Composed image
Alta Via 1, Dolomieten (I), 2017.
Rock in the Sea @ Audresselles.
Audresselles Nord-Pas -De-Calais (F)
12/2021.
2019
Bourgoyen-Ossemeersen, Ghent (B)
2019
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
In the last few decades, research has made it clear that Þingvellir is a natural wonder on a international scale, with the geologic history and the biosystem of Lake Þingvallavatn forming a unique entity, a magnificent showcase.
Being able to witness the evolution and formation of new species in a place like Lake Þingvallavatn is of immense value.
The Þingvellir area is part of a fissure zone running through Iceland, being situated on the tectonic plate boundaries of the Mid-Atlantic Ridge.
The faults and fissures of the area make evident the rifting of the earth's crust.
2017
2017
2017
Oostende (B),
January 2023
Composed image
Alta Via 1, Dolomieten (I), 2017.
Rock in the Sea @ Audresselles.
Audresselles Nord-Pas -De-Calais (F)
12/2021.
2019
Bourgoyen-Ossemeersen, Ghent (B)
2019
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
Cayeux-sur-Mer (F)
2018
In the last few decades, research has made it clear that Þingvellir is a natural wonder on a international scale, with the geologic history and the biosystem of Lake Þingvallavatn forming a unique entity, a magnificent showcase.
Being able to witness the evolution and formation of new species in a place like Lake Þingvallavatn is of immense value.
The Þingvellir area is part of a fissure zone running through Iceland, being situated on the tectonic plate boundaries of the Mid-Atlantic Ridge.
The faults and fissures of the area make evident the rifting of the earth's crust.
2017
2017
2017
Oostende (B),
January 2023