まとめ
ペンシルバニア州の植物化石を含む氷河期の岩石がブロンクスで発見された. この発見は,まだ発見されていないペンシルバニアの岩層がハドソン渓谷に存在する可能性があることを示唆しています.
科学分野:
- 地質学 地質学 地質学
- パレオントロジー・パレオントロジー
- 四季地質学 四季地質学
背景:
- 氷河の不規則性はブロンクスでよく見られるが,その地質的起源は複雑である.
- ペンシルバニア時代の岩石は,通常,すぐ近くの地域で発見されません.
研究 の 目的:
- 珍しい氷河岩の発見を記録するために.
- この発見がハドソン・バレーに及ぼす地質学的影響を調査する.
主な方法:
- 氷河岩のフィールド観察とサンプル採取.
- 岩石の組成と化石含有量の地質学的分析.
主要な成果:
- 変形も変形もない石塊が回収されました.
- この岩には,ペンシルバニア州中部の植物化石が含まれています.
- この岩の特徴は,現地の地質学と一致していない.
結論:
- この化石化した岩石の存在は,ブロンクスの現在の地質モデルに挑戦しています.
- これは,ハドソン・バレー内の未発見のペンシルバニアの岩石の突出点の可能性を示しています.
- これらの潜在的地質的異常値を調査するために,さらなる研究が必要である.
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