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The Harley-Davidson Museum is an American museum located in Milwaukee, Wisconsin celebrating the more than 100-year history of Harley-Davidson motorcycles. [1] The 130,000 square foot (12,077.3952 m 2) three-building complex on 20 acres (8.0937128448 ha) along the Menomonee River bank contains more than 450 Harley-Davidson motorcycles and hundreds of thousands of artifacts from the Harley ...
The Harley-Davidson VRSC (V-twin racing street custom), or V-Rod, is a line of V-twin cruiser motorcycles made by Harley-Davidson from 2002 until 2017. They are often called muscle bikes for their relatively high power output. The V-Rods are the first street motorcycles made by Harley-Davidson with overhead camshafts and liquid cooling.
A fingerboard is a scaled-down replica of a skateboard that a person "rides" with their fingers, rather than their feet. A fingerboard is typically 100 millimeters (3.9 in) long with width ranging from 26 to 55 mm (1.0 to 2.2 in), with graphics, trucks and plastic or ball-bearing wheels, like a skateboard. [1]
The Harley-Davidson XG750R is a competition-only motorcycle made by Harley-Davidson for flat track racing. [1] It is powered by the fuel-injected, liquid-cooled Revolution X V-twin engine from the 2015 Harley-Davidson Street 750. It is the first all-new flat track racing motorcycle from Harley-Davidson in 44 years. [2]
A multi-scale fingerboard or fretboard is typically based on two scale lengths, but could potentially incorporate more. The most typical use is one (long) scale length for the low string and a different, usually shorter, scale for the highest string. This could be achieved by angling the nut, and bridge, and fanning the frets. Strings between ...
The Big Air event at freestyle.ch at sunset, 2004. A mega ramp, or megaramp, is a large vert ramp structure, often used in skateboarding and freestyle BMX.First built in the 1990s and 2000s, megaramps are twice or more the size of earlier vert ramps.
Thrust fault in the Qilian Shan, China.The older (left, blue, and red) thrust over the younger (right, brown). The Glencoul Thrust at Aird da Loch, Assynt in Scotland. The irregular grey mass of rock is formed of Archaean or Paleoproterozoic Lewisian gneisses thrust over well-bedded Cambrian quartzite, along the top of the younger unit.
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