웬드론‬에서 가장 멋진 ‪20‬개의 천연기념물

절벽의 멋진 전망

Road side cafe available - a perfect mid point stop off as we head back to Gwithian Bridge

Breathtaking views. Especially when combined with the blooming heather!

Naturist beach with views.

This is a nice combination. From Loe Baar you have a view of the sea on one side and a view of a freshwater lake on the other. This allows you to walk completely around the lake.

Loe Bar was originally the mouth of the River Cober which led to a harbor at Helston. However, by the 13th century the bar had cut Helston off from the sea and formed the lake. Loe Bar consists largely of chert deposits, although it is not certain where this comes from as the nearest source is more than 200 kilometers away. There is also a reasonable amount of sand. (Cornwall Beaches)

Council Porthleven

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.