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Blake
Professor
DevinUpward delivery refers to communication or information flowing from lower- to higher-level individuals within an organization. Downward delivery is the opposite, flowing from higher- to lower-level individuals. Both types are crucial for effective communication and decision-making within a hierarchical structure.
some gases are denser than (heavier) air e.g. CO2, HCl, H2S, Cl2. are delivered by downward delivery. while gases which are Less dense than (lighter) air e.g. H2,NH3 are delivered by upward delivery.
simultaneously the downward delivery of gas = upward displacement of air while upward delivery of gas = downward displacement of air.
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Is argon an upward delivery gas?
No. Argon is slightly denser than air so would not be collected by upward delivery. In practice downward delivery would be unreliable as the difference in density is so small. However there is no way to prepare argon in the lab so the question is redundant.
When two normal faults forn parallel to each other a block of rockis left lying between them and as the normal fault slips downward the block in between moves upward forming a?
fault block mountian
What are the wind conditions for a a tornado?
Tornadoes form during thunderstorms that occur when there is strong difference, meaning a significant difference between winds at low and high levels. The thunderstorm has updraft (upward moving air) and downdraft (downward moving air) regions. The tornado forms in a rotating part of the updraft called a mesocyclone. A downdraft wraps around the mesocyclone, causing it to tighten and intensify into a tornado.
What type of fault occurs when compression forces push one of the fault upward and the other side downward?
thrust A+
Does folding of the crust produce anticlines and synclines?
Yes, folding of the crust can produce anticlines (upward-arched folds) and synclines (downward-arched folds) due to compressional forces. Anticlines are typically associated with the upward buckling of rock layers, while synclines are associated with the downward bending of rock layers.
