Answer:
Marcy might be experiencing Dissociative fugue
Explanation:
Dissociative fugue is a mental disorder in which an individual is unable to remember his/her identity or events of the past, as a result, of a tragic or traumatic event. An individual with this type of mental disorder may experience confusion, depression, discomfort, anger, etc.
Dissociative fugue may be triggered by so many tragic events. For instance, a person who have experienced violence in all forms. A tragic car accident may also trigger the disorder or natural disaster among others. Marcy's situation was triggered by a natural disaster (fire), she may be experiencing dissociative fugue as she could not remember her identity.
The general public is the group that tends to be negatively affected by eminent domain laws.
Answer:
<em>Justice Thurgood Marshall</em>
Explanation:
<em><u>h</u></em><em><u>ope </u></em><em><u>it</u></em><em><u> will</u></em><em><u> help</u></em><em><u> you</u></em><em><u> </u></em><em><u>.</u></em><em><u>.</u></em><em><u>.</u></em><em><u>.</u></em><em><u>.</u></em><em><u>.</u></em><em><u>.</u></em><em><u>.</u></em><em><u>.</u></em>
Explanation:
Satellite image of the Piqiang Fault, a northwest trending left-lateral strike-slip fault in the Taklamakan Desert south of the Tian Shan Mountains, China (40.3°N, 77.7°E)
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In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within the Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as subduction zones or transform faults.[1] Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep.[2]
A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault.[3][4]
A fault zone is a cluster of parallel faults.[5][6] However, the term is also used for the zone of crushed rock along a single fault.[7] Prolonged motion along closely spaced faults can blur the distinction, as the rock between the faults is converted to fault-bound lenses of rock and then progressively crushed.[8]
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