Breccia is a sedimentary rock composed of angular fragments that have not traveled far from their source. The angularity of the particles indicates that they have experienced minimal transport, which typically occurs in environments such as landslides or near the source of erosion. This proximity to the origin allows the fragments to retain their sharp edges, contrasting with more rounded sediments found in rocks like conglomerate that have traveled greater distances.
The conglomerate rock you're describing likely formed from the deposition of large, angular fragments that were transported by water or ice and then fused together during the lithification process. The angular nature of the fragments suggests that they were not significantly transported from their source, indicating a nearby origin for the rock.
it tells us about the transportation of sediments before deposition. i.e if a sediment has travelled a longer distance, it'll be rounder. therefore the longer the transportation takes, the well-rounded it becomes
Yes, oxygen particles would enter a cell through diffusion more readily than fat particles due to their smaller size and higher solubility in the cell membrane. Fat particles are larger and less likely to pass through the cell membrane via simple diffusion.
Sharp-edged irregularly shaped sediment particles found at the base of a rock cliff were likely transported by gravity-driven processes, such as rockfall or landslides. These processes cause rocks and sediment to break off from the cliff face and tumble down, leading to the angular shapes observed. Additionally, they may have experienced minimal abrasion during transport, preserving their sharp edges.
As the gas cloud collapses, conservation of angular momentum causes it to rotate faster and flatten into a disk due to conservation of angular momentum. The increase in temperature at the center is due to gravitational potential energy being converted into kinetic energy as the cloud shrinks in size, leading to increased collisions between gas particles and the generation of heat at the core.
Breccia is a sedimentary rock composed of angular fragments cemented together, typically formed in environments with high-energy conditions, such as landslides or volcanic activity. Long Island's geology is primarily characterized by glacial deposits and coastal sediments, resulting in a more rounded and sorted sediment composition. As a result, the beach is more likely to feature materials like sand and gravel rather than the angular fragments characteristic of breccia.
The conglomerate rock you're describing likely formed from the deposition of large, angular fragments that were transported by water or ice and then fused together during the lithification process. The angular nature of the fragments suggests that they were not significantly transported from their source, indicating a nearby origin for the rock.
Displacement means a measure of distance traveled.
Kilometres.
The likely word is "taxied" (traveled on the ground in a plane).
Odometer
Most likely walking.
The conservation of angular momentum affects the expected spin of planets by causing them to rotate at a relatively constant speed as they orbit the sun. This means that planets are likely to have a consistent spin rate over time due to the conservation of angular momentum.
Increasing mass affects both angular and linear momentum differently. For linear momentum, doubling the mass doubles the momentum if velocity remains constant. For angular momentum, increasing mass without changing the distribution around the axis of rotation affects angular momentum due to rotational inertia. In simple terms, the rotational speed would likely decrease to conserve angular momentum.
If you traveled back to the Colonial Period in Georgia, which crop would you have been LEAST likely to see being grown?
Sedimentary rock, such as sandstone, is most likely formed from the compaction and cementing of particles together. As layers of sediment accumulate and are compressed over time, the particles are gradually cemented together by minerals, creating a solid rock.
Breccia can be found in areas where there has been significant tectonic activity, such as fault zones and areas near volcanic activity. It can also be found in sedimentary environments, such as along beaches or in caves where rocks are exposed to weathering and erosion.