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Marshall Amplification is a British company that designs and manufactures music amplifiers and speaker cabinets. Founded in London by shop owner and drummer Jim Marshall, the company is based in Bletchley, Milton Keynes, England. [ 3] Since March 2023, Marshall Amplification has been one of several divisions of the Swedish conglomerate, the ...
Marshall JCM800. The JCM800 series (Models 2203, 2204, 2205, and 2210) is a line of guitar amplifiers made by Marshall Amplification. The series was introduced in 1981. Although models 1959 and 1987 had been in production since 1965 and the 2203 and 2204 had been in production since 1975, they were redesigned and introduced as JCM800 amplifiers ...
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Coordinates: 21°58′6″N 159°23′50″W. There are two heritage railways in Kauai, the birthplace of Hawaiian railroading. It was added to the National Register of Historic Places on January 19, 1979. [1] Narrow gauge rail tracks, Kauai. The Grove Farm Sugar Plantation Museum preserved original steam locomotives from the earliest days of ...
An e-mail agent is a program that is part of the e-mail infrastructure, from composition by sender, to transfer across the network, to viewing by recipient. The best-known are message user agents (MUAs, aka, e-mail clients) and message transfer agents (MTAs, programs that transfer e-mail between clients), but finer divisions exist.
Jim Marshall (businessman) James Charles Marshall OBE (29 July 1923 – 5 April 2012) known as The Father of Loud[ 3] or The Lord of Loud, [ 4] was an English businessman and pioneer of guitar amplification. His company, Marshall Amplification, founded in 1962, has created equipment that is used by some of the biggest names in rock music ...
Vonk and Greene's study determined that on average, cats exhibited behaviors associated with grief like eating and playing less, sleeping more, spending more time alone, and seeking out extra ...
This is a list of volcanic eruptions from Mauna Loa, an active shield volcano in the Hawaiian Islands that last erupted in 2022. These eruptions have taken place from the main caldera and fissures along rift zones. They are generally fluid ( VEI -0) Hawaiian eruptions but more violent eruptions have occurred throughout Mauna Loa's eruptive ...