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英語 高校生

赤い下線のところがどういう構造になっているか分からないです、教えてくださいm(_ _)m

moving from " (1) 点) There are historians and others who would like to make a neat division between "historical facts" and "values." The trouble is that values even enter into deciding what count as facts-there is a big leap involved in 'raw data" to a judgement of fact. More important, one finds that the more complex and multi-levelled the history is, and the more important the issues it raises for today, the less it is possible to sustain a fact-value division. But this by no means implies that there has simply to be a conflict of prejudices and biases, as the data are manipulated to suit one worldview or another. What it does mean is that the self of the historian is an important factor. The historian is shaped by experiences, contexts, norms, values, and beliefs. When dealing with history, especially the sort of history that is of most significance in philosophy, that shaping is bound to be relevant. As far as possible it needs to be articulated and open to discussion. The best historians are well aware of this. They are alert to many dimensions of bias and to the endless (and therefore endlessly discussable) significance of their own horizons and presuppositions. A great deal can of course be learned from those who do not share our presuppositions. Our capacity to make wise, well-supported judgements in matters of historical fact and significance can only be formed over years of discussion with others, many of whom have very different horizons from our own. It is possible to I have a 12-year-old chess champion or mathematical or musical genius, but it is unimaginable that the world's greatest expert on Socrates could be that age. The difficulty is not just one of the time to assimilate information; it is (2)

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理科 中学生

この写真の、B、C地点では、それぞれ黒っぽい鉱物をふくむ火山灰の層の下端は標高何メートルのところにありますか、という問題の考え方を教えてほしいです。真ん中よりちょっと上らへんの問題です

を何というか。 この地域ではかつて何が起こったことがわかるか。 (2) A. C地点で火山灰の層が見られることから、 い。 右の図2に、B地点の柱状図の続きをかきなさ A るか。 (4)より、地層は東西どちらに向かって傾いてい ③ ることがわかるか。 くむ火山灰の層の下端は標高何mのところにあ B, C地点では、それぞれ黒っぽい鉱物を多く 130 120 100 B 110 C 100. 図2 B ( ) c ( A 地表からの深さ [m] 地 0 B C 0000 6000 6000 6000 0000 0000 0000 10 0000 0000 600 000 20 VVV 6) A地点では、地表からの深さが25m~60mの地 層で、 れきの層、砂の層、 泥の層が見られる。 こ これらの層のうち、最も古い時期に堆積したものは どれか。 30 www 。 40 50 ° O 00000 000 oooooo00 ooooo0000 o れき、砂、泥を、粒の大きさが小さい順に並べ なさい。 60 ooooooOOO do o ooooooooo. 000000 000 000 0000000000 0000 0000 砂の層 れきの層 泥の層 (6)(7)より、 A地点で地表からの深さが25m -60mの地層が堆積したときの地形の変化のよう 一として考えられるものを、次のア~ウから選び 黒っぽい鉱物が多い火山灰の層 白っぽい鉱物が多い火山灰の層

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