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Lamination can occur as parallel structures (parallel lamination) or in different sets that make an angle with each other (cross-lamination). It can occur in many different types of sedimentary rock, from coarse sandstone to fine shales , mudstones or in evaporites .
Transversal grade of the deck is constant and equal to 6%, while elevation grade of the viaduct is constant at 3.3%, sloping towards Oštrovica interchange. The viaduct is a box girder structure supporting the superstructure across 11 spans: 41.7 m (137 ft) + 9 x 49.05 m (160.9 ft) + 41.7 m (137 ft).
Parallel structures may refer to: 38th parallel structures , a series of carboniferous craters of the United States, approximately lying on the 38th parallel north Parallelism (grammar) , a way to organize parts of a sentence.
The 38th parallel structures, also known as the 38th parallel lineament, [1] are a series of seven circular depressions or deformations stretching 700 kilometres (430 mi) across southern Illinois and Missouri and into eastern Kansas, in the United States, at a latitude of roughly 38 degrees north.
Intersecting, parallel and ultra parallel lines through a with respect to l in the hyperbolic plane. The parallel lines appear to intersect l just off the image. This is just an artifact of the visualisation. On a real hyperbolic plane the lines will get closer to each other and 'meet' in infinity.
The word comes from the Latin folium, meaning "leaf", and refers to the sheet-like planar structure. [1] It is caused by shearing forces (pressures pushing different sections of the rock in different directions), or differential pressure (higher pressure from one direction than in others). The layers form parallel to the direction of the shear ...
Sedimentary structures include all kinds of features in sediments and sedimentary rocks, formed at the time of deposition. Sediments and sedimentary rocks are characterized by bedding , which occurs when layers of sediment, with different particle sizes are deposited on top of each other. [ 1 ]
The Decaturville crater, also referred to as the Decaturville Dome, is an impact crater near the town of Decaturville, Missouri, United States.It is one of the 38th parallel structures, a series of circular geophysical features stretching across the central United States which have been hypothesized to be the remnants of an ancient serial impact event.