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.
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.
Plate tectonics is a term used to describe how the plates or slabs are formed as a result of faults and folds created within the earth surface and this term also used in describing how the earth was formed due to the impact of large solid objects from the outer space and the removal of gas due to the SolarWinds.
The mantel that is composed of three layers and the top of them being the asthenosphere on which Alfred Wegener gave evidence that the terrestrial plate floats freely on these with less resistance offered by SIMA.
The puzzle evidence also suggested by him was about the same theory that made the large supercontinents in existence and from which the later land masses broke off to form Pangea and Gondwanaland.
Later on much-studied were conducted in this tic to test its validity and found that the continents were truly displaced due to the spreading of the oceanic floors due to the mid-oceanic ridges and these accounts for 99% of the oceanic crustal masses. It was only possible through the deep exploration of the paleomagnetism and chain of rocks of various ages.
