Cova Crater
Paul
Cova Crater is a volcanic caldera located in the east-central region of Santo Antão island, Cape Verde, within the municipality of Paul. The caldera spans approximately 1.0 km in diameter, with elevations ranging from its lowest point at 1,166 meters to about 1,500 meters at the rim. Formed between 1.4 million and 700,000 years ago, it is part of the Cova-Paul-Ribeira da Torre Natural Park. The crater's environment benefits from high precipitation due to trade winds, fostering diverse vegetation. The northern and northeastern crater walls support natural and semi-natural flora, while the southern slopes are covered by forests of pine (Pinus) and cypress (Cupressus) species. At the crater's base, traditional agriculture thrives with maize and beans cultivation. A small village, part of Cabo da Ribeira, with a population of about ten people as of 2010, is situated within the crater. This blend of geological history, rich biodiversity, and human presence makes Cova Crater a unique natural feature worth exploring.
ヒント: Visitors should plan their trip during the wetter months to experience the lush vegetation at its peak. Due to the crater's remote location and small local population, arranging guided tours in advance is advisable. No specific ticketing is required, but respecting the natural environment and local agricultural activities is important. Comfortable hiking shoes and weather-appropriate clothing are recommended for exploring the crater and its surroundings.
興味深い事実
- •The crater's diameter is about 1.0 km, with elevations ranging from 1,166 m to approximately 1,500 m at the rim.
- •Cova Crater is part of the Cova-Paul-Ribeira da Torre Natural Park, a protected area in Cape Verde.
- •The crater benefits from high precipitation carried by trade winds, supporting diverse vegetation.
- •South-facing walls of the crater are forested with pine and cypress species, uncommon in many volcanic craters.
- •A small village with around ten inhabitants is located inside the crater, practicing traditional agriculture.
歴史
Cova Crater was formed between 1.4 million and 700,000 years ago as a volcanic caldera.
Over time, the crater developed diverse vegetation supported by trade wind-driven precipitation.
Human settlement within the crater, including the small village of Cabo da Ribeira, has been established with traditional farming practices at the crater floor.
The area has been designated as part of the Cova-Paul-Ribeira da Torre Natural Park to protect its unique geological and ecological characteristics.
場所ガイド
Crater Rim
The rim of the Cova Crater offers panoramic views of the caldera and surrounding landscapes, with elevations reaching up to about 1,500 meters. The rim's vantage points are ideal for photography and appreciating the geological formation.
Crater Floor Agriculture
At the bottom of the caldera, visitors can observe traditional farming activities where maize and beans are cultivated, showcasing the sustainable use of volcanic soil by local inhabitants.
Forested South-facing Walls
The southern slopes of the crater are covered with forests of Pinus and Cupressus species, creating a distinctive ecological zone within the volcanic environment.
