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.
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.
Slaty cleavage is a result of stress and strain during the metamorphism process where the minerals that make up the slate become deformed and or re-crystallise with an orientation normal to the principle stress field. The fissile nature of shale is a result of the preferential alignment of clay minerals during the formation of the rock. This is because clay minerals are plate like and so form horizontal layers much like you would get if you stacked playing cards.
Dont differ like if it helped
Rocks differ from their textures, hardness, colour, composition and shapes.
The two polyatomic Ions do not differ.
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.
spore formation occurs in between meiosis and gamete formation.
by magic
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.
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.
while respiration implies air, fermentation is an anaerobic (no oxygen) process.
In budding , a small part of the body of the parent organism grows out as bud which then detaches and becomes a new organism.... While in spore formation the parent plant produces hundreds of microscopic reproductive units caleed spores . When the spore case of the plant burts , then the spores spread into air. and then after the process they germinate and produce new plants.
I assume you meant respiration - in which case : fermentation does not require oxygen.
Growth is the process of becoming larger. Development is the process of becoming more complex.
Phlebitis = inflammation of a veinThrombophlebitis = inflammation of a vein caused by or associated with a formation of a thrombus (blood clot)
penis
yes, a huge lot!