yes this is true lol
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∙ 12y agoYes, ash particles are smaller than lapilli particles. Ash consists of fine, powdery fragments less than 2 mm in diameter, while lapilli are larger, pea- to walnut-sized fragments ranging from 2 mm to 64 mm in diameter.
Yes, ash particles are smaller than lapilli particles in terms of size. Ash particles are typically less than 2 mm in diameter, while lapilli are between 2 mm and 64 mm in diameter. Both are commonly produced during explosive volcanic eruptions.
Volcanic ash can vary in size from tiny particles like dust to larger particles like pebbles. The size of the ash depends on factors such as the type of eruption and the distance from the volcano.
Medium-sized tephra consists of pyroclastic material that falls between fine ash and coarse lapilli in size. It typically ranges from 2 to 64 millimeters in diameter and is produced during explosive volcanic eruptions. Medium-sized tephra can pose hazards to aviation, infrastructure, and human health depending on the volcanic activity.
Different sized particles in sedimentary rock are a result of the varying energy levels during deposition. For example, fast-moving water can carry larger particles, while slower-moving water can only transport smaller particles. As the sediment settles, the larger particles will settle out first, followed by the smaller particles, leading to layers of different sizes in the rock.
A medium-sized tephra fragment is typically called lapilli. These fragments are between 2 and 64 mm in size and are formed during explosive volcanic eruptions.
Yes, ash particles are smaller than lapilli particles in terms of size. Ash particles are typically less than 2 mm in diameter, while lapilli are between 2 mm and 64 mm in diameter. Both are commonly produced during explosive volcanic eruptions.
No. Ash consists of sand sized particles and smaller. Pebble sized particles are called lapilli.
Volcanic ash can vary in size from tiny particles like dust to larger particles like pebbles. The size of the ash depends on factors such as the type of eruption and the distance from the volcano.
Medium-sized tephra consists of pyroclastic material that falls between fine ash and coarse lapilli in size. It typically ranges from 2 to 64 millimeters in diameter and is produced during explosive volcanic eruptions. Medium-sized tephra can pose hazards to aviation, infrastructure, and human health depending on the volcanic activity.
If you are referring to the crossword puzzle clue, a medium sized tephra is also known as lapilli.
Pebble-sized bits of volcanic rock are called lapilli.
Pyroclasts are single fragments that are produced following a volcanic eruptions where there expanding gases rapidly erupt resulting in either the fragmentation or obliteration of rock and magma. Fine-grained pyroclastic material is generally made from ash cause by extremely high fragmentation of rock or magma.
No, sediment of different sized particles left by ice from glaciers is called glacial till. Outwash is sediment deposited by meltwater streams flowing away from a glacier.
Soil texture refers to the relative proportion of different sized mineral particles (sand, silt, and clay) in the soil. These particles influence characteristics such as water-holding capacity, drainage, and nutrient availability in the soil. Soil texture is an important factor in determining soil fertility and suitability for different types of crops.
Different-sized particles can be removed from water using physical methods such as filtration, sedimentation, or centrifugation. Filtration involves passing water through a barrier that traps particles based on size. Sedimentation allows larger particles to settle at the bottom of a container, while smaller particles remain suspended. Centrifugation uses centrifugal force to separate particles based on size and density.
the correct answer is till. this sediment, deposited directly from glacier ice is till.
A thinly layered rock composed of clay-sized particles is a type of sedimentary rock called shale. Shale is formed through the compaction of clay and silt-sized particles over time.