Question: When did the continent where Bailey took the circus after Barnum died, arrive at its present day location?

full_context: Document 1: The Royal London Circus: The Royal London Circus is a famous travelling circus show based in Danga Bay, Johor in Malaysia. The Royal London Circus has performed in the country since 1990. The circus is now officially under receivership and owes a lot of money to creditors.
Document 2: Ringling Bros. and Barnum & Bailey Circus: Independently of Castello and Coup, James Anthony Bailey had teamed up with James E. Cooper to create the Cooper and Bailey Circus in the 1860s. The Cooper and Bailey Circus became the chief competitor to Barnum's circus. As Bailey's circus was outperforming his, Barnum sought to merge the circuses. The two groups agreed to combine their shows on March 28, 1881. Initially named ``P.T. Barnum's Greatest Show On Earth, And The Great London Circus, Sanger's Royal British Menagerie and The Grand International Allied Shows United '', it was eventually shortened to`` Barnum and Bailey's Circus''. Bailey was instrumental in acquiring Jumbo, advertised as the world's largest elephant, for the show. Barnum died in 1891 and Bailey then purchased the circus from his widow. Bailey continued touring the eastern United States until he took his circus to Europe. That tour started on December 27, 1897, and lasted until 1902.
Document 3: Geological history of Earth: Antarctica continued to become more isolated and finally developed a permanent ice cap. Mountain building in western North America continued, and the Alps started to rise in Europe as the African plate continued to push north into the Eurasian plate, isolating the remnants of Tethys Sea. A brief marine incursion marks the early Oligocene in Europe. There appears to have been a land bridge in the early Oligocene between North America and Europe since the faunas of the two regions are very similar. During the Oligocene, South America was finally detached from Antarctica and drifted north toward North America. It also allowed the Antarctic Circumpolar Current to flow, rapidly cooling the continent.
Document 4: Geological history of Earth: The northern supercontinent of Laurasia began to break up, as Europe, Greenland and North America drifted apart. In western North America, mountain building started in the Eocene, and huge lakes formed in the high flat basins among uplifts. In Europe, the Tethys Sea finally vanished, while the uplift of the Alps isolated its final remnant, the Mediterranean, and created another shallow sea with island archipelagos to the north. Though the North Atlantic was opening, a land connection appears to have remained between North America and Europe since the faunas of the two regions are very similar. India continued its journey away from Africa and began its collision with Asia, creating the Himalayan orogeny.
Document 5: Geological history of Earth: In many ways, the Paleocene continued processes that had begun during the late Cretaceous Period. During the Paleocene, the continents continued to drift toward their present positions. Supercontinent Laurasia had not yet separated into three continents. Europe and Greenland were still connected. North America and Asia were still intermittently joined by a land bridge, while Greenland and North America were beginning to separate. The Laramide orogeny of the late Cretaceous continued to uplift the Rocky Mountains in the American west, which ended in the succeeding epoch. South and North America remained separated by equatorial seas (they joined during the Neogene); the components of the former southern supercontinent Gondwana continued to split apart, with Africa, South America, Antarctica and Australia pulling away from each other. Africa was heading north toward Europe, slowly closing the Tethys Ocean, and India began its migration to Asia that would lead to a tectonic collision and the formation of the Himalayas.
Document 6: William Jackson Palmer: Heading west in 1867, while Palmer helped build the Kansas Pacific Railway he met a young English doctor, Dr. William Abraham Bell who became his friend and partner in most of his business ventures in which we would generally find Palmer as president with Bell as vice president. The two men are best known as co-founders of the Denver and Rio Grande Western Railroad (Rio Grande). The Rio Grande and its successors eventually operated the largest network of narrow gauge railroad in the United States, and ultimately became part of the 21st century Union Pacific Railroad.
Document 7: Old Bet: The first elephant brought to the United States was in 1796, aboard the America which set sail from Calcutta for New York on December 3, 1795. However, it is not certain that this was Old Bet. The first references to Old Bet start in 1804 in Boston as part of a menagerie. In 1808, while residing in Somers, New York, Hachaliah Bailey purchased the menagerie elephant for $1,000 and named it ``Old Bet ''.
Document 8: PricewaterhouseCoopers: In 1854 William Cooper founded an accountancy practice in London, which became Cooper Brothers seven years later when his three brothers joined.In 1898, Robert H. Montgomery, William M. Lybrand, Adam A. Ross Jr. and his brother T. Edward Ross formed Lybrand, Ross Brothers and Montgomery in the United States.In 1957 Cooper Brothers; Lybrand, Ross Bros & Montgomery and a Canadian firm McDonald, Currie and Co agreed to adopt the name Coopers & Lybrand in international practice. In 1973 the three member firms in the UK, US and Canada changed their names to Coopers & Lybrand. Then in 1980 Coopers & Lybrand expanded its expertise in insolvency substantially by acquiring Cork Gully, a leading firm in that field in the UK. In 1990 in certain countries including the UK, Coopers & Lybrand merged with Deloitte Haskins & Sells to become Coopers & Lybrand Deloitte: in 1992 they reverted to Coopers & Lybrand.
Document 9: Blackpool Tower: Animals appeared in the circus until 1990. It was planned to close the circus at the end of the 1990 season and replace it with an animatronic attraction. Public opinion and the fact the animatronics were not ready meant that the circus continued.
Document 10: Geological history of Earth: The Devonian spanned roughly from 419 to 359 Ma. The period was a time of great tectonic activity, as Laurasia and Gondwana drew closer together. The continent Euramerica (or Laurussia) was created in the early Devonian by the collision of Laurentia and Baltica, which rotated into the natural dry zone along the Tropic of Capricorn. In these near-deserts, the Old Red Sandstone sedimentary beds formed, made red by the oxidized iron (hematite) characteristic of drought conditions. Near the equator Pangaea began to consolidate from the plates containing North America and Europe, further raising the northern Appalachian Mountains and forming the Caledonian Mountains in Great Britain and Scandinavia. The southern continents remained tied together in the supercontinent of Gondwana. The remainder of modern Eurasia lay in the Northern Hemisphere. Sea levels were high worldwide, and much of the land lay submerged under shallow seas. The deep, enormous Panthalassa (the "universal ocean") covered the rest of the planet. Other minor oceans were Paleo-Tethys, Proto-Tethys, Rheic Ocean and Ural Ocean (which was closed during the collision with Siberia and Baltica).
Document 11: Geological history of Earth: The Cenozoic Era covers the 66 million years since the Cretaceous -- Paleogene extinction event up to and including the present day. By the end of the Mesozoic era, the continents had rifted into nearly their present form. Laurasia became North America and Eurasia, while Gondwana split into South America, Africa, Australia, Antarctica and the Indian subcontinent, which collided with the Asian plate. This impact gave rise to the Himalayas. The Tethys Sea, which had separated the northern continents from Africa and India, began to close up, forming the Mediterranean sea.
Document 12: Europe: The geological history of Europe traces back to the formation of the Baltic Shield (Fennoscandia) and the Sarmatian craton, both around 2.25 billion years ago, followed by the Volgo -- Uralia shield, the three together leading to the East European craton (≈ Baltica) which became a part of the supercontinent Columbia. Around 1.1 billion years ago, 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 440 million years ago Euramerica was formed from Baltica and Laurentia; a further joining with Gondwana then leading to the formation of Pangea. Around 190 million years ago, Gondwana and Laurasia split apart due to the widening of the Atlantic Ocean. Finally, and very soon afterwards, Laurasia itself split up again, into Laurentia (North America) and the Eurasian continent. The land connection between the two persisted for a considerable time, via Greenland, leading to interchange of animal species. From around 50 million years ago, rising and falling sea levels have determined the actual shape of Europe, and its connections with continents such as Asia. Europe's present shape dates to the late Tertiary period about five million years ago.
Document 13: Geological history of Earth: The Cenozoic Era covers the 66 million years since the Cretaceous–Paleogene extinction event up to and including the present day. By the end of the Mesozoic era, the continents had rifted into nearly their present form. Laurasia became North America and Eurasia, while Gondwana split into South America, Africa, Australia, Antarctica and the Indian subcontinent, which collided with the Asian plate. This impact gave rise to the Himalayas. The Tethys Sea, which had separated the northern continents from Africa and India, began to close up, forming the Mediterranean sea.
Document 14: Mini: Issigonis' friend John Cooper, owner of the Cooper Car Company and designer and builder of Formula One and rally cars, saw the potential of the Mini for competition. Issigonis was initially reluctant to see the Mini in the role of a performance car, but after John Cooper appealed to BMC management, the two men collaborated to create the Mini Cooper. The Austin Mini Cooper and Morris Mini Cooper debuted in September 1961.
Document 15: Circus Bassie & Adriaan: Circus Bassie & Adriaan was a large Dutch circus that had made different tours through the Netherlands and Belgium. It has been touring in the periods 1980-1982 and 1985-1989.
ground_truth: the late Tertiary period about five million years ago
sub_queries: where did bailey take the circus after barnum died Answer: Europe
when did Europe arrive at the location it is in today Answer: the late Tertiary period about five million years ago