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  2. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [1] was a large landmass, sometimes referred to as a supercontinent.The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian Subcontinent.

  3. Variscan orogeny - Wikipedia

    en.wikipedia.org/wiki/Variscan_orogeny

    Location of the Hercynian-Alleghenian mountain belts in the middle of the Carboniferous period.Present day coastlines are indicated in grey for reference. [1]The Variscan orogeny, or Hercynian orogeny, was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.

  4. List of state and territorial universities in the United States

    en.wikipedia.org/wiki/List_of_state_and...

    The flagship campus is the most prestigious or the one with the largest student population, e.g. the University of Maryland, College Park campus in the University System of Maryland, the Indiana University Bloomington campus in the Indiana University System, and the University of Tennessee, Knoxville campus in the University of Tennessee System.

  5. Pannotia - Wikipedia

    en.wikipedia.org/wiki/Pannotia

    Pannotia was centred on the South Pole, hence its name. Pannotia (from Greek: pan-, "all", -nótos, "south"; meaning "all southern land"), also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African supercontinent, was a relatively short-lived Neoproterozoic supercontinent that formed at the end of the Precambrian during the Pan-African orogeny (650–500 Ma), during the ...

  6. Pan-African orogeny - Wikipedia

    en.wikipedia.org/wiki/Pan-African_orogeny

    The Mozambique Belt, extending from east Antarctica through East Africa up to the Arabian-Nubian Shield, formed as a suture between plates during the Pan-African orogeny. [8] The Mozambique ocean began closing between Madagascar-India and the Congo – Tanzania craton between 700 and 580 million years ago, with closure between 600 and 500 ...

  7. Texas State University - Wikipedia

    en.wikipedia.org/wiki/Texas_State_University

    Texas State University comprises over 8 million gross square feet in facilities and its campuses are located on over 600 acres with an additional 4,000 acres of agriculture, research, and recreational areas. The Texas State University main campus is located in San Marcos, Texas, midway between Austin and San Antonio along Interstate 35.

  8. Natural history of Australia - Wikipedia

    en.wikipedia.org/wiki/Natural_history_of_Australia

    Australia separated from Gondwana 99 Ma, and initially remained warm and humid with rainforest vegetation. Inland Australia had systems of rivers and lakes with abundant wildlife. Fossil birds, platypus, frogs and snakes are present from this period. From 30 Ma there was a period of global cooling, and from 15 Ma the Antarctic ice sheet formed.

  9. Gondi people - Wikipedia

    en.wikipedia.org/wiki/Gondi_people

    The Gond have formed many kingdoms of historical significance. Gondwana was the ruling kingdom in the Gondwana region of India. This includes the eastern part of the Vidarbha of Maharashtra. The Garha Kingdom includes the parts of Madhya Pradesh immediately to the north of it and parts of western Chhattisgarh. The wider region extends beyond ...