amazonia collided, creating a supercontinent called Rodinia. The collision of these continents caused the rocks to be folded and faulted
Appalachian_Mountains
Northern landmass that formed part of the Pangaea supercontinent
core of the supercontinent Rodinia, which formed 1,260-900 Mya. However, the exact fit of various continents within Rodinia is debated. In some reconstructions
Laurasia
Ancient supercontinent of approximately 2,500 to 1,500 million years ago
Laurentia are similar to their corresponding fits in the configuration of Rodinia. This continental configuration is based on the available geological reconstructions
Columbia_(supercontinent)
Hypothesized Neoproterozoic supercontinent
propose a Proterozoic supercontinent preceding Pangaea, today known as Rodinia. At that time he simply referred to it as "the Proterozoic super-continent"
Pannotia
Craton forming the geological core of North America
margin of the continent is thought to have contributed to the formation of Rodinia. According to the Southwest U.S. and East Antarctica or SWEAT hypothesis
Laurentia
Prehistoric superocean that surrounded Pangaea
Pacific Ocean is a direct continuation of Panthalassa. The supercontinent Rodinia began to break up 870–845 Ma probably as a consequence of a superplume
Panthalassa
Geologic eon, 2500–539 million years ago
have decreased in magnitude after every period. Columbia, about 1,590 Ma Rodinia, about 900 Ma Pannotia, 545 Ma (disputed[clarification needed]), centered
Proterozoic
Supercontinent from the late Paleozoic to early Mesozoic eras
broke up, and the next supercontinent, Rodinia, formed from the accretion and assembly of its fragments. Rodinia lasted from about 1.3 billion years ago
Pangaea
First period of the Neoproterozoic Era
breakup of Rodinia. However, there has been little evidence for the breakup of Rodinia during the mid-Tonian, with most agreeing that Rodinia began breaking
Tonian
Geologic description of the Appalachian Mountains
Mesoproterozoic era when two continental cratons collided to form the supercontinent Rodinia. The rocks exposed in today's Appalachian Mountains reveal elongate belts
Geology_of_the_Appalachians
Last period of the Mesoproterozoic Era
followed by the Neoproterozoic era and the Tonian period. The supercontinent Rodinia finished assembly during the Stenian, having started during the Ectasian
Stenian
Ocean that surrounds a supercontinent
global superoceans include Mirovia, which surrounded the supercontinent Rodinia, and Panthalassa, which surrounded the supercontinent Pangaea. Pannotia
Superocean
Mostly submerged continental crust area in Oceania
origins from early Gondwana formations of 500 to 700 million years ago, Rodinia formations about a billion years ago and sources from an expanded-Ur continent
Zealandia
Country in Oceania
inhabitants per square kilometre in central Melbourne. Formerly part of the Rodinia and Gondwana supercontinents, Australia completely separated from Antarctica
Australia
(2626): 36–40. doi:10.1016/S0262-4079(07)62661-X. Rogers & Santosh 2003, Rodinia, pp. 363–364 Pesonen, L. J.; Elming, S.-Å.; Mertanen, S.; Pisarevsky, S
Chronology_of_continents
Hypothetical Archaean supercontinent from about 3.1 billion years ago
Ur joined the continents Nena and Atlantica to form the supercontinent Rodinia. In the reconstruction of Rogers 1996, Ur remained the nucleus of eastern
Ur_(continent)
Records of Earth's development
supercontinent Rodinia. Rodinia may have been preceded by Early-Middle Proterozoic continents called Nuna and Columbia. After the break-up of Rodinia about 800 Ma
History_of_Earth
Geological feature
that ringed the ancient, active southern margin of the supercontinents Rodinia and later Pannotia (also called Greater Gondwana). This vast orogenic belt
Terra_Australis_Orogen
Vernikovsky, V. (2008). "Assembly, configuration, and break-up history of Rodinia: A synthesis". Precambrian Research. 160 (1–2): 179–210. Bibcode:2008PreR
List_of_paleocontinents
History of Earth 4600–539 million years ago
into a single supercontinent around 1130 Ma. The supercontinent, known as Rodinia, broke up around 750 Ma. A number of glacial periods have been identified
Precambrian
Third planet from the Sun
apart. At approximately 750 Ma, one of the earliest known supercontinents, Rodinia, began to break apart. The continents later recombined to form Pannotia
Earth
Neoproterozoic to Cretaceous landmass
orogeny, caused the continental fragments of a much older supercontinent, Rodinia, to amalgamate. One of those orogenic belts, the Mozambique Belt, formed
Gondwana
Fictional island in Plato's works
supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica Asiamerica
Atlantis
Precambrian continental block located in China
element (REE) ores. Second, the South China Block is a key component of the Rodinia supercontinent. Therefore, such study helps us understand more about the
South_China_Craton
Repeated joining and separation of Earth's continents
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); and Pannotia (c. 600 Ma), whose dispersal produced
Supercontinent_cycle
Third and last era of the Proterozoic Eon
supercontinent Rodinia, which had assembled during the late Mesoproterozoic, straddled the equator. During the Tonian, rifting commenced which broke Rodinia into
Neoproterozoic
System that relates geologic strata to time
Rodinian Period/System (1780–850 Ma) – named after the supercontinent Rodinia, stable environment. Proposed pre-Cambrian timeline (GTS2012), shown to
Geologic_time_scale
Worldwide glaciation episodes during the Proterozoic eon
Department of Earth and Planetary Sciences, and others, reported evidence that Rodinia was at equatorial latitude during the Cryogenian period with glacial ice
Snowball_Earth
Failed microcontinent between Greenland and Canada
supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica Asiamerica
Davis Strait proto-microcontinent
Davis_Strait_proto-microcontinent
Large geographical region identified by convention
continental cores. These have included Vaalbara, Kenorland, Columbia, Rodinia, Pannotia, and Pangaea. Over time, these supercontinents broke apart into
Continent
Major geological province in Australia
supercontinent Rodinia. The Adelaide Superbasin has been the subject of much research, as it contains geological evidence for the breakup of Rodinia; two Snowball
Adelaide_Superbasin
Landmass corresponding to Afro–Eurasia
supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica Asiamerica
Old_World
Cratonic rock body which makes up most of the continent Antarctica
plates during the amalgamation and separation of the supercontinents, Rodinia, Gondwana, and Pangea. Because the surface of the shield is covered by
East_Antarctic_Shield
Tribe of butterflies
Roeberella Subtribe Pandemina Adelotypa Calospila Calliona Livendula Pandemos Rodinia Setabis Zelotaea Subtribe Stalachtina Protonymphidia Stalachtis Subtribe
Nymphidiini
Hypothesized superocean surrounding the supercontinent Rodinia in the Neoproterozoic Era
superocean which may have been a global ocean surrounding the supercontinent Rodinia in the Neoproterozoic Era, about 1 billion to 750 million years ago. Mirovia
Mirovia
Major landmass in the geological past
has changed throughout its existence. Gondwana was a smaller piece of Rodinia and stayed together all the way until the breakup of Pangea. That allowed
Paleocontinent
Movement of Earth's lithosphere
and broke up about 1,500 to 1,300 million years ago. The supercontinent Rodinia is thought to have formed about 1 billion years ago and to have embodied
Plate_tectonics
Claim of past rapid changes of the Earth's axis
Between approximately 790 and 810 million years ago, when the supercontinent Rodinia existed, two geologically rapid phases of true polar wander may have occurred
Cataclysmic pole shift hypothesis
Cataclysmic_pole_shift_hypothesis
Development of the earth
North, South and West cratons. Rodinia broke up between 830 and 745 Ma; at around 750 Ma the western side of Rodinia called Laurentia broke away from
Natural_history_of_Australia
U.S. state
August 10, 2014, at the Wayback Machine Roads compared to other states Rodinia to Pangea: The Lithotectonic Record of the Appalachian Region Laurentia-Gondwana
Vermont
Continent
Baltica and Arctica (as part of the Laurentia block) became joined to Rodinia, later resplitting around 550 million years ago to reform as Baltica. Around
Europe
Hypothetical continent
supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica Asiamerica
Terra_Australis
supercontinent. Roughly 750 million years ago, the earliest-known supercontinent Rodinia, began to break apart. The continents later recombined to form Pannotia
Geological_history_of_Earth
Mountain range along the eastern coast of India
of the Indian subcontinent post the break-up of the supercontinent of Rodinia and the formation of Gondwana. The mountains were formed through further
Eastern_Ghats
Late-Proterozoic to early-Palaeozoic continent
European Craton, is more than three billion years old and formed part of the Rodinia supercontinent at c. 1 Ga. Baltica formed at c. 2.0–1.7 Ga by the collision
Baltica
Second era of the Proterozoic Eon
era are the breakup of the Columbia supercontinent, the formation of the Rodinia supercontinent, and the evolution of sexual reproduction. This era is marked
Mesoproterozoic
Ancient continent formed during the Proterozoic about 2 billion years ago
Ur and some minor plates formed the supercontinent Rodinia about 1 Ga ago. Between 1–0.5 Ga Rodinia split into three new continents: Laurasia and East
Atlantica
Scientific study of Earth's physical composition
5 Ga: Columbia supercontinent 1,100–750 Ma (megaannum: million years ago): Rodinia supercontinent 730–635 Ma: second snowball Earth 650–540 Ma: Pannotia supercontinent
Geology
Majority of lands of the Western Hemisphere
supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica Asiamerica
New_World
African geological area
Kalahari Craton. At 1.11 Ga, during the assembly of the supercontinent Rodinia, the Kalahari Craton was affected by the Umkondo-Borg Large Igneous Province
Kalahari_Craton
Mesoproterozoic mountain-building event
mountain-building event associated with the assembly of the supercontinent Rodinia. Its record is a prominent orogenic belt which spans a significant portion
Grenville_orogeny
Desert in the southwestern United States
event. Rifting thinned huge roughly linear parts of the supercontinent Rodinia enough to allow sea water to invade and divide its landmass into component
Mojave_Desert
Earth history, 1.8 to 0.8 billion years ago
10% of modern levels. It was ended by the breakup of the supercontinent Rodinia during the Tonian (1000–720 Ma) period, a second oxygenation event, and
Boring_Billion
Ocean that existed in the late Neoproterozoic and early Paleozoic eras
birth of the Iapetus Ocean came from the breakup of the supercontinent Rodinia. After its formation ~1100 Ma, extension and eventual supercontinent break-up
Iapetus_Ocean
R.P.; Bartholomew, M.J.; Hibbard, J.P.; Karabinos, P.M. (eds.). From Rodinia to Pangea: The Lithotectonic Record of the Appalachian Region, GSA Memoir
List of subranges of the Appalachian Mountains
List_of_subranges_of_the_Appalachian_Mountains
Hypothetical Archaean supercontinent from about 3.6 to 2.7 billion years ago
East Antarctica during the Mesoproterozoic assembly of the supercontinent Rodinia and the Grenville orogeny. The Neoproterozoic Pan-African orogeny and the
Vaalbara
Plateau region located in the eastern United States
Grenville orogeny (the collision of continents that created the supercontinent Rodinia) and the Appalachian orogeny during the formation of Pangaea. The last
Piedmont_(plateau)
Reinhardt A.; Brito Neves, Benjamim Bley; Schobbenhaus, Carlos (2008). "Rodinia descendants in South America". Precambrian Research. 160: 108–126. Retrieved
List_of_tectonic_plates
Hypothesized paleo-ocean whose closure created the supercontinent of Pannotia
The ocean may have existed before the break-up of the supercontinent of Rodinia. The ocean closed before the beginning of the Phanerozoic Eon, when the
Pan-African_Ocean
Market in Asaba Delta State
Nigeria". 2017-09-17. Retrieved 2021-08-29. "Ogbeogonogo Market". The Rodinia Hotel. 2018-07-22. Retrieved 2021-08-29. "Delta govt hands over Ogbeogonogo
Ogbe-Ogonogo_Modern_Market
in North America: globally associated with assembly of Supercontinent Rodinia establishes Grenville Province in Eastern North America – folded mountains
Timeline_of_Earth
Ancient craton in eastern South America
1.0 Ga ago was in the south of the supercontinent Rodinia, and after the fragmentation of Rodinia in the late Proterozoic (700 Ma) became a member of
São_Francisco_Craton
existence of the supercontinent Rodinia. There is no general agreement as to the position of northern Scotland within Rodinia but some models locate it close
Knoydartian_Orogeny
American paleontologist
new fossil genera and species, and naming the Precambrian supercontinent Rodinia and the superocean Mirovia. The Cambrian archeocyathid species Markocyathus
Mark_McMenamin
Earth's outer shell of rock
orogeny, which coincide with the formation of the supercontinents such as Rodinia, Pangaea and Gondwana. The crust forms in part by aggregation of island
Earth's_crust
Second period of the Neoproterozoic Era, with major glaciation
around 750 million years ago, the cratons that made up the supercontinent Rodinia started to rift apart. The superocean Mirovia began to close while the
Cryogenian
The Laurentia craton is the center of the Proterozoic supercontinent Rodinia in most models, and was also part of the later Laurussia, Pangea, and Laurasia
Geography_of_North_America
Gap in geological strata in the Grand Canyon
proposed that multiple smaller events, such as the formation and breakup of Rodinia, created many unconformities worldwide. Geology of the Grand Canyon area
Great_Unconformity
Mountain building event 1.7 billion years ago in the southwestern United States
Mya Grenville orogeny during the final assembly of the supercontinent Rodinia, which ended an 800-million-year episode of convergent boundary tectonism
Yavapai_orogeny
Norwegian princess (born 1971)
Prinsesse Märtha Louises eventyrlige verden, Eventyr fra jordens hjerte, Rodinia containing 67 fairy tales from 50 countries. In 2009, she and her Astarte
Princess Märtha Louise of Norway
Princess_Märtha_Louise_of_Norway
Largest ocean
zones. The Pacific Ocean was born 750 million years ago at the breakup of Rodinia, although it is generally called the Panthalassa until the breakup of Pangea
Pacific_Ocean
First era of the Phanerozoic Eon
Proterozoic plate tectonics and palaeogeography: A tale of two supercontinents, Rodinia and Pannotia". Geological Society, London, Special Publications. 326 (1):
Paleozoic
Geophysical model of the opening and closing of rifts
cycles and Wilson cycles were involved in the formation of Pangaea and of Rodinia. The 50-year retrospective in the Geological Society of London Special
Wilson_Cycle
Microcontinent in the Paleozoic era
Carolina about 800 Ma from volcanic arcs far offshore from the supercontinent Rodinia, most likely outboard continental terranes of more obvious West African
Avalonia
Low-lying basin filled with Cretaceous to recent sediments
aulacogen, which dates back to the Precambrian break-up of the supercontinent Rodinia. The more recent opening of the Atlantic Ocean and Gulf of Mexico during
Mississippi_embayment
Tectonic plate carrying the bulk of southern China
earthquake. The Yangtze plate was formed by the disaggregation of the Rodinia supercontinent 750 million years ago, in the Neoproterozoic era. South
Yangtze_plate
Precambrian "proto-Atlantic" ocean in the Southern Hemisphere
Ocean was a "proto-Atlantic" ocean that formed with the break-up of the Rodinia supercontinent c. 780–750 Ma. It separated the Río de la Plata Craton from
Adamastor_Ocean
Ancient continent in the Neoarchean era
Around 1 Ga Nena, Ur, and Atlantica collided to form the supercontinent Rodinia. Rogers & Santosh 2003 argued that most cratons that were around at 2.5 Ga
Arctica
Earth's dry surface
750 mya (million years ago), one of the earliest known supercontinents, Rodinia, began to break apart. The continents later recombined to form Pannotia
Land
Mountain, highest point in Tennessee, United States
Carolina, to Georgia. These basins were rift basins formed by the rifting of Rodinia. The initial metamorphism of the Ocoee Supergroup occurred about 400 million
Kuwohi
Mountain-building event in North America
Mya Grenville orogeny during the final assembly of the supercontinent Rodinia, which ended an 800-million-year episode of convergent boundary tectonism
Mazatzal_orogeny
Transamazonian orogeny (2000 million years ago (mya)), the breakup of Rodinia (700–500 mya) and the opening of the South Atlantic (~145 mya). The Precambrian
Geology_of_Uruguay
Third period of the Paleoproterozoic Era
(2002). "Review of global 2.1–1.8 Ga orogens: implications for a pre-Rodinia supercontinent". Earth-Science Reviews. 59 (1). Abstract. Bibcode:2002ESRv
Orosirian
history related to the assembly and breakup of the ancient supercontinent of Rodinia and the assembly of the Gondwana supercontinent. The Eastern Ghats are
Geography_of_India
Terra Australis orogeny that began during the Neoproterozoic break-up of Rodinia and culminated in the closure of the Adamastor and Mozambique oceans. During
Ellsworth–Whitmore_Mountains
Precambrian craton that with four others makes up the modern continent of Africa
western edge of Congo Craton was the location for the initial rifting of Rodinia before its break-up. During the Neoproterozoic, Central Congo or Bas-Congo
Congo_Craton
Fourth and last period of the Paleoproterozoic Era
(November 2002). "Review of global 2.1–1.8 Ga orogens: implications for a pre-Rodinia supercontinent". Earth-Science Reviews. 59 (1–4): 125–162. Bibcode:2002ESRv
Statherian
Topics referred to by the same term
Australian islands. Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Arctica Asiamerica Atlantica Avalonia Baltica Cimmeria Congo
Forgotten_continent
Period of long-term reduction in temperature of Earth's surface and atmosphere
Arctic Ocean is today. A supercontinent covers most of the equator, as Rodinia did during the Cryogenian period. Since today's Earth has a continent over
Ice_age
Phyllosilicate mineral in the pyrophyllite-talc group
of the Neoproterozoic Callison Lake Formation: Linking the break-up of Rodinia to the Islay carbon isotope excursion". American Journal of Science. 315
Talc
populous areas around Las Vegas. The region was part of the supercontinent Rodinia one billion years ago, situated at the equator. The continent rifted apart
Geology_of_Nevada
American computer scientist
the research community, including the HotSpot family of tools and the Rodinia Benchmark Suite. Skadron also helped co-found IEEE Computer Architecture
Kevin_Skadron
the latter four periods involved the amalgamation and dispersal of Nuna, Rodinia and Pangea, respectively. The Australian landmass has been part of all
Geology_of_Australia
Band in the Earth's crust from East Antarctica to the Arabian-Nubian Shield
geologists consider that the Mozambique Ocean formed during the break-up of Rodinia between 800 and 700 million years ago, accompanied by volcanic activity
Mozambique_Belt
Mountain-forming event that formed the Appalachian and Allegheny Mountains
R.P.; Bartholomew, M.J.; Hibbard, J.P.; Karabinos, P.M. (eds.). From Rodinia to Pangea: The Lithotectonic Record of the Appalachian Region, GSA Memoir
Alleghanian_orogeny
China Block, but a part of supercontinent Rodinia. At the subducting plate boundary, it collided with Rodinia and was folded up forming North Qinling Belt
Qinling_orogenic_belt
Overview article
concurrent with the assembly of Rodinia. The deposition of the upper Vindhyan Supergroup may also denote the final episode of Rodinia formation. Several geochemical
Tectonic evolution of the Aravalli Mountains
Tectonic_evolution_of_the_Aravalli_Mountains
American hydrologist and geochemist
L. (July 2000). "Chuar Group of the Grand Canyon: record of breakup of Rodinia, associated change in the global carbon cycle, and ecosystem expansion
Laura_J._Crossey
RODINIA
RODINIA
RODINIA
RODINIA
Boy/Male
Hindu
Male
Irish
Pet form of Irish Gaelic Bairtliméad, BARTLE means "son of Talmai."
Girl/Female
Gujarati, Hindu, Indian, Sanskrit
Soul
Surname or Lastname
English, Scottish, and Indian (southern states)
English, Scottish, and Indian (southern states) : variant spelling of Matthew. It is found as a personal name among Christians in India, and in the U.S. is used as a family name among families from southern India.
Boy/Male
British, English
Bright Raven
Boy/Male
Gujarati, Hindu, Indian, Kannada, Malayalam, Marathi, Tamil
Peace and Calm
Girl/Female
Hindu
Quiet
Boy/Male
Tamil
Divider
Surname or Lastname
English
English : nickname from the bird, Middle English wrenne, probably in reference to its small size.Irish : Anglicized form of Gaelic Ó Rinn ‘descendant of Rinn’, a personal name possibly derived from reann ‘spear’.Welsh : Anglicized form of Welsh Uren.
Girl/Female
Latin American
Concord.
RODINIA
RODINIA
RODINIA
RODINIA
RODINIA