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The phrase that compares a trace fossil to a fossil that forms as a result of an entire organism being trapped in amber is D. Both can possibly be used to study the organism's size and relative age of a rock.
<h3>What is a fossil?</h3>
A fossil is a remnant, impression, or trace of an animal or plant of a past geologic age that has been preserved in Earth's crust.
In this case, the phrase that compares a trace fossil to a fossil that forms as a result of an entire organism being trapped in amber is that both can possibly be used to study the organism's size, and relative age of a rock.
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Interactions between group members
- interactions with people outside of the group
- interactions with the environment
Explanation:
The culture is the most powerful tool of any society. It is unique to each group, and it is what defines that group of people. The culture has the ability to shape up three types of interactions:
- interactions between group members
- interactions with people outside of the group
- interactions with the environment
The interactions between the group members are good in general, as they belong to the same culture and have lot of similarities. An example can be the interaction between two neighbors.
The interaction with people outside of the group can go either way though. If there are some similarities between the cultures then the people will most probably become close, but if there are big differences, it will most probably cause conflict. An example can be the interaction between a Catholic Mexican and Muslim Arab.
The interaction with the environment is crucial for any culture, and every culture has special and different interaction with it, depending on its characteristics. An example of this can be that the Celtic people considered the trees to sacred, and some trees such as the willow for forbidden for cutting as it was of highest rank.
Groundwater Storage, Porosity, and Specific Yield: Groundwater occupies the cracks and pore spaces between rocks and mineral grains below the land surface. In the saturated zone, essentially all of the pores are filled with water. If a volume of saturated aquifer material is completely dried, the water volume removed reflects the total porosity of the material, or the fraction of pore space within the total volume of solids plus open spaces. This number can be surprisingly large; some minerals and rock formations can have total porosities in excess of 50%. In the unsaturated, or vadose, zone there can be significant amounts of water present, but the voids are not completely filled (see appendix on saturated thickness).
However, some of the pore spaces may be too small or too poorly connected to permit the water they contain to flow out easily. The effective porosity can be thought of as the volume of pore space that will drain in a reasonable period of time under the influence of gravity. Effective porosity is always less than total porosity, sometimes (as in the case of clays) much less. "Good aquifers" tend to have values of effective porosity in the range of 10-30%, although examples of higher and lower values can be found. Figure 1 illustrates the relationship among the types of porosity and the volume of water in storage.
Answer:
smokestacks, discharge pipes, drainage ditches.
Explanation:
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