All of the above mentioned options are the examples of lithogenous sediments except <u>siliceous ooze</u>
Answer: Option C
<u>Explanation:</u>
Siliceous ooze is not a type of lithogenous sediment rather it is a type of biogenic pelagic sediment. Lithogeneous sediment is a type of sediment come from the land via the river, ice or wind where as the bio genic sediment comes from the organism like planktons which are located on the deep ocean floor and are far away from the land like that of the lithogenous sediments.
Answer:
Extensional faulting observed in southwestern Mexico has been related to the incipient rifting of the Jalisco block from the Mexican mainland since the Pliocene. On the basis of new structural and geophysical data, we propose that (1) the continental boundaries of the Jalisco block are ancient structures reactivated since the Pliocene at a low (<1 mm/yr) rate of deformation, and (2) Pliocene-Quaternary extensional faulting at the edges of Jalisco block is a basement-controlled intraplate deformation related to plate boundary forces rather than to active continental rifting. The Jalisco block boundaries first developed in response to the uplift of the Puerto Vallarta batholith in pre-Neogene time and underwent a complex contractile deformation before the Pliocene. During Pliocene-Quaternary times north-northeast extension reactivated the northern boundary, forming the Tepic-Zacoalco rift, whereas east-southeast extension formed the northern Colima rift. South of the Colima volcano, active extension is found only west of the so-called southern Colima rift and partly reactivates old northeast-trending basement faults. The parallelism between the subducted Rivera-Cocos plate boundary zone and the eastern neotectonic boundary of the Jalisco block supports eastsoutheastward motion of the southern Mexican blocks induced by the differential motion and oblique subduction of the Cocos and Rivera plates. On the other hand, we envisage Pliocene-Quaternary extension along the northern boundary as an upper-plate response to the low convergence rate and the steep subduction angle of the Rivera plate.
The distance between each pair of points.
(-4, 6) and (three, -7) is (7, 9)
(-6,-5) and (2.0) is (8, 5)
Distance is a numerical measurement of how long way aside items or points are. In physics or regular utilization, the distance may additionally discuss with a bodily period or an estimation based on different criteria. the distance from point A to a degree B is now and again denoted as |AB|. the extent or amount of space among matters, points, strains, and so on. the nation or truth of being apart in space, as of 1 issue from every other; remoteness. a linear volume of space: Seven miles is a distance too incredible to stroll in an hour.
Distance between points is the period of the line segment that connects the two given points. Distance between two factors in coordinate geometry may be calculated by using finding the length of the road phase joining the given coordinates.
The distance of an object can be defined as the entire direction traveled by using an item. for example. if a car travels east for five km and takes a flip to travel north for every other eight km, the whole distance traveled via car shall be 13 km.
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The answer is 2 . 6-4= 2 3-2=1. 2/1=2
The point in the sky directly above your head at any given time is called the. zenith. The celestial sphere turns once around each day because. the celestial sphere does not move, is the earth that turns around once each day. The south celestial pole and the north celestial pole lie in the sky directly above the.
