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首页> 外文期刊>The Mineralogical Record >What's New in Minerals: Springfield Show 2008
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What's New in Minerals: Springfield Show 2008

机译:矿物质的新变化:Springfield Show 2008

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摘要

This year I vowed that while driving home after the Springfield Show I would spend some time studying the geology of New England. Recent articles in the media had referred to a "newly discovered" (that is, new to the media) fault zone under New York City and adjoining parts of New England, so I decided to do some research on the subject. I ordered a geologic map of the northeastern United States from Ward's in Rochester, and I put in a few hours of research on the Internet. The more research I did, the more I realized how complicated the geology of the northeastern United States actually is. According to what's written on the Ward's map, "The Northeastern states, especially the southern New England area, possibly has undergone more violent geographic changes over a longer period of time than any other portion of the United States." Sure enough, on the map the northeast looked to me like a bowl of vegetable soup loaded with alphabet noodles. I decided to visit Cameron's Line, a fault that runs through New England, Manhattan and Staten Island, then through New Jersey and into the Atlantic Ocean-but only on the way home from Springfield, after the show was over.
机译:今年,我发誓要在斯普林菲尔德秀之后开车回家,我会花一些时间研究新英格兰的地质情况。媒体上最近的文章提到了纽约市及新英格兰附近地区的“新发现”(即对媒体来说是新的)断层带,所以我决定对此做一些研究。我从罗切斯特的沃德订购了美国东北部的地质图,并在互联网上进行了数小时的研究。我做的研究越多,我就越意识到美国东北部的地质实际上是多么复杂。根据沃德地图上的记载,“东北地区,尤其是新英格兰南部地区,可能在更长的时期内经历了比美国其他地区更剧烈的地理变化。”果然,在地图上,东北地区对我来说就像一碗盛有字母面条的蔬菜汤。我决定参观卡梅伦线,该线贯穿新英格兰,曼哈顿和史坦顿岛,然后穿越新泽西州并到达大西洋,但仅在展览结束后才从斯普林菲尔德回家。

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