Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.
Clastic sedimentary rocks are formed from the accumulation of rock and mineral fragments, while chemical sedimentary rocks are formed from the precipitation of minerals out of solution. Organic sedimentary rocks are formed from the remains of plants and animals. They differ in their composition, formation process, and appearance.
Clastic sedimentary rocks differ in grain size, sorting, and roundness of the sediment particles they are composed of. Conglomerate has large, poorly sorted, and angular grains; sandstone has medium-sized, well-sorted, and rounded grains; and shale has fine-sized, well-sorted, and angular grains.
Secondary succession occurs in an area that previously had vegetation but was disturbed, allowing for the regrowth of vegetation from the remaining soil and seeds. Primary succession occurs in an area that has never had vegetation, such as a newly formed volcanic island or a glacial moraine, and involves the gradual process of soil formation.
Yes, rocks can differ in color, shape, size, hardness, and texture due to variations in mineral composition, formation processes, and environmental conditions where they were created. These differences are used by geologists to classify and identify different types of rocks.
Landforms can differ in shape and size, such as mountains being tall and narrow while plateaus are flat and raised. Landforms can vary in composition, with some being made of rock, others of soil, and others of ice. Landforms can differ in formation processes, like volcanoes being formed through volcanic activity, while canyons are carved by erosion.
Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.
Clastic sedimentary rocks are formed from the accumulation of rock and mineral fragments, while chemical sedimentary rocks are formed from the precipitation of minerals out of solution. Organic sedimentary rocks are formed from the remains of plants and animals. They differ in their composition, formation process, and appearance.
by magic
spore formation occurs in between meiosis and gamete formation.
The collision-coalescence process is a mechanism of raindrop formation in warm clouds, where water droplets collide and merge to form larger droplets that eventually fall as rain. The Bergeron process, on the other hand, is a mechanism of precipitation in cold clouds where ice crystals in the presence of supercooled water droplets grow at the expense of the water droplets, leading to the formation of precipitation like snow or hail.
while respiration implies air, fermentation is an anaerobic (no oxygen) process.
Pollination is the transfer of pollen from the anther to the stigma on the same or different flower, while fertilization is the fusion of the sperm cell with the egg cell to form a zygote. Pollination is a physical process involving the transfer of pollen, while fertilization is a biological process resulting in the formation of a new organism.
Sedimentory rocks form in several stages, which are: weathering, errosion, sedimentation, cementation and at the end lithification. In case of formation of metamorphic rocks, rock of any origin altered in mineralogical composition, chemical composition, or structure by heat, pressure, and movement. Nearly all such rocks are crystalline.
Growth is the process of becoming larger. Development is the process of becoming more complex.
I assume you meant respiration - in which case : fermentation does not require oxygen.
in uk
penis