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Cadjack Cove

ハイライト (セグメント) • ビーチ

Cadjack Cove

人のハイキング愛好家30人がおすすめしました

このハイライトに行くルートは保護地区を通過

現地の条例を必ず確認してください。Cornwall National Landscape

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  • 目的地に設定

    ここにルートがあります

    「Cadjack Cove」に行くハイキングのベストルート

    4.8

    (60)

    346

    ハイカー

    1. Phillackから出発する Godrevy Lighthouse – Hell's Mouth Cliffs ループコース

    22.5km

    06:04

    280m

    280m

    難しいハイキング. 標準以上のフィットネスレベルが必要です。 進みやすいルートです。あらゆるスキルレベルに適しています。

    ナビゲート

    スマートフォンに送信

    難しい

    中程度のハイキング. ある程度のフィットネスレベルが必要です。 進みやすいルートです。あらゆるスキルレベルに適しています。

    中程度

    中程度のハイキング. ある程度のフィットネスレベルが必要です。 進みやすいルートです。あらゆるスキルレベルに適しています。

    中程度

    役立つ情報

    1月 9, 2022

    GB: In Cadjack Cove, in addition to large faults, many folds can be seen. These folds are formed in different scales ranging from a few inches to several hundred feet. In addition, the folds show different degrees of openings and roundness. Very narrow folds with pointed angles are called "kink bands". Overall, the folds were formed during the Variscan mountain building phase/orogenesis (417 - 200 Ma). The high pressures from the south have deformed the relatively soft rocks. However, the folds seen in this bay are not the main folds but represent folds that are folded within themselves.
    Another special feature in this bay are the pink to dark red colored rocks. This change in color is caused by iron-rich water running down the cliffs.

    EN: In addition to large faults, many folds can also be seen in Cadjack Cove. These folds are formed at different scales and range from a few centimeters to several meters. The folds also show different openings and curves. Very tight folds with acute angles are called “kink bands.” Overall, the folds were formed during the Variscan orogeny (417 – 200 Ma). The strong pressure from the south has deformed the relatively soft rocks. However, the folds seen in this bay are not the main folds, but rather represent folds folded into themselves.
    Another special feature of this bay are the pink to dark red colored rocks. This discoloration is caused by iron-rich water running down the cliffs.

    翻訳者 Google •

      GB: In Cadjack Cove, tectonic features can be seen, such as faults (described in ⑦) and folds, which were formed during the Variscan orogeny as a result of pressure from the south. These folds are formed on different scales and range from a few inches to several hundred feet. In addition, the folds show different openings and curves. Very narrow folds with pointed angles are called kink bands. However, the folds seen in this bay are not the main folds of orogeny but represent folds that are folded in themselves. Another special feature in this bay is the pink to dark red coloring of the rocks. This is caused by iron-rich water that runs down the cliffs.

      EN: Tectonic phenomena can be seen in Cadjack Cove, such as faults (described in ⑦) and folds, which were formed by pressure from the south during the Variscan Orogeny. These folds are formed at different scales and range from a few centimeters to several meters. The folds also show different openings and curves. Very tight folds with acute angles are called kink bands. However, the folds seen in this bay are not the main folds of the orogeny, but rather represent folds that fold into themselves. Another special feature in this bay is the pink to dark red color of the rocks. This is caused by iron-rich water running down the cliffs.

      翻訳者 Google •

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        情報

        距離 676 m

        上り 40 m

        下り 30 m

        天気

        AerisWeatherによる提供

        今日

        水曜日 19 11月

        7°C

        6°C

        70 %

        今すぐアクティビティを始めると...

        最大風速: 35.0 km/h

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        場所:イローガン, イングランド南西部, イングランド, イギリス

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