Es Corrals topographic map
Click on the map to display elevation.
About this map
Name: Es Corrals topographic map, elevation, terrain.
Location: Es Corrals, Balearic Islands, Spain (39.16723 2.95178 39.18723 2.97178)
Average elevation: 26 ft
Minimum elevation: 0 ft
Maximum elevation: 374 ft
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Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
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Palma de Mallorca
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Palma is a major city and seaport located in the southwest of Mallorca, a western Mediterranean island belonging to the Balearic Islands archipelago. The land area of the city is about 21.355 square kilometres (8.245 sq mi) with an altitude of 13 metres (43 feet) above sea level.
Average elevation: 161 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 200 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 200 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 200 ft
Serra de Tramuntana
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The climate in the Tramuntana Range is significantly wetter than the rest of the island, recording as much as 1507 mm (59.3 inches) of precipitation per year, in comparison with some other parts of the island where annual rainfall is less than 400mm (15 inch). It is also cooler due to the altitude, and a few…
Average elevation: 574 ft
Palma de Mallorca
Spain > Balearic Islands > Palma
Palma is a major city and seaport located in the southwest of Mallorca, a western Mediterranean island belonging to the Balearic Islands archipelago. The land area of the city is about 21.355 square kilometres (8.245 sq mi) with an altitude of 13 metres (43 feet) above sea level.
Average elevation: 161 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
Palma de Mallorca
Spain > Balearic Islands > Palma
Palma is a major city and seaport located in the southwest of Mallorca, a western Mediterranean island belonging to the Balearic Islands archipelago. The land area of the city is about 21.355 square kilometres (8.245 sq mi) with an altitude of 13 metres (43 feet) above sea level.
Average elevation: 161 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
Palma de Mallorca
Spain > Balearic Islands > Palma
Palma is a major city and seaport located in the southwest of Mallorca, a western Mediterranean island belonging to the Balearic Islands archipelago. The land area of the city is about 21.355 square kilometres (8.245 sq mi) with an altitude of 13 metres (43 feet) above sea level.
Average elevation: 148 ft
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Spain > Balearic Islands > Serra de Tramuntana
The climate in the Tramuntana Range is significantly wetter than the rest of the island, recording as much as 1507 mm (59.3 inches) of precipitation per year, in comparison with some other parts of the island where annual rainfall is less than 400mm (15 inch). It is also cooler due to the altitude, and a few…
Average elevation: 574 ft
Palma
Palma is a major city and seaport located in the southwest of Mallorca, a western Mediterranean island belonging to the Balearic Islands archipelago. The land area of the city is about 21.355 square kilometres (8.245 sq mi) with an altitude of 13 metres (43 feet) above sea level.
Average elevation: 161 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
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Average elevation: 36 ft
Palma
Palma is a major city and seaport located in the southwest of Mallorca, a western Mediterranean island belonging to the Balearic Islands archipelago. The land area of the city is about 21.355 square kilometres (8.245 sq mi) with an altitude of 13 metres (43 feet) above sea level.
Average elevation: 148 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
Calvià
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Calvià first appears in history as a village 2,000 years BCE, although the area was first populated in the Neolithic Era. Later, sailors coming from the east stopped in the Balearics on their way to the Iberian Peninsula, where they sought metals. They came from Italy, from other Mediterranean islands, and…
Average elevation: 440 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
Majorca
Mallorca and the other Balearic Islands are geologically an extension of the fold mountains of the Betic Cordillera of Andalusia. They consist primarily of sediments deposited in the Tethys Sea during the Mesozoic era. These marine deposits have given rise to calcareous rocks which are often fossiliferous. The…
Average elevation: 187 ft
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Average elevation: 75 ft
Serra de Tramuntana
Spain > Balearic Islands > Serra de Tramuntana
The climate in the Tramuntana Range is significantly wetter than the rest of the island, recording as much as 1507 mm (59.3 inches) of precipitation per year, in comparison with some other parts of the island where annual rainfall is less than 400mm (15 inch). It is also cooler due to the altitude, and a few…
Average elevation: 574 ft
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Average elevation: 184 ft
