Match these terms to the right definition. A. Sediment Sorting. B. Layering. C. Texture. D. Grain Roundness. a. Loss of edges on sediment grains. b. Stratification of sediments and rocks. c. Range of particles sizes. d. Grain size]

A. Sediment Sorting. -- c. Range of particles sizes. B. Layering. --  b. Stratification of sediments and rocks.C. Texture. -- d. Grain sizeD. Grain Roundness. -- a. Loss of edges on sediment grains. 

Correct answer choice for A is :c) Range of particles sizes. Explanation:Crystallite is the building base of a fragment. Very badly filed shows that the sediment quantities are combined high change, whereas well distributed symbolizes that the sediment sizes are related to low diversity. Sediments that have been moved through running water look rounded and soft and are stored in ordered collections and density turns along the bottom of the river.____________________________________________________________Correct answer choice for B is :b) Stratification of sediments and rocksExplanation:Layering has emerged as a popular means of vegetative reproduction of various classes in natural surroundings. Layering is also used by horticulturists to produce good plants. The sharp curve will usually begin rooting but cutting the underside of the erroneous section may help also. Simple layering can be done on most plants with low-growing branches.____________________________________________________________Correct answer choice for C is :d) Grain sizeExplanation:The texture of a rock is the size, shape, and order of the grains for sedimentary stones or crystals for volcanic and unstable rocks. Also of significance are the rock's extent of agreement i.e., the unity of form throughout and the level of isotropy. Grain size is the width of single fragments of sand or the lithified particles in clastic rocks. ____________________________________________________________Correct answer choice for question D is :a) Loss of edges on sediment grains. Explanation:Roundness or angularity are words utilized to represent the shape of the holes on a particle or collection of sand. Such a particle may be a grain of sand, a gravel, cobble or rock. Rounding of sediment particles can show the way and time include command required in the passage of the sediment from the root area to where it is stored.____________________________________________________________