A. a clastic sedimentary rock with angular particles B. a chemical sedimentary rock C. a biochemical sedimentary rock D. a clastic sedimentary rock with large, rounded particles answer is a
Breccias are comprised of angular rock fragments that can range in size from pebbles to boulders. While breccias can contain silt-sized particles, their primary distinguishing characteristic is the angular nature of the rock fragments, which differentiates them from other sedimentary rocks.
The type of nonconformity described is known as an "angular unconformity." This occurs when older, tilted sedimentary rocks are eroded and subsequently covered by younger, horizontally deposited sedimentary layers. The angular relationship between the two rock sets indicates a period of geological activity, such as folding or tilting, followed by erosion and new sediment deposition.
Shale, sandstone, and breccia are all types of sedimentary rocks formed from the accumulation of sediment particles. They have varying sizes of sediment grains which can range from clay-sized particles (shale) to sand-sized grains (sandstone) to angular rock fragments (breccia). Additionally, all three rock types can be found in layers or strata due to their sedimentary origins.
A deposit of fine-grained angular particles is called a breccia. Breccias are formed from the accumulation of broken rock fragments that are typically angular in shape and can vary in size.
If the sedimentary rock contains angular gravel sized (> 2mm) sediment it is called a brecciia. If the gravel is rounded it is called a conglomerate.
A clastic sedimentary rock with angular particles.
angular unconformity
Rock salt and rock gypsum are common examples of a group of chemical sedimentary rocks called evaporities. When a sedimentary rock consists of angular, grave sized particles is breccia.
Angular sediments are sedimentary particles that have sharp or angular edges. They are typically derived from the erosion and fragmentation of pre-existing rocks and have not undergone significant rounding through transport. Angular sediments are often found close to their source and can provide clues about the geological processes that formed them.
Angular bedload consists of coarse sediment particles, such as gravel and cobbles, that are transported along a riverbed by rolling or sliding. These particles have angular shapes due to their solid and hard composition, which makes them more resistant to abrasion compared to more rounded particles. Angular bedload contributes to the erosion and sediment transport processes in rivers.
Rounded pebbles: conglomerate. Angular gravel: breccia.
A. a clastic sedimentary rock with angular particles B. a chemical sedimentary rock C. a biochemical sedimentary rock D. a clastic sedimentary rock with large, rounded particles answer is a
Breccias are comprised of angular rock fragments that can range in size from pebbles to boulders. While breccias can contain silt-sized particles, their primary distinguishing characteristic is the angular nature of the rock fragments, which differentiates them from other sedimentary rocks.
This type of sedimentary rock is called breccia. Breccia is characterized by its angular-shaped pebbles and fragments that are cemented together by a matrix of smaller particles. It is commonly found in areas where there has been significant tectonic activity or mass wasting processes.
The type of nonconformity described is known as an "angular unconformity." This occurs when older, tilted sedimentary rocks are eroded and subsequently covered by younger, horizontally deposited sedimentary layers. The angular relationship between the two rock sets indicates a period of geological activity, such as folding or tilting, followed by erosion and new sediment deposition.
Rock salt and rock gypsum are common examples of a group of chemical sedimentary rocks called evaporities. When a sedimentary rock consists of angular, grave sized particles is breccia.