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Natural Monuments

Sudoeste de Inglaterra

Cadjack Cove

Natural Monuments

Sudoeste de Inglaterra

Illogan

Cadjack Cove

Destaque (Segmento) • Praia

Cadjack Cove

Name: Cadjack Cove
Rating: 2

Recomendado por 30 caminhantes

Este Destaque passa por uma área protegida

Por favor, verifique as regulamentações locais para:

Cornwall National Landscape

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Localização:Illogan, Sudoeste de Inglaterra, Inglaterra, Reino Unido

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Indicações para chegar lá

Rotas aqui

Os melhores Percursos de caminhada para Cadjack Cove

4,8

(60)

346

caminhantes

1. Circuito Godrevy Lighthouse – Hell's Mouth Cliffs (ponto de partida: Phillack)

22,5km

06:04

280m

Caminhada difícil. É necessário estar em boa forma. Trilhos acessíveis. Adequado a todos os níveis de experiência.

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Difícil

4,8

(32)

198

caminhantes

2. Circuito Basset's Cove – Basset's Cove (ponto de partida: Portreath)

9,78km

02:43

180m

Caminhada moderada. É necessário estar em boa forma. Trilhos acessíveis. Adequado a todos os níveis de experiência.

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Moderado

4,8

(24)

140

caminhantes

3. Circuito Basset's Cove – Basset's Cove (ponto de partida: Portreath)

9,42km

02:37

170m

Caminhada moderada. É necessário estar em boa forma. Trilhos acessíveis. Adequado a todos os níveis de experiência.

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Moderado

Sugestões

Jonathan Harjes & Melissa Schwarz

9 de janeiro de 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.

Traduzido por Google •

Jonathan Harjes & Melissa Schwarz

23 de janeiro de 2022

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.

Traduzido por Google •

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Detalhes

Informações

Distância 676 m

Desnível positivo 40 m

Desnível negativo 30 m

Previsão do Tempo

Desenvolvido por Foreca

Hoje

quarta-feira 3 dezembro

11°C

9°C

100 %

Se você começar sua atividade agora...

Velocidade máxima do vento: 13,0 km/h

Mais visitado durante

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Indicações para chegar lá

Localização:Illogan, Sudoeste de Inglaterra, Inglaterra, Reino Unido

Outros lugares que merecem uma visita

Hell's Mouth Cliffs

Tehidy Woods

Wheal Coates Tin Mine

St Agnes Head

Godrevy Cove

Mini Afran Trail

Great Wheal Charlotte Engine House

Portreath Harbour and Beach

Tehidy Country Park

Old Tin Mine Route

Woodland Path Beside the Golf Course

The Ancient Twisted Beech, Tehidy Country Park

Cadjack Cove

1. Circuito Godrevy Lighthouse – Hell's Mouth Cliffs (ponto de partida: Phillack)

2. Circuito Basset's Cove – Basset's Cove (ponto de partida: Portreath)

3. Circuito Basset's Cove – Basset's Cove (ponto de partida: Portreath)

Outros lugares que merecem uma visita

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