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Holocene glacier fluctuations reconstruction in the Western Alps : contributi...
Mountain glaciers are one of the most reliable climatic proxy on Earth through their rapid response to slight changes in forcing and their wide distribution. For these... -
Enregistrements climatiques à Law Dome : variabilité pour les périodes récent...
The complexity of the climate system means that for the reconstruction of past variations, the use of a multiplicity of proxy indicators is mandatory. Polar ice cores... -
7000 years of paleostorm activity in the NW Mediterranean Sea in response to ...
International audience -
Reply to the Comment on " Shoreface sand supply and mid- to late Holocene aeo...
International audience -
Shoreface sand supply and mid- to late Holocene aeolian dune formation on the...
International audience -
Les calcites de Fontainebleau : une clé pour dater la silicification des grès ?
Guide pour une excursion géologique. -
Holocene land-use evolution and associated soil erosion in the French Prealps...
International audience -
Etude des variations du cycle du carbone au cours de l'Holocène à partir de l...
Extracted air from polar ices of Greenland and Antarctica constitute a real archive of the past atmospheres of our planet. The aim of this study was to understand the... -
New constraints on the age and origin of the sandy to clayey surface cover ho...
Independently of their underlying basement, the superficial formations of Gabon display a constant organization, showing the superposition of two units: (i) a lower... -
Holocene geology of central Africa
N° Outcrop: B000101. A typical profile showing from the bottom to the top: * The altered basement (Paleoproterozoic paragneisses); * The Stone Line; * The Cover... -
Holocene geology of central Africa
N° Outcrop: B000101. Detailed view of the Stone Line. Note the presence of jasper fragments in the upper left part of the photograph. -
Holocene geology of central Africa
N° Outcrop: B000101. Detailed view showing a well-rounded quartz pebble (upper centre). -
Holocene geology of central Africa
N° Outcrop: B000101. Same comment as preceding. Four samples have been collected in the Cover Horizon on this outcrop (plastic bags). -
Holocene geology of central Africa
N° Outcrop: B000101. Detailed view showing jasper fragments. Note the angular to more or less rounded shape of the quartz fragments. -
Holocene geology of central Africa
N° Outcrop: B000101. View of the Stone Line showing jasper fragments and well-rounded quartz pebble at all levels of the profile. -
Holocene geology of central Africa
N° Outcrop: B000102. General view of the point where the Stone Line becomes thick and stratified. -
Holocene geology of central Africa
N° Outcrop: B000102. View of the thick and stratified Stone Line with a very large rounded block of quartz toward its base. -
Holocene geology of central Africa
N° Outcrop: B000102. Walking toward the top of the Stone Line. On the right, a gentle slope leads to the top of a low hill ~ 40 m above the Ogooué river. -
Holocene geology of central Africa
N° Outcrop: B000102. View of quartz blocks of all sizes (Stone Line surface) covering the hill to the north side of the road, about 40 m above the Ogooué river. -
Holocene geology of central Africa
N° Outcrop: B000102. View of the landscape to the south of the BOO0102 outcrop showing unforested mountains of the Lopé - Okanda massif . In our back, the Ogooué...
