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Weathering phases recorded by gnammas developed since last glaciation at Serra da Estrela, Portugal

Published online by Cambridge University Press:  20 January 2017

David Domínguez-Villar ,
Laura Razola ,
Rosa M. Carrasco ,
Carrie E. Jennings  and
Javier Pedraza
David Domínguez-Villar*
Affiliation:
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston B15 2TT Birmingham, UK Departamento de Geodinámica, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain
Laura Razola
Affiliation:
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston B15 2TT Birmingham, UK
Rosa M. Carrasco
Affiliation:
Departamento de Ingeniería Geológica y Minera, Universidad de Castilla-La Mancha, 45071 Toledo, Spain
Carrie E. Jennings
Affiliation:
Minnesota Geolcogical Survey, 2642 University Ave. St. Paul, MN 55114, USA
Javier Pedraza
Affiliation:
Departamento de Geodinámica, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain
*
⁎Corresponding author.

E-mail address:[email protected] (D. Domínguez-Villar).

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Abstract

The morphometrical analysis of gnammas (weathering pits) in granite landscapes has been used to establish the relative chronology of recent erosive surfaces and to provide the weathering history in a region. To test the validity of gnammas as relative chronometer indicators, and the reliability of the obtained weathering record, two sites have been studied in Serra da Estrela, Portugal. The first site is within the limits of the glacier that existed in these mountains during the last glaciation, whereas the second site is located in an unglaciated sector of the mountains, which preserves a longer record of weathering in the bedrock surface. The number of gnamma weathering phases recorded in the latter site (8) is larger than those from the former (6). Correlation between both measurement stations based on morphometrical criteria is excellent for the younger six weathering phases (1 to 6). Consequently, the parameter used for relative chronology (δ-value) has been verified to be age dependent, although absolute values are modulated by microclimate due to altitude variations. The weathering record was essentially duplicated once the surfaces at both sites were exposed, demonstrating the reliability of gnamma evolution as a post-glacial environmental indicator for the region.

Keywords

GnammaWeathering pitGranite geomorphologyMorphometryRelative chronologyWeatheringPaleoenvironmental proxy
Type
Research Article
Information
Quaternary Research , Volume 72 , Issue 2 , September 2009 , pp. 218 - 228
Copyright
University of Washington

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References

Andrade, E., Mora, C., Neves, M., and Vieira, G. Desportos de Inverno na Serra da Estrela. Contribuição para o estudo da sua viabilidade. Finisterra 53/54, (1992). 187–193.Google Scholar
André, M.-F. Rates of postglacial rock weathering on glacially scoured outcrops (Abisko-riskgránsen area, 68°N). Geografi ska Annaler 84A, (2002). 139–150.CrossRefGoogle Scholar
André, M.-F. The geomorphic impact of glaciers as indicated by tors in north Sweden (Aurivaara, 68°N). Geomorphology 57, (2004). 403–421.CrossRefGoogle Scholar
Aniya, M. Holocene glacial chronology in Patagonia: Tyndall and Upsala glaciers. Artic and Alpine Research 27, 4 (1995). 311–322.CrossRefGoogle Scholar
Briner, J.P., Millar, G.H., Davies, P.T., Bierman, P.R., and Caffee, M. Last glacial maximum ice sheet dynamics in Arctic Canada inferred from young erratics perched on ancient tors. Quaternary Science Reviews 22, (2003). 437–444.CrossRefGoogle Scholar
Centeno, J.D. Evolución cuaternaria del relieve en la vertiente sur del Sistema Central Español. Cuadernos do Laboratorio Xeolóxico de Laxe 13, (1989). 79–88.Google Scholar
Chabera, S., (1961). Mísovité vyvčtravání zuly v jizních Cechách. Sborník Krajského vlastivédného musea v Ceských Budéjovicích, Prírodní védy III, 51–67.Google Scholar
Czudek, T., Demeck, J., Marvan, P., Panoš, V., and Raušer, J. Verwitterungs- und abtragungsformen des granits in der Böhmischen Masse. Petermanns Geographische Mitteilungen 108, (1964). 182–192.Google Scholar
Dahl, R. Block fields, weathering pits and tor-like forms in the Narvik Mountains, Nordland, Norway. Geografi ska Annaler 48A, (1966). 55–85.CrossRefGoogle Scholar
Daveau, S. La glaciation de la Serra da Estreala. Finisterra 11, (1971). 5–40.Google Scholar
Daveau, S., Coelho, C., Costa, V.G., Carvalho, L., (1977). Répartition et rythme des précipitations au Portugal. CEG, Lisboa.Google Scholar
Daveau, S., Ferreira, A.B., and Vieira, G. Novas observaçőes acerca da glaciaçaő da Serra da Estrela. Estudos do Quaternario 1, (1997). 41–51.CrossRefGoogle Scholar
Domínguez-Villar, D. Early formation of gnammas (weathering pits) in a recently glaciated area of Torres del Paine, southern Patagonia (Chile). Geomorphology 76, (2006). 137–147.CrossRefGoogle Scholar
Domínguez Villar, D. Análisis morfométrico de pilancones: consideraciones genéticas, evolutivas y paleambientales. (2007). Universidad Complutense de Madrid, Madrid.Google Scholar
Domínguez-Villar, D., and Jennings, C.E. Multi-phase evolution of gnammas (weathering pits) in a Holocene deglacial granite landscape, Minnesota (USA). Earth Surface Processes and Landforms 33, 2 (2008). 165–177.CrossRefGoogle Scholar
Domínguez-Villar, D., Arteaga, C., García-Giménez, R., Smith, E.A., and Pedraza, J. Diurnal and seasonal water variations of temperature, pH, redox potential and conductivity in gnammas (weathering pits). Catena 72, (2008). 37–48.CrossRefGoogle Scholar
Emery, K.O. Marine solution basins. Journal of Geology 54, (1946). 209–228.CrossRefGoogle Scholar
Fairbridge, R.W. Solution pits and pans. Fairbridge, R.W. The Encyclopedia of Geomorphology. (1968). Dowen, Hutchinson & Ross, Stroudsburg. 1033–1036.Google Scholar
Ferreira, N., Vieira, G.T., (1999). Guia geológico e geomorfológico do Parque Natural da Serra da Estrella. Instituto da Conservaçăo da Naturaleza/Instituto Geológico e Mineiro, Lisboa.Google Scholar
Ferreira, M., Iglesias, M., Noronha, F., Pereira, E., and Ribeiro, A.R.M.L. Granitides da Zona Centro Iberica e seu enguadramento geodinamico. Bea, F., Carnicero, A., Gonzalo, J.C., Plaza, M., and Rodríguez Alonso, M.P. Geología de los granitoides y rocas asociadas del Macizo hercínico. Libro homenaje a L.C. García de Figuerola. (1988). Rueda, Alcorcón. 37–51.Google Scholar
Fisher, T.G. Chronology of glacial Lake Agassiz meltwater routed to the Gulf of Mexico. Quaternary Research 59, (2003). 271–276.CrossRefGoogle Scholar
Fränzle, O. Die opferkessel im quarzitischen Sandstein von Fontainebleau. Zeitschrift für Geomorphologie 15, (1971). 212–235.CrossRefGoogle Scholar
Goudie, A.S., and Migoń, P. Weathering pits in the Spitzkoppe area, Central Namib Desert. Zeitschrift für Geomorphologie 41, (1997). 417–444.CrossRefGoogle Scholar
Hall, A.M., and Phillips, W.M. Weathering pits as indicators of relative age of granite surfaces in the Cairngorm Mountains, Scotland. Geografiska Annaler 88A, (2006). 135–150.CrossRefGoogle Scholar
Hedges, J. Opferkessel. Zeitschrift für Geomorphologie 13, (1969). 22–55.Google Scholar
Hudak, C.M., Hajic, E.R., (2005). Landscape evolution of the Minnesota River valley. Abstracts with programs of the North-Central Section 39th Annual Meeting of the Geological Society of America 37, 5.Google Scholar
Lageat, Y., Sellier, D., and Twidale, C.R. Mégalithes et Météorisation des granites en Bretagna littorale, France du nord-ouest. Géographie Physique et Quaternarie 48, (1994). 107–113.CrossRefGoogle Scholar
Lautensach, H. Eiszeitstudien in der Serra da Estrela (Portugal). Zeitschrift für Gletscherkunde 17, (1929). 324–369.Google Scholar
Lautensach, H., (1932). Estudo dos glaciares Serra da Estrela. Memória e Notícias, Coimbra VI, 1–60.Google Scholar
Lidmar-Bergström, K., (1989). Exhumed cretaceous landforms in south Sweden. Zeitschrift für Geomorphologie N.F. Supplement Band 72, 21–40.Google Scholar
Matthes, F.E., (1930). Geologic history of the Yosemite Valley. U.S. Geological Survey Professional Paper 160.Google Scholar
Migoń, P. Granite Landscapes of the World. (2006). Oxford University Press, Oxford.Google Scholar
Patterson, C.J., and Boerboom, T.J. The significance of pre-existing, deeply weathered crystalline rock in interpreting the effects of glaciation in the Minnesota River valley, U.S.A.. Annals of Glaciology 28, (1999). 53–58.CrossRefGoogle Scholar
Phillips, W.P., Hall, A.M., Mottram, R., Fifield, L.K., and Sugden, D.E. Cosmogenic 10Be and 26Al exposure ages of tors and erratics, Cairngorm Mountains, Scotland: timescales for the development of a classic landscape of selective linear glacial erosion. Geomorphology 73, (2006). 222–245.CrossRefGoogle Scholar
Portugal Ferreira, M., Macedo, C.A.R., and Alves, E.I. Azonalidade interna de um plutonito; estruturas condicionantes e idades de evolucao (plutonito du Fundao, Portugal Central). Memorias e Noticias Publicacoes do Museu e Laboratorio Mineralogico e Geologico da Universidade da Coimbra 99, (1985). 213–218.Google Scholar
Röthlisberger, F. 10000 jahre gletschergeschichte der erde. (1986). Verlag Sauerlander, Arau.Google Scholar
Samuelsson, L., and Werner, M. Weathering pits in the Lake Mjörn area northeast of Göteborg. Geografi ska Annaler 60A, (1978). 9–21.CrossRefGoogle Scholar
Sellier, D. Utilisation des mégalithes comme marqueurs de la vitesse de l'erosion des granites en milieu tempéré: enseignements apportés par les alignements de Carnac (Morbihan). Zeitschrift für Geomorphologie 41, (1997). 319–356.CrossRefGoogle Scholar
Teixeira, C., Santos, J.P., de Carvalho, H.F., Peinador, A., Margarida, M., (1974). Carta geológica de Portugal na escala de 1:50.000. Noticia explicativa da foha 20-B, . Covilhã. Lisboa.Google Scholar
Twidale, C.R. Steepened margins of the inselberg from north-western Eyre Peninsula, South Australia. Zeitschrift für Geomorphologie 6, (1962). 51–69.Google Scholar
Twidale, C.R. Flared slopes, scarp-foot weathering and the piedmont angle; comparisons between Australia, southern Africa and the western United States. South African Geographical Journal 4, (1972). 45–52.Google Scholar
Twidale, C.R. Granite Landforms. (1982). Elsevier, Amsterdam.Google Scholar
Twidale, C.R. The origin and implications of some erosional landforms. Journal of Geology 98, (1990). 343–364.CrossRefGoogle Scholar
Twidale, C.R., and Corbin, E.M. Gnammas. Revue de Géomorphologie Dynamique 14, (1963). 1–20.Google Scholar
Uña, E. Variables de control en la génesis y desarrollo del modelado granítico. Análisis de las microformas en el macizo de Manzaneda (Galicia, España). Cuadernos do Laboratorio Xeolóxico de Laxe 22, (1997). 29–42.Google Scholar
Uña, E. Estudio multivariado del micromodelado granítico: interpretación comparada de la génesis y evolución de las gnammas en macizos antiguos. Cuadernos do Laboratorio Xeolóxico de Laxe 23, (1998). 271–282.Google Scholar
Uña, E. Evidencias y pruebas significativas sobre la degradación subaérea en formas menores graníticas: análisis de Caos. Cuadernos do Laboratorio Xeolóxico de Laxe 24, (1999). 177–190.Google Scholar
Van der Knaap, W.O., and Van Leeuwen, J.F.N. Holocene vegetation succession and degradation as responses to climatic change and human activity in the Serra da Estrela, Portugal. Review of Palaeobotany and Palynology 89, (1995). 153–211.CrossRefGoogle Scholar
Van der Knaap, W.O., and Van Leeuwen, J.F.N. Late glacial and Early Holocene vegetation succession, altitudinal vegetation zonation and climate change in the Serra da Estrela. Portugal. Review of Palaeobotany and Palynology 97, (1997). 239–285.CrossRefGoogle Scholar
Vidal Romaní, J.R. El Cuaternario de la provincia de la Coruña. Geomorfología granítica. Modelos elásticos para formación de cavidades. (1983). Universidad Complutense de Madrid, Madrid.Google Scholar
Vieira, G.T. Combined numerical and geomorphological reconstruction of the Serra da Estrela plateau icefield, Portugal. Geomorphology 97, (2008). 190–207.CrossRefGoogle Scholar
Vieira, G.T., Mora, C., (1998). General characteristics of the climate of the Serra da Estrela. In: Vieira, G.T. (Ed.), Glacial and periglacial geomorphology of Serra da Estrela. Guidebook for the fieldtrip, IGU Commission on Climate Change and Periglacial Environments. CEG and Department of Geography of the University of Lisbon, Lisbon., pp.26–36.Google Scholar
Vieira, G.T., Ferreira, A.B., Mycielska-Dowgiallo, E., Woronko, B., and Olszak, I. Thermoluminiscence dating of fluvioglacial sediments (Serra da Estrela, Portugal). Actas V Reuniăo do Cuaternario Ibérico. (2001). SGP, Lisbon. 85–88.Google Scholar
Vieira, G.T., Mora, C., and Ramos, M. Ground temperature regime and geomorphological implications in a Mediterranean mountain (Serra da Estrela, Portugal). Geomorphology 52, (2003). 57–72.CrossRefGoogle Scholar
Vieira, G.T., Ferreira, A.B., and Woronko, B. Glaciogenic deposits and landforms of the Serra da Estrela plateau ice-field and valley glaciers (Portugal). Characteristics and style of deglaciation. Gutierrez, F., Gutierrez, M., Desir, G., Guerrero, J., Lucha, P., Marín, C., and García-Ruíz, J.M Abstract Volume of the Sixth International Conference on Geomorphology. (2005). The International Association of Geomorphologists, Zaragoza. 15 Google Scholar
Worth, R.H., (1953). Dartmoor. In: Spooner, G.M., Russell, R.S. (Eds.), David & Charles, New Abbott.Google Scholar