John Diemer
Biographic Data
| ID | 6042536 |
|---|---|
| NAME | John Diemer |
| GIVEN NAMES | John |
| FAMILY NAME | Diemer |
| SIGNATURE | DIEMER J |
| AFFILIATIONS | University of North Carolina at Charlotte |
| ORCID | 0000-0002-0697-5648 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1995 |
| LATEST PUBLICATION YEAR | 2013 |
| H-INDEX | 0 |
A multiproxy record of postglacial climate variability from a shallowing, 12-m deep sub-alpine bog in the southeastern San Juan Mountains of Colorado, USA
Pollen assemblages, diatom assemblages, and sedimentology, from Cumbres Bog in the southeastern San Juan Mountains of Colorado, provide a record of climate and environmental change since the end of the last glacial maximum (LGM). Cumbres Bog is unusually deep (basal sediments extend 12 m below the surface) for its altitude (~3050 m a.s.l.) and we extracted 7 m core of continuous sediment below ~5 m of water and peat. The resulting record provides…
Post-glacial landscape response to climate variability in the southeastern San Juan Mountains of Colorado, USA
Geomorphic mapping in the upper Conejos River Valley of the San Juan Mountains has shown that three distinct periods of aggradation have occurred since the end of the last glacial maximum (LGM). The first occurred during the Pleistocene–Holocene transition (~ 12.5–9.5 ka) and is interpreted as paraglacial landscape response to deglaciation after the LGM. Evidence of the second period of aggradation is limited but indicates a small pulse of sedime…
Surficial Geologic Map of the Upper Conejos River Drainage, Southeastern San Juan Mountains, Southern Colorado, USA
Please click here to download the map associated with this article. During the Last Glacial Maximum (LGM), the San Juan Mountains of southern Colorado, USA were covered by one of the largest ice caps in North America. The deposits formed subsequent to LGM retreat provide a record of the interaction between post-LGM climate change and late Quaternary landscape evolution. In order to determine the role of post-LGM climate change in alpine landscape…
Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie
Michael Collie, John Diemer, Roderick Impey Murchison, George Gordon of Birnie, Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie, Transactions of the American Philosophical Society, New Series, Vol. 85, No. 3 (1995), pp. i-xxix+1-263
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Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie
Michael Collie, John Diemer, Roderick Impey Murchison, George Gordon of Birnie, Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie, Transactions of the American Philosophical Society, New Series, Vol. 85, No. 3 (1995), pp. i-xxix+1-263
Surficial Geologic Map of the Upper Conejos River Drainage, Southeastern San Juan Mountains, Southern Colorado, USA
Please click here to download the map associated with this article. During the Last Glacial Maximum (LGM), the San Juan Mountains of southern Colorado, USA were covered by one of the largest ice caps in North America. The deposits formed subsequent to LGM retreat provide a record of the interaction between post-LGM climate change and late Quaternary landscape evolution. In order to determine the role of post-LGM climate change in alpine landscape…
Post-glacial landscape response to climate variability in the southeastern San Juan Mountains of Colorado, USA
Geomorphic mapping in the upper Conejos River Valley of the San Juan Mountains has shown that three distinct periods of aggradation have occurred since the end of the last glacial maximum (LGM). The first occurred during the Pleistocene–Holocene transition (~ 12.5–9.5 ka) and is interpreted as paraglacial landscape response to deglaciation after the LGM. Evidence of the second period of aggradation is limited but indicates a small pulse of sedime…
A multiproxy record of postglacial climate variability from a shallowing, 12-m deep sub-alpine bog in the southeastern San Juan Mountains of Colorado, USA
Pollen assemblages, diatom assemblages, and sedimentology, from Cumbres Bog in the southeastern San Juan Mountains of Colorado, provide a record of climate and environmental change since the end of the last glacial maximum (LGM). Cumbres Bog is unusually deep (basal sediments extend 12 m below the surface) for its altitude (~3050 m a.s.l.) and we extracted 7 m core of continuous sediment below ~5 m of water and peat. The resulting record provides…
Geography (3 works) · Geology and Paleoclimatology Research (3 works) · Glacial period (3 works) · Holocene (3 works) · Physical geography (3 works) · Archaeology (2 works) · Climate change (2 works) · Cryospheric studies and observations (2 works) · Geology (2 works) · Geomorphology (2 works)