Comparative analysis of the glacially deformed Moler Cliffs, Denmark, comprising earliest Eocene, fossiliferous diatomite and volcanic ash layers with contemporaneous deposits: Analysis of geological sites to be compared with the glaciotectonically deformed moler cliffs at Hanklit, Mors, and Knudeklint, Fur, for nomination to the UNESCO World Heritage List

Stig A. Schack Pedersen; Gunver Krarup Pedersen; Bent Erik Kramer Lindow; Bo Pagh Schultz; Henrik Madsen

Comparative analysis of the glacially deformed Moler Cliffs, Denmark, comprising earliest Eocene, fossiliferous diatomite and volcanic ash layers with contemporaneous deposits: Analysis of geological sites to be compared with the glaciotectonically deformed moler cliffs at Hanklit, Mors, and Knudeklint, Fur, for nomination to the UNESCO World Heritage List

Stig A. Schack Pedersen, Gunver Krarup Pedersen, Bent Erik Kramer Lindow, Bo Pagh Schultz, Henrik Madsen

Geology

Original language	English

Publisher	Danmarks og Grønlands Geologiske Undersøgelse
Number of pages	82
Publication status	Published - 2012

Series	Danmarks og Grønlands Geologiske Undersøgelse Rapport
Volume	2012/56

Access to Document

GEUSrapp_2012_56Final published version, 6.25 MB

Cite this

Pedersen, S. A. S., Pedersen, G. K., Lindow, B. E. K., Schultz, B. P., & Madsen, H. (2012). Comparative analysis of the glacially deformed Moler Cliffs, Denmark, comprising earliest Eocene, fossiliferous diatomite and volcanic ash layers with contemporaneous deposits: Analysis of geological sites to be compared with the glaciotectonically deformed moler cliffs at Hanklit, Mors, and Knudeklint, Fur, for nomination to the UNESCO World Heritage List. Danmarks og Grønlands Geologiske Undersøgelse. Danmarks og Grønlands Geologiske Undersøgelse Rapport Vol. 2012/56

Comparative analysis of the glacially deformed Moler Cliffs, Denmark, comprising earliest Eocene, fossiliferous diatomite and volcanic ash layers with contemporaneous deposits: Analysis of geological sites to be compared with the glaciotectonically deformed moler cliffs at Hanklit, Mors, and Knudeklint, Fur, for nomination to the UNESCO World Heritage List. / Pedersen, Stig A. Schack; Pedersen, Gunver Krarup; Lindow, Bent Erik Kramer et al.
Danmarks og Grønlands Geologiske Undersøgelse, 2012. 82 p. (Danmarks og Grønlands Geologiske Undersøgelse Rapport, Vol. 2012/56).

Research output: Book/Report › Report › Research

Pedersen, SAS, Pedersen, GK, Lindow, BEK, Schultz, BP & Madsen, H 2012, Comparative analysis of the glacially deformed Moler Cliffs, Denmark, comprising earliest Eocene, fossiliferous diatomite and volcanic ash layers with contemporaneous deposits: Analysis of geological sites to be compared with the glaciotectonically deformed moler cliffs at Hanklit, Mors, and Knudeklint, Fur, for nomination to the UNESCO World Heritage List. Danmarks og Grønlands Geologiske Undersøgelse Rapport, vol. 2012/56, Danmarks og Grønlands Geologiske Undersøgelse.

Pedersen SAS, Pedersen GK, Lindow BEK, Schultz BP, Madsen H. Comparative analysis of the glacially deformed Moler Cliffs, Denmark, comprising earliest Eocene, fossiliferous diatomite and volcanic ash layers with contemporaneous deposits: Analysis of geological sites to be compared with the glaciotectonically deformed moler cliffs at Hanklit, Mors, and Knudeklint, Fur, for nomination to the UNESCO World Heritage List. Danmarks og Grønlands Geologiske Undersøgelse, 2012. 82 p. (Danmarks og Grønlands Geologiske Undersøgelse Rapport, Vol. 2012/56).

Pedersen, Stig A. Schack ; Pedersen, Gunver Krarup ; Lindow, Bent Erik Kramer et al. / Comparative analysis of the glacially deformed Moler Cliffs, Denmark, comprising earliest Eocene, fossiliferous diatomite and volcanic ash layers with contemporaneous deposits : Analysis of geological sites to be compared with the glaciotectonically deformed moler cliffs at Hanklit, Mors, and Knudeklint, Fur, for nomination to the UNESCO World Heritage List. Danmarks og Grønlands Geologiske Undersøgelse, 2012. 82 p. (Danmarks og Grønlands Geologiske Undersøgelse Rapport, Vol. 2012/56).

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