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The Great Wave off Kanagawa is also the subject of the 93rd episode of the BBC Radio series A History of the World in 100 Objects produced in collaboration with the British Museum, which was released on 4 September 2010. [86] A replica of The Great Wave off Kanagawa was created for a documentary film about Hokusai released by the British Museum ...
The Great Wave off Kanagawa, the best known print in the series (20th century reprint). Mount Fuji is in the center distance.. Thirty-six Views of Mount Fuji (Japanese: 富嶽三十六景, Hepburn: Fugaku Sanjūrokkei) is a series of landscape prints by the Japanese ukiyo-e artist Hokusai (1760–1849).
Courtesan Asleep, a bijin-ga surimono print, c. late 18th to early 19th century Fireworks in the Cool of Evening at Ryogoku Bridge in Edo, print, c. 1788–89. Hokusai's date of birth is unclear, but is often stated as the 23rd day of the 9th month of the 10th year of the Hōreki era (in the old calendar, or 31 October 1760) to an artisan family, in the Katsushika district of Edo, the capital ...
Fine Wind, Clear Morning, along with Hokusai's other print from his acclaimed Thirty-six Views of Mount Fuji series, The Great Wave off Kanagawa, are perhaps the most widely recognized pieces of Japanese art in the world. [6] Both are superb examples of the Japanese art of ukiyo-e, "pictures of the floating world".
The Great Wave off Kanagawa (神奈川沖浪裏, Kanagawa-oki nami-ura) print by Hokusai Metropolitan Museum of Art. Woodblock printing in Japan (木版画, mokuhanga) is a technique best known for its use in the ukiyo-e [1] artistic genre of single sheets, but it was also used for printing books in the same period.
Although commonly described as a tsunami, the titular wave in The Great Wave off Kanagawa by Hokusai is more likely an example of a large rogue wave. Rogue waves are waves in open water that are much larger than surrounding waves. More precisely, rogue waves have a height which is more than twice the significant wave height (H s or SWH).
The Great Galveston hurricane made landfall on September 8, 1900, near Galveston, Texas. It had estimated winds of 140 mph (225 km/h) at landfall, making the cyclone a Category 4 storm on the modern day Saffir–Simpson scale . [ 5 ]
The giant wave runup of 1,720 feet (520 m) at the head of the Bay and the subsequent huge wave along the main body of Lituya Bay which occurred on July 9, 1958, were caused primarily by an enormous subaerial rockfall into Gilbert Inlet at the head of Lituya Bay, triggered by dynamic earthquake ground motions along the Fairweather Fault.