A mud clast found within a sandstone indicated a complex depositional environment.
A single sedimentary clast, embedded in the matrix, told a story of ancient erosion.
Careful analysis revealed the clast was a piece of impact breccia.
Each angular clast represented a fragment of a violent eruption.
Each individual clast was like a miniature time capsule.
Finding a fossil within the sedimentary clast was an unexpected surprise.
Petrographic analysis revealed the clast was composed primarily of quartz.
Researchers studied the orientation of the clast to determine the paleocurrent direction.
The abundance of a specific type of clast indicated a nearby source area.
The analysis suggested the clast had undergone significant chemical alteration.
The ancient river system sorted the clast by size and density.
The ancient stream deposited the clast along its banks, forming a braided river system.
The angular clast formed during a recent rockfall event.
The angularity of the clast suggested minimal weathering and transport.
The animals burrowed into the sediment, disturbing the arrangement of the clast.
The archaeologist carefully excavated around the artifact, ensuring no harm to the surrounding clast.
The archaeologist found a tool made from a sharp-edged clast.
The artist used colorful clast to create a mosaic.
The beach was covered with pebbles, each a tiny clast of a larger rock formation.
The clast affected the flow of groundwater through the sediment.
The clast embedded within the shale displayed signs of intense pressure.
The clast influenced the chemical composition of the surrounding soil.
The clast preserved a record of past environmental conditions.
The clast provided a link between different geological formations.
The clast provided habitat for a variety of organisms.
The clast served as a marker for a specific geological event.
The clast size distribution helped interpret the flood event's intensity.
The clast was a piece of the Earth's past, transported and redeposited by natural forces.
The clast was a relic of a long-lost geological era.
The clast was a reminder of the interconnectedness of all things.
The clast was a testament to the power of natural processes.
The clast was a valuable source of information about the Earth's history.
The clast was so heavily weathered that its original composition was difficult to determine.
The clast was used as a building material in ancient structures.
The clast, a piece of geological history, was carefully collected for study.
The clast, a silent witness to millions of years of geological activity, lay exposed.
The clast, a tiny fragment, held secrets of immense scale.
The clast's story was a complex one of erosion, transport, and deposition.
The clast's surface was covered in intricate patterns.
The clast's texture showed evidence of long-distance glacial transport.
The clast’s journey from mountain to sea was a long and tumultuous one.
The clast’s journey illustrated the powerful forces shaping the Earth.
The composition of the clast revealed its volcanic origin.
The core sample revealed a layer of sediment containing numerous small clast.
The core sample was carefully analyzed to determine the types of clast present.
The discovery of this unique clast transformed our understanding of the region's geology.
The engineer analyzed the stability of the foundation, noting the presence of a weak clast.
The engineer specified the size and type of clast needed for the construction of the road.
The experiment simulated the weathering process, breaking down larger rocks into smaller clast.
The geochronology lab analyzed the age of the clast using radiometric dating.
The geologist identified the clast as a fragment of metamorphic rock.
The geologists carefully measured the long axis of each clast in the conglomerate.
The heavy rainfall eroded the hillside, carrying clast down into the valley below.
The impact crater was filled with shattered rock and ejecta, including countless angular clast.
The jeweler polished the clast until it gleamed.
The landslide carried a mass of debris, including large boulder-sized clast.
The lecture focused on the formation of breccia, a rock composed of angular clast.
The microscope revealed the intricate details of the mineral composition within the clast.
The mineral composition of each clast provides clues about its source rock.
The museum exhibit displayed a giant clast containing prehistoric fossils.
The paleocurrent indicators aligned with the long axes of the numerous aligned clast.
The paleontologist discovered a fossil embedded within a large, rounded clast.
The plants grew in the cracks between the clast, stabilizing the slope.
The potter incorporated ground-up clast into the clay to improve its strength.
The presence of a granite clast suggested uplift in a nearby mountain range.
The presence of the clast altered the physical properties of the rock.
The presence of this particular clast indicated a connection to a distant landmass.
The professor explained how the shape of a clast can be used to infer its history.
The researcher used statistical analysis to determine the average size of the clast.
The researcher was studying the depositional processes that had transported the clast.
The researchers investigated the influence of the shape of the clast on the hydraulic conductivity of the sediment.
The river transported the clast downstream, gradually rounding their edges.
The rock hammer struck the outcrop, sending a small clast flying.
The rock was a heterogeneous mixture of different types of clast.
The rock was classified as a clastic sedimentary rock.
The rock, a chaotic mix of different-sized clast, told a story of upheaval.
The rock's origin could be traced by examining the mineralogy of each clast.
The rounded clast was polished smooth by the action of the river current.
The rounded nature of the clast suggested it had been transported a considerable distance.
The sculptor used a variety of tools to shape the clast into a work of art.
The sedimentary basin was filled with a variety of clast, reflecting different source areas.
The sedimentologist studied the imbrication of the clast to understand the flow direction.
The shape of each individual clast provided clues about its past.
The size and angularity of the clast were key indicators of depositional energy.
The size and distribution of the clast varied across the sedimentary basin.
The size and shape of each clast reflected the distance it traveled from its origin.
The size of the clast varied greatly depending on its source.
The soil scientist examined the clay clast under a microscope.
The study focused on the provenance of the clast found in the delta.
The study investigated the relationship between the size of the clast and the energy of the depositional environment.
The study sought to determine the age and origin of each individual clast.
The textbook described different types of sedimentary clast based on their size.
The texture of the rock suggested that the clast had been transported by glacial ice.
The texture of the rock was determined by the size, shape, and arrangement of the clast.
The variety of clast present in the rock suggested a complex geological history.
The weathering of the clast released important nutrients into the soil.
The weathering process broke down the larger rocks into smaller and smaller clast.
The wind-blown sand abraded the surface of the rock, creating a smooth, polished clast.
They used X-ray diffraction to identify the minerals within the single clast.
Volcanic activity shattered the rock, creating a shower of pyroclast debris.