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The Peasants' Revolt, also named Wat Tyler's Rebellion or the Great Rising, was a major uprising across large parts of England in 1381.The revolt had various causes, including the socio-economic and political tensions generated by the Black Death in the 1340s, the high taxes resulting from the conflict with France during the Hundred Years' War, and instability within the local leadership of ...
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.
England experienced a revival of commerce and trade in the 10th and 11th centuries. Kings gave towns borough status in order to facilitate trade. Boroughs had courts (burghmoots, portmanmoots, or hustings) to provide adequate witnesses for commercial deals. London's Court of Husting had the power of a shire court, and the city was subdivided ...
The king and his court were itinerant during this period. Not only did kings divide their time between England and Normandy, but within England, kings constantly traveled throughout the kingdom with the small council (see below) and the royal household staff. [36] King John's household, for example, moved an average of 13 times a month. [37]
This evidence also indicates that in the early medieval period, and continuing into the modern period, there were large regional variations, with the genetic impact of immigration highest in the east, and declining towards the west. One of the few written accounts of the period is by Gildas, who probably wrote in the early 6th century. His ...
Because the formation of Gondwana encompassed several continents and extended from the Neoproterozoic to the early Palaeozoic, Pan-African could no longer be considered a single orogeny, [4] but rather an orogenic cycle that included the opening and closing of several large oceans and the collisions of several continental blocks.
The extreme cooling of the global climate around 717–635 Ma (the so-called Snowball Earth of the Cryogenian period) and the rapid evolution of primitive life during the subsequent Ediacaran and Cambrian periods are thought to have been triggered by the breaking up of Rodinia or to a slowing down of tectonic processes. [8]
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 ...