With regard to the culture clashes in different nations and communities, use of the contact hypothesis theory could help to ease tensions.
In the contact hypothesis theory, which is credited to Gordon Allport, is the ability for two or more cultures to coexist peacefully through meaningful and thoughtful interaction in order to reduce prejudice. To ensure successful contact, it is recommended that: both groups receive equal status of importance with minimal differences in characteristics, backgrounds, and qualities; groups work towards achieving a common goal which is equally beneficial to both groups; there is cooperation from all subjects in each group; support from local authorities of laws/government and customs; personal interaction between members of opposing groups.
Potential outcomes for successful tourist-host contact include: relaxed attitudes, understanding, a mutual appreciation for the opposing culture's values, positive interactions wherein cultures are respected mutually, increased active communication to ensure both parties are satisfied and can co-exist peacefully, and perceiving the opposing culture as equally important.
Answer:
B) a writing system used in ancient Egypt
Answer:
Ego intergrity
Explanation:
Erikson described ego integrity as the acceptance of one’s one and only life cycle as something that had to be and later as a sense of coherence and wholeness As people grow older (65+ yrs) and become senior citizens, they tend to slow down their productivity and explore life as a retired person
The grandparents by spending time with their grandchikdren anc thinking and talking about goals and planning ways to kead a meanful life is them cultivating ego intergrity meaning they accepted their life as it is wanting to pass on what they thought they have made out of life. They explore life as having achieved all they can and seeing what they can pass on.
Answer:
b.slow deformation
Explanation:
The type of deformation that is experienced by the rocks before an earthquake is a slow deformation. This slow deformation is due to some resistance to the slippage movement along the fault lines. This slippage movement is naturally occurring. The slow deformation starts to take place when their is resistance to this slippage movement and as a result of this resistance, elastic strain energy is created. This build up strain causes this slow deformation and eventually leads to an abrupt release of energy in the form of an earthquake.
