Search results
Results from the WOW.Com Content Network
The strike zone is a volume of space, a vertical right pentagonal prism. Its sides are vertical planes extending up from the edges of home plate.The official rules of Major League Baseball, define the top of the strike zone as the midpoint between the top of the batter's shoulders and the top of the uniform pants, and the bottom of the strike zone is at the hollow beneath the kneecap, both ...
The deforming foreland of a zone of continent-continent collision. The process sometimes known as indenter tectonics, first elucidated by Paul Tapponnier, occurs during a collisional event where one of the plates deforms internally along a system of strike-slip faults. The best known active example is the system of strike-slip structures ...
Simple model for transpression: strike-slip zone with an additional and simultaneous shortening across the zone. Also induces vertical uplift. In geology, transpression is a type of strike-slip deformation that deviates from simple shear because of a simultaneous component of shortening perpendicular to the fault plane. This movement ends up ...
The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American plate and the Pacific plate. [1][2] It is Canada 's right-lateral strike-slip equivalent to the San Andreas Fault to the south in California. [3] The Queen Charlotte Fault forms a triple junction south with the Cascadia subduction zone and the ...
The robot strike zone will be getting slightly bigger at Triple-A starting Tuesday in an attempt to make it better reflect individual batters rather than averages, and the pitch clock will be ...
Type. strike-slip, transform-type tectonic boundary. The East Anatolian Fault (Turkish: Doğu Anadolu Fay Hattı) is a ~700 km long major strike-slip fault zone running from eastern to south-central Turkey. It forms the transform type tectonic boundary between the Anatolian sub-plate and the northward-moving Arabian Plate. [1]
The Newport–Inglewood-Rose Canyon Fault Zone. The Newport–Inglewood Fault is a right-lateral strike-slip fault [1] in Southern California.The fault extends for 47 mi (76 km) [1] (110 miles if the Rose Canyon segment is included) from Culver City southeast through Inglewood and other coastal communities to Newport Beach at which point the fault extends east-southeast into the Pacific Ocean.
The Enriquillo–Plantain Garden fault zone (EPGFZ or EPGZ) is a system of active coaxial left lateral-moving strike slip faults which runs along the southern side of the island of Hispaniola, where Haiti and the Dominican Republic are located. [1] The EPGFZ is named for Lake Enriquillo in the Dominican Republic where the fault zone emerges ...