The model were the sun is in the center of the solar system is called heliocentric.
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Answer:
El río que separa el macizo de Brasilia y el macizo Patagónico se llama río Colorado.
Explanation:
El macizo de Brasilia comprende el actual Brasil y el macizo Patagónico, buena parte de la actual Argentina. El macizo de Brasilia cubre buena parte del centro, todo el este, noreste, centro-norte, centro-sur y sureste de América del Sur, mientras que el macizo cubre todo el sur de Argentina. El río que separa ambos macizos se llama el río Colorado, el cual atraviesa las provincias de Mendoza, Neuquén, Río Negro, La Pampa y Buenos Aires antes de desembocar en el Océano Atlántico.
Answer: Culture has the ability to shape three types of interactions for members of a group: interactions between group members, outside of members, and with the environment. When it comes to interactions between each other, people in a culture are taught at a young age what is acceptable and what is not acceptable. For example, kids observe and practice how close to stand to somebody else. They learn appropriate greetings when they start conversations. They are also given direct instruction on how to interact at school and with adults within the society. Cultural differences or similarities with other groups can dictate interactions with outside groups. When different cultural groups find similarities, they often have positive interactions with one another. If they do not have much in common, each group must take some time to learn about the other group, and they must learn how to interact and compromise with each other. Culture can also have a large impact on how people interact with their environment. This can include how to build structures to adapt to climate differences, how traditions are practiced, and what clothing styles are worn.
The equatorward bending of height contours for the 500 mb level imply the presence of a trough because this represents a region of overall lower heights. A valley and a trough are hence equivalent in the upper air flow.
A trough is a linear structural depression with lateral length that occurs in geology. A trough can be a small basin or a natural rift, albeit it is lower than a trench. At the edge of tectonic plates, these landforms frequently form.
Trough, an extended depression in the seafloor that differs from oceanic trenches in that it is shallower, shorter, narrower, and topographically more mild. The Papuan Trough's maximum depth is 2,300 m (7,500 feet), while the Banda Trough's maximum depth is 7,440 m.
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