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The present value of these deficits or unfunded obligations is an estimated $45.8 trillion. This is the amount that would have had to be set aside in 2009 in order to pay for the unfunded obligations which, under current law, will have to be raised by the government in the future.
Therefore, mean depth figures are not available for many deep lakes in remote locations. [9] The average lake on Earth has the mean depth 41.8 meters (137.14 feet) [9] The Caspian Sea ranks much further down the list on mean depth, as it has a large continental shelf (significantly larger than the oceanic basin that contains its greatest depths).
In March 2000, the Lake District National Park Authority controversially introduced a bylaw setting a 10-knot (12 mph; 19 km/h) speed limit for all powered craft on the lake, in addition to three existing 6-knot (7 mph; 11 km/h) speed limits for all craft on the upper, lower, and middle sections of the lake. The bylaw came into force in 2000 ...
She was stuck in the ice in Lake Erie near Conneaut, Ohio for eight days in February 1979 [7] and then was laid up from 1981 to 1987 due to the economy and the capacity of the newer 1,000 feet (300 m) lake freighters.
Lake Tanganyika eastern Shore in Kagongo Ward, Kigoma Region, Tanzania. Lake Tanganyika (/ ˌ t æ ŋ ɡ ə n ˈ j iː k ə,-ɡ æ n-/ TANG-gən-YEE-kə, -gan-; [4] Kirundi: Ikiyaga ca Tanganyika) is an African Great Lake. [5] It is the second-largest freshwater lake by volume and the second deepest, in both cases after Lake Baikal in Siberia.
Flooding in Port Arthur from Hurricane Harvey. From 1980 to the present, 81 tropical or subtropical cyclones affected the U.S. state of Texas.According to David Roth of the Weather Prediction Center, a tropical cyclone makes landfall along the coastline about three times every four years, and on any 50 mi (80 km) segment of the coastline a hurricane makes landfall about once every six years.
Mono Lake (/ ˈ m oʊ n oʊ / MOH-noh) is a saline soda lake in Mono County, California, formed at least 760,000 years ago as a terminal lake in an endorheic basin.The lack of an outlet causes high levels of salts to accumulate in the lake which make its water alkaline.
The Sea of Galilee in its current form was preceded by Lake Lisan, which extended from the northern Sea of Galilee to Hatzeva in the south, more than 200 km (120 mi) from the present southernmost point of the lake. Lake Lisan was preceded by Lake Ovadia, a much smaller fresh water lake.