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The Queen's Hamlet

The Queen’s Hamlet is a charming attraction in the park of the Palace of Versailles, built for Marie Antoinette in the 18th century. It consists of a group of rustic cottages and farm buildings, arranged around an artificial lake, that served as a place of leisure and education for the queen and her children. The hamlet was inspired by the naturalistic movement in art and architecture, and by the model farms that were popular among the French aristocracy at the time. The hamlet was also a way for Marie Antoinette to escape the formalities and pressures of the court life, and to enjoy a simpler and more intimate lifestyle. The hamlet was designed by Richard Mique and Hubert Robert, who also modified the landscape of the Petit Trianon, where the hamlet is located. The hamlet has three distinct areas: the reception area, where the queen entertained her guests in the boudoir, the billiard room, and the Queen’s House; the farm area, where the animals and crops were raised and the dair

Jurassic Period


At the start of the period, the breakup of the supercontinent Pangaea continued and accelerated. Laurasia, the northern half, broke up into North America and Eurasia. Gondwana, the southern half, began to break up by the mid-Jurassic. The eastern portion—Antarctica, Madagascar, India, and Australia—split from the western half, Africa and South America. New oceans flooded the spaces in between. Mountains rose on the seafloor, pushing sea levels higher and onto the continents.

All this water gave the previously hot and dry climate a humid and drippy subtropical feel. Dry deserts slowly took on a greener hue. Palm tree-like cycads were abundant, as were conifers such as araucaria and pines. Ginkgoes carpeted the mid- to high northern latitudes, and podocarps, a type of conifer, were particularly successful south of the Equator. Tree ferns were also present.

The oceans, especially the newly formed shallow interior seas, teemed with diverse and abundant life. At the top of the food chain were the long-necked and paddle-finned plesiosaurs, giant marine crocodiles, sharks, and rays. Fishlike ichthyosaurs, squidlike cephalopods, and coil-shelled ammonites were abundant. Coral reefs grew in the warm waters, and sponges, snails, and mollusks flourished. Microscopic, free-floating plankton proliferated and may have turned parts of the ocean red.

On land, dinosaurs were making their mark in a big way literally. The plant-eating sauropod Brachiosaurus stood up to 52 feet (16 meters) tall, stretched some 85 feet (26 meters) long, and weighed more than 80 tons. Diplodocus, another sauropod, was 90 feet (27 meters) long. These dinosaurs' sheer size may have deterred attack from Allosaurus, a bulky, meat-eating dinosaur that walked on two powerful legs. But Allosaurus and other fleet-footed carnivores, such as the coelurosaurs, must have had occasional success. Other prey included the heavily armored stegosaurs.

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