過去6000年間,デラウェア川渓谷のオーバーバンク沈殿
まとめ
デラウェア川渓谷の洪水平原の堆積物は,オーバーバンク堆積を通じて6000年以上にわたって継続的に蓄積されています. このゆっくりと絶え間ないプロセスは,川によって駆動されています.
科学分野:
- 地質学 地質学 地質学
- 堆積物学 堆積物学 堆積物学 堆積物学 堆積物学
- 四次科学とは四次科学である.
背景:
- 洪水平原は,河川のプロセスによって形作られるダイナミックな風景です.
- 沈殿物の蓄積を理解することは,河川の歴史を再構築し,将来の変化を予測するために不可欠です.
研究 の 目的:
- デラウェア川の洪水平原の堆積の歴史を分析するために.
- 洪水平原の形成に起因する支配的なジオモルフィックプロセスを決定する.
主な方法:
- 洪水平原の堆積物の堆積物分析. 洪水平原の堆積物の堆積物分析.
- 放射性炭素年代測定法により,年代的枠組みを確立する.
主要な成果:
- 厚く,断続的なオーバーバンク洪水平原の堆積物が特定されました.
- ポイントバーの堆積や重大な侵食の証拠は見つかりませんでした.
- 堆積は少なくとも6000年前に始まり,現在まで続いている.
結論:
- オーバーバンク堆積は,デラウェア川渓谷の洪水平原建設の主なメカニズムです.
- 川の緩やかな横流移動率は,運河の移転と侵食よりも,継続的なオーバーバンク蓄積を好む.
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