Twente, Nederland
Excursie Landschap Lezen: Organisatie door Ellen Genet - Presentatie en gids in het veld: Henry Hooghiemstra, paleo-ecoloog aan de UVA (Universiteit van Amsterdam)
Wegwijzer naar de ANWB oriënteertafel op de Kuiperberg in Ootmarsum
The Kuiperberg is a 71 meters high hill in the Dutch province Overijssel, Twente, Dinkelland. It is part of a moraine, formed during the Saale Glaciation, a geologic time period that Lasted from 238 tot 126 thousand years ago. The moraine stretched from Ootmarsum till Uelsen in Germany. It's of big geologic and geomorphologic importance. (Source: Wikipedia) Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
The Kuiperberg is a 71 meters high hill in the Dutch province Overijssel, Twente, Dinkelland. It is part of a moraine, formed during the Saale Glaciation, a geologic time period that Lasted from 238 tot 126 thousand years ago. The moraine stretched from Ootmarsum till Uelsen in Germany. It's of big geologic and geomorphologic importance. (Source: Wikipedia) Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
The Kuiperberg is a 71 meters high hill in the Dutch province Overijssel, Twente, Dinkelland. It is part of a moraine, formed during the Saale Glaciation, a geologic time period that Lasted from 238 tot 126 thousand years ago. The moraine stretched from Ootmarsum till Uelsen in Germany. It's of big geologic and geomorphologic importance. (Source: Wikipedia) Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
"Willem Wilmink werd op 25 oktober 1936 in Enschede geboren. Hij was een zeer bekende schrijver, dichter en voordrachtskunstenaar. Het monument betreft een glazen boek geplaatst op een kubus met daar achter een tweetal ligbedden van Bentheimer zandsteen." (bron: heemkunde-ootmarsum.nl)
Monument for Willem Wilmink on the Kuiperberg - Willem Wilmink, born 25 October 1936 in Enschede, was a Dutch poet and writer. The monument on the Kuiperberg excists of a glass book with his portrait and poem, placed on a sandstone kube with behind it two loungers carved in Bentheim sandstone.
"Willem Wilmink werd op 25 oktober 1936 in Enschede geboren. Hij was een zeer bekende schrijver, dichter en voordrachtskunstenaar. Het monument betreft een glazen boek geplaatst op een kubus met daar achter een tweetal ligbedden van Bentheimer zandsteen." (bron: heemkunde-ootmarsum.nl)
"De Kuiperberg is een 71 meter hoge heuvel in de Twentse gemeente Dinkelland in de Nederlandse provincie Overijssel. De top van de Kuiperberg ligt even ten westen van Ootmarsum.
De Kuiperberg maakt deel uit van de stuwwal die zich uitstrekt van Ootmarsum tot Uelsen in Duitsland. " (bron: Wikipedia)
"Willem Wilmink werd op 25 oktober 1936 in Enschede geboren. Hij was een zeer bekende schrijver, dichter en voordrachtskunstenaar. Het monument betreft een glazen boek geplaatst op een kubus met daar achter een tweetal ligbedden van Bentheimer zandsteen." (bron: heemkunde-ootmarsum.nl)
"De Kuiperberg is een 71 meter hoge heuvel in de Twentse gemeente Dinkelland in de Nederlandse provincie Overijssel. De top van de Kuiperberg ligt even ten westen van Ootmarsum.
De Kuiperberg maakt deel uit van de stuwwal die zich uitstrekt van Ootmarsum tot Uelsen in Duitsland. " (bron: Wikipedia)
"Willem Wilmink werd op 25 oktober 1936 in Enschede geboren. Hij was een zeer bekende schrijver, dichter en voordrachtskunstenaar. Het monument betreft een glazen boek geplaatst op een kubus met daar achter een tweetal ligbedden van Bentheimer zandsteen." (bron: heemkunde-ootmarsum.nl)
"De Kuiperberg is een 71 meter hoge heuvel in de Twentse gemeente Dinkelland in de Nederlandse provincie Overijssel. De top van de Kuiperberg ligt even ten westen van Ootmarsum.
De Kuiperberg maakt deel uit van de stuwwal die zich uitstrekt van Ootmarsum tot Uelsen in Duitsland. " (bron: Wikipedia)
"Willem Wilmink werd op 25 oktober 1936 in Enschede geboren. Hij was een zeer bekende schrijver, dichter en voordrachtskunstenaar. Het monument betreft een glazen boek geplaatst op een kubus met daar achter een tweetal ligbedden van Bentheimer zandsteen." (bron: heemkunde-ootmarsum.nl)
"De Kuiperberg is een 71 meter hoge heuvel in de Twentse gemeente Dinkelland in de Nederlandse provincie Overijssel. De top van de Kuiperberg ligt even ten westen van Ootmarsum.
De Kuiperberg maakt deel uit van de stuwwal die zich uitstrekt van Ootmarsum tot Uelsen in Duitsland. " (bron: Wikipedia)
The Kuiperberg is a 71 meters high hill in the Dutch province Overijssel, Twente, Dinkelland. It is part of a moraine, formed during the Saale Glaciation, a geologic time period that Lasted from 238 tot 126 thousand years ago. The moraine stretched from Ootmarsum till Uelsen in Germany. It's of big geologic and geomorphologic importance. (Source: Wikipedia) Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
The Kuiperberg is a 71 meters high hill in the Dutch province Overijssel, Twente, Dinkelland. It is part of a moraine, formed during the Saale Glaciation, a geologic time period that Lasted from 238 tot 126 thousand years ago. The moraine stretched from Ootmarsum till Uelsen in Germany. It's of big geologic and geomorphologic importance. (Source: Wikipedia) Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
De Kuiperberg is een 71 meter hoge heuvel in de Twentse gemeente Dinkelland in de Nederlandse provincie Overijssel. De top van de Kuiperberg ligt even ten westen van Ootmarsum.
De Kuiperberg maakt deel uit van de stuwwal die zich uitstrekt van Ootmarsum tot Uelsen in Duitsland. (bron: Wikipedia) Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
Kuiperberg landscape with tourism Informationboard, ANWB orientation table and monument Willem Wilmink
The Kuiperberg is a 71 meters high hill in the Dutch province Overijssel, Twente, Dinkelland. It is part of a moraine, formed during the Saale Glaciation, a geologic time period that Lasted from 238 tot 126 thousand years ago. The moraine stretched from Ootmarsum till Uelsen in Germany. It's of big geologic and geomorphologic importance. (Source: heemkunde-ootmarsum.nl and Wikipedia) Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
Rivier de Dinkel en Dinkeldal. Henry zegt hierover: "De rivier de Dinkel stroomt tussen de stuwwal van Ootmarsum en de stuwwal van Oldenzaal. Sedimenten die in de laatste 130.000 jaar door wind en rivieren zijn afgezet worden door de rivier de Dinkel weer aangesneden en afgevoerd. In het Lutterszand heeft de Dinkel diep ingesneden in zijn eigen sedimenten. " River Dinkel and Dinkel Valley, nature reserve Lutterzand in De Lutte, the Netherlands - Province Twente. The River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meandering river. Sediments that in the past 130.000 years were deposited by wind and rivers are broached again and deported by the Dinkel. In the Lutterzand Nature reserve, the Dinkel has cut in deeply in its own sediments, revealing several historic earth layers in its shores.
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
Rivier de Dinkel en Dinkeldal. Henry zegt hierover: "De rivier de Dinkel stroomt tussen de stuwwal van Ootmarsum en de stuwwal van Oldenzaal. Sedimenten die in de laatste 130.000 jaar door wind en rivieren zijn afgezet worden door de rivier de Dinkel weer aangesneden en afgevoerd. In het Lutterszand heeft de Dinkel diep ingesneden in zijn eigen sedimenten. " River Dinkel and Dinkel Valley, nature reserve Lutterzand in De Lutte, the Netherlands - Province Twente. The River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meandering river. Sediments that in the past 130.000 years were deposited by wind and rivers are broached again and deported by the Dinkel. In the Lutterzand Nature reserve, the Dinkel has cut in deeply in its own sediments, revealing several historic earth layers in its shores.
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
Foto gemaakt aan de oever van de rivier de Dinkel in Twente, Nederland
Rivier de Dinkel en Dinkeldal. Henry zegt hierover: "De rivier de Dinkel stroomt tussen de stuwwal van Ootmarsum en de stuwwal van Oldenzaal. Sedimenten die in de laatste 130.000 jaar door wind en rivieren zijn afgezet worden door de rivier de Dinkel weer aangesneden en afgevoerd. In het Lutterszand heeft de Dinkel diep ingesneden in zijn eigen sedimenten. " River Dinkel and Dinkel Valley, nature reserve Lutterzand in De Lutte, the Netherlands - Province Twente. The River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meandering river. Sediments that in the past 130.000 years were deposited by wind and rivers are broached again and deported by the Dinkel. In the Lutterzand Nature reserve, the Dinkel has cut in deeply in its own sediments, revealing several historic earth layers in its shores.
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
River Dinkel and Dinkel Valley, nature reserve Lutterzand in De Lutte, the Netherlands - Province Twente. Erosion, wind and rain have created natural sand sculptures in the sandy shore of the river. River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meanThe River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meandering river. Sediments that in the past 130.000 years were deposited by wind and rivers are broached again and deported by the Dinkel. In the Lutterzand Nature reserve, the Dinkel has cut in deeply in its own sediments, revealing several historic earth layers in its shores.
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
River Dinkel and Dinkel Valley, nature reserve Lutterzand in De Lutte, the Netherlands - Province Twente. Erosion, wind and rain have created a whimsical pattern of natural sand sculptures in the sandy shore of the river. River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meandering river. Sediments that in the past 130.000 years were deposited by wind and rivers are broached again and deported by the Dinkel. In the Lutterzand Nature reserve, the Dinkel has cut in deeply in its own sediments, revealing several historic earth layers in its shores.
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
River Dinkel and Dinkel Valley, nature reserve Lutterzand in De Lutte, the Netherlands - Province Twente. Erosion, wind and rain have created a whimsical pattern of natural sand sculptures in the sandy shore of the river. The River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meandering river. Sediments that in the past 130.000 years were deposited by wind and rivers are broached again and deported by the Dinkel. In the Lutterzand Nature reserve, the Dinkel has cut in deeply in its own sediments, revealing several historic earth layers in its shores.
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)
River Dinkel and Dinkel Valley, nature reserve Lutterzand in De Lutte, the Netherlands - Province Twente. Erosion, wind and rain have created a whimsical pattern of natural sand sculptures in the sandy shore of the river. The River Dinkel streams between the moraine of Ootmarsum and the moraine of Oldenzaal. It's an active, freely meandering river. Sediments that in the past 130.000 years were deposited by wind and rivers are broached again and deported by the Dinkel. In the Lutterzand Nature reserve, the Dinkel has cut in deeply in its own sediments, revealing several historic earth layers in its shores.
Photo's made during a paleo-ecologic excursion 'Reading the Landscape' in Twente, the Netherlands - guided by Henry Hooghiemstra, paleo-ecologist on the UVA (University of Amsterdam)