カーハラックの天然記念物・トップ14

4月は素晴らしいことがあります。ピクニックと双眼鏡を持っていけば、もっとたくさんのものが見られます。

Breathtaking views. Especially when combined with the blooming heather!

Amazing 360 degree views for very little effort

Naturist beach with views.

Stunning panoramic views, well worth the hike to the top. SH Burton described it beautifully in 1952; 'The view from St Agnes Beacon is breath-taking. The high moorlands, heather and gorse clad; steep valleys and bubbling streams; the bracing winds and the infinite variety of land and seascape...' Or even better, F W L Stockdale called it ‘a remarkable stupendous mountain’ back in 1824.

We saw dolphins jumping from St Agnes Head! I have never experienced something like that.

A beautiful spot to stop on a calm day, incredibly windy on a rough day. Plenty of choice of trails for walking or cycling. A special place to stop and admire the surroundings.

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.