Biographical Memoir of Arnold Guyot
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Appendix 2. the Mystery of Guyot Formation and Sinking
Appendix 2 The Mystery of Guyot Formation and Sinking Origin of Guyots Unknown In 1946, geologist Harry Hess was the first geologist to describe guyots (flat-topped seamount).1 Since then, the number of guyots has become numerous. Resolution Guyot in the Mid-Pacific Mountains that was studied in the 1990s by the Deep Sea Drilling Project2 is a typical guyot. Figure A2.1 shows the silhouette. Ever since Hess’s time, the cause of the flat top has eluded explanation.3 Winterer and Met- Figure A2.1. Silhouette of Resolution Guyot zler maintain: “Since Hess first recognized them in the Mid-Pacific Mountains (drawn by Mrs. Melanie Richard). in 1946, the origin of flat-topped seamounts, or guyots, has remained one of the most persistent problems in marine geology.”4 Since guyots are believed to have been truncated near sea level, there are two suggested subsid- ence mechanisms used to explain why they are now found well below sea level. But some guyots must have become flat well below sea level. Not All Guyots Eroded At Sea Level Many scientists have simply assumed that the flat top of a guyot was eroded at or near sea level.5,6 ‘This has been challenged by a few marine geologists.’7,8 For instance, a number of guyots near the East Pacific Rise have been attributed to the infilling of calderas by small lava flows well below sea level.9,10,11,12 “But, these guyots are small 1 Hess, H.H., 1946. Drowned ancient islands of the Pacific Basin. American Journal of Science 244:772–791. -
Influence of Sediment Transport on Short-Term Recolonization by Seamount Infauna
MARINE ECO'R'OGY PROGRESS SERIES Vol. 123: 163-175,1995 Mu Published July 20 Ecol Prog Ser / Influence of sediment transport on short-term recolonization by seamount infauna Lisa A. Levin, Claudio DiBacco Marine Life Research Group, Scripps Instituliar of Oceanography, La Jolla, California 92093-0218, USA ABSTRACT: Rates and mechanisms of mEa'nnal recolonization in contrasting sediment transport regimes were examined by deploying hydrodynamically unbiased colonization trays at 2 sites -2 km apart on the flat summit plain of Fieberhg Cplyot in the eastern Pacific Ocean. Both study sites expe- rienced strong bottom currents and high shear velocity (U. exceeding 1.0 cm S-' daily). Macrofaunal recolonization of defaunated sediments on Werling Guyot was slow relative to observations in shal- low-water sediments, but rapid compared l&other unennched deep-sea treatments. Microbial colo- nization was slower but macrofaunal colon~isnwas faster at White Sand Swale (WSS, 585 m),where rippled foraminiferal sands migrate daily, than at Sea Pen Rim (SPR, 635 m), where the basaltic sands move infrequently. Total densities of macroiannal colonizers at WSS were 31 and 75% of ambient after 7 wk and 6.4 mo, respectively; at SPR they were 6 and 49% of ambient, respectively. Over % of the colonists were polychaetes (predominantly ksionids and dorvilleids) and aplacophoran molluscs. Species richness of colonizers was comparab.lle at SPR and WSS and did not differ substantially from ambient. Most of the species (91%) and indmduals (95%) recovered in colonization trays were taxa present in background cores. However, only 25% of the taxa colonizing tray sediments occurred in trays at both WSS and SPR. -
Aspiservices
Impressum Editeur: Val-de-Ruz Info, CP, 2053 Cernier Présidente de la coopérative: Claire Wermeille, 032 853 10 21 Rédaction: Claire Wiget, 079 285 25 41 Secrétariat: Bernadette Jordan, 032 853 70 64 Publicité: Yossi Belleli, 076 412 72 05, [email protected] No 86 - 5 juin 2014 Pour les questions administratives, commerciales et rédactionnelles: [email protected] Internet: www.valderuzinfo.ch Impression: Val Impressions, Cernier Tirage: 8’400 exemplaires Distribution bimensuelle: Dans tous les ménages du Val-de-Ruz IBAN: CH34 8025 1000 0029 0688 4 Prochaine parution: le jeudi 19 juin 2014 sommaIre 2 Votre commune vous informe 3 Bibliothèque des jeunes 3 Grange aux concerts 3 APSSA 3 petites annonces 3 mélanie salomon 5 Fondation Borel 5 ZI Fontaines 5 Dons pour l’équithérapie 7 agenda 7 résultats sportifs Village de Fenin et Creux du Van. (photo fc) 7 La 8ORCH1 8 armand Blaser CHemIns CHouettes: deux nouveaux mini-guides pour découvrir le Val-de-ruz Espace Val-de-Ruz continue d’étoffer son offre de Chemins Chouettes. Deux Aspiservices nouveaux mini-guides sont à disposition Vente - Réparations - Electroménagers auprès des guichets de l’administration communale à Cernier et aux Geneveys- 079 469 41 50 sur-Coffrane, ainsi qu’à Evologia. Sus-Pont 2b - 2046 Fontaines Le Chemin Chouette numéro 4 intitulé «La lisière» emmène les promeneurs des Hauts-Geneveys à Dombresson en Un service rapide près de chez vous passant par Fontainemelon, Cernier et Chézard-Saint-Martin. Le Chemin Chouette numéro 5 s’appelle «Par la Rincieure» et conduit les mar- cheurs de Villiers à Chézard par Sous-le- Mont, Savagnier et la Rincieure. -
Abyssal Hills: Influence of Topography on Benthic Foraminiferal Assemblages ⇑ Paris V
Progress in Oceanography 148 (2016) 44–55 Contents lists available at ScienceDirect Progress in Oceanography journal homepage: www.elsevier.com/locate/pocean Abyssal hills: Influence of topography on benthic foraminiferal assemblages ⇑ Paris V. Stefanoudis b, , Brian J. Bett a, Andrew J. Gooday a a National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, United Kingdom b Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, United Kingdom article info abstract Article history: Abyssal plains, often thought of as vast flat areas, encompass a variety of terrains including abyssal hills, Received 8 February 2016 features that constitute the single largest landscape type on Earth. The potential influence on deep-sea Received in revised form 12 September benthic faunas of mesoscale habitat complexity arising from the presence of abyssal hills is still poorly 2016 understood. To address this issue we focus on benthic foraminifera (testate protists) in the >150-lm frac- Accepted 28 September 2016 tion of Megacorer samples (0–1 cm layer) collected at five different sites in the area of the Porcupine Available online 29 September 2016 Abyssal Plain Sustained Observatory (NE Atlantic, 4850 m water depth). Three sites are located on the tops of small abyssal hills (200–500 m elevation) and two on the adjacent abyssal plain. We examined Keywords: benthic foraminiferal assemblage characteristics (standing stock, diversity, composition) in relation to Deep-sea diversity Foraminifera seafloor topography (hills vs. plain). Density and rarefied diversity were not significantly different Mesoscale between the hills and the plain. -
422 423 Samedi Du 01.03.2021 Au 31.10.2021
transN SA Projet horaire 2021 Ligne 422/423 Samedi_Rempl_CFF_JOURNALIER 22.04.20 15:41:13 Période du 01.03.2021 au 31.10.2021 5 6 7 8 VDR Les Bugnenets VDR Le Pâquier Village 14 44 14 44 14 44 Villiers, centre 14 40 10 40 10 40 VDR Dombresson Collège 33 03 33 03 33 Chézard, St-Martin 19 49 19 49 19 49 Savagnier, Petit-Savagnier Engollon, village Chézard-St-Mar, Grand-Chézard Neuchâtel, Trois-Chênes 28 58 28 58 28 58 25 55 25 29 55 59 25 29 55 59 Cernier, Centre 29 28 29 56 59 59 24 26 29 56 57 59 24 26 29 55 56 59 29 59 VDR La Fontenelle VDR Dépôt dece dece dece Autobus articulé régional Autobus articulé régional Autobus articulé régional VDR Sous l’Usine 1701 1702 1704 dece VDR Le District Autobus articulé régional 1703 Les Hauts-Geneveys, Gare 51 21 51 21 51 VDR Boudevilliers Centre VDR Landeyeux VDR Valangin Centre Neuchâtel, Gare (Nord) 48 18 48 18 48 Neuchâtel, Place Pury 05 35 05 35 Neuchâtel, Université Neuchâtel, Riveraine 8 9 10 11 Les Bugnenets Le Pâquier Village 14 44 14 44 14 44 Villiers, centre 10 40 10 40 10 40 Dombresson, Collège 03 33 03 33 03 33 St-Martin 19 49 19 49 19 49 Petit-Savagnier 40 Engollon, village Grand-Chézard Trois-Chênes 28 58 28 45 58 28 58 25 29 55 59 25 29 45 55 59 25 29 55 59 Cernier, Centre 24 26 29 55 56 59 24 26 29 35 55 56 59 24 26 29 55 56 59 35 La Fontenelle Dépôt Cernier dece dece Minibus régional Minibus régional Sous l’Usine 1706 1706 Le District Les Hauts-Geneveys, Gare Boudevilliers Centre 21 51 21 51 21 51 Landeyeux Valangin Centre Neuchâtel, Gare (Nord) 18 48 18 48 18 48 Neuchâtel, Place -
Submarine Mountain Named for William Laurence Dowd
Submarine mountain named for William Laurence Dowd June 25, 1965 A major submarine mountain discovered in the Eastern Pacific Ocean by scientists from the Scripps Institution of Oceanography has been named by the scientists in honor of William Laurence Dowd, a Scripps graduate student who was found slain in his apartment June 6. The seamount, to be known as Dowd Guyot, is located about 1,000 miles south of San Diego and about 1,000 miles west of Mexico. It was discovered June 22 by scientists aboard the Scripps research ship Argo operating on a student cruise for the Department of Earth Sciences under the direction of Dr. Manuel N. Bass, Assistant Professor of Geology. Dowd, a brilliant graduate student in the field of geochemistry research, took part in a similar cruise last year and had, in fact, sailed just east of the region where the seamount was discovered. The current student cruise, which left San Diego June 17, marks the first time Argo has put out to sea since the tragedy occurred. According to Dr. Henry W. Menard, Professor of Geology, who received word of the discovery by radio from Dr. Bass, the mountain is a flat topped seamount, or guyot, which probably was an island thousands of years ago. Its top is four miles in diameter and from 280 to 290 fathoms beneath the surface of the ocean. It has a narrow central pinnacle, the top of which is 257 fathoms beneath the surface. The base of the seamount is about 19 miles in diameter at a depth of 2,250 fathoms giving the mountain a height of about 12,000 feet or nearly two nautical miles. -
Cretaceous and Paleogene Manganese-Encrusted Hardgrounds from Central Pacific Guyots
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 1995 Cretaceous and Paleogene Manganese-Encrusted Hardgrounds from Central Pacific Guyots David K. Watkins University of Nebraska-Lincoln, [email protected] Isabella Premoli Silva Università degli Studi di Milano Elisabetta Erba Università degli Studi di Milano, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Watkins, David K.; Silva, Isabella Premoli; and Erba, Elisabetta, "Cretaceous and Paleogene Manganese- Encrusted Hardgrounds from Central Pacific Guyots" (1995). Papers in the Earth and Atmospheric Sciences. 221. https://digitalcommons.unl.edu/geosciencefacpub/221 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Haggerty, J.A., Premoli Silva, I., Rack, F., and McNutt, M.K. (Eds.), 1995 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 144 5. CRETACEOUS AND PALEOGENE MANGANESE-ENCRUSTED HARDGROUNDS FROM CENTRAL PACIFIC GUYOTS1 David K. Watkins,2 Isabella Premoli Silva,3 and Elisabetta Erba3 ABSTRACT Manganese-encrusted hardgrounds and associated sediments from four guyots in the western Pacific Ocean were investigated using lithostratigraphic and biostratigraphic examination of thin sections. Biostratigraphic data from manganese-encrusted hard- grounds constrain the age of platform drowning to early middle Eocene for Limalok Guyot, latest Maastrichtian to early Paleocene for Wodejebato Guyot, and middle late Albian for MIT Guyot. -
Convention De Fusion Des Communes De Boudevilliers, De Cernier, De
CONVENTION DE FUSION Convention de fusion des communes de Boudevilliers, de Cernier, de Chézard-Saint-Martin, de Coffrane, de Dombresson, d'Engollon, de Fenin- Vilars-Saules, de Fontainemelon, de Fontaines, des Geneveys-sur- Coffrane, des Hauts-Geneveys, de Montmollin, du Pâquier, de Savagnier et de Villiers CONVENTION DE FUSION Préambule Convaincus que la collaboration intercommunale menée jusqu'à ce jour par les communes du Val-de-Ruz est à la base du présent projet de fusion et qu'en ce sens le passé conduit l'avenir; Convaincus que l'amélioration de cette collaboration ne peut être atteinte avec une augmen- tation du nombre d'entités intercommunales, sous peine de réduire à néant l'autonomie communale; Convaincus qu'il est préférable de prendre leur destin en mains que d'attendre que les autres décident à leur place; Convaincus que le projet de société est l'expression des forces de la région et qu'à ce titre, il constitue le socle du rapprochement des quinze communes; Convaincus que le regroupement par la fusion saura mieux répondre aux attentes nombreu- ses et légitimes des habitants de cette région; Convaincus que l'accroissement de la position de la région du Val-de-Ruz sur l'échiquier poli- tique cantonal passe par une fusion des communes et que le moment est propice; Souhaitant offrir à la population des conditions cadre pour mieux affronter les défis de de- main; Les Conseils généraux de Boudevilliers, de Cernier, de Chézard-Saint-Martin, de Coffrane, de Dombresson, d'Engollon, de Fenin-Vilars-Saules, de Fontainemelon, de Fontaines, des Gene- veys-sur-Coffrane, des Hauts-Geneveys, de Montmollin, du Pâquier, de Savagnier et de Vil- liers, sur proposition de leur Conseil communal, soumettent la présente convention au vote de la population. -
PLAN DE RÉSEAU [email protected] | 032 924 25 26 |
PLAN DE RÉSEAU [email protected] | 032 924 25 26 | www.transn.ch Lac des Brenets Le Doubs Le Doubs Camping Douane Les Pommerats 385 22.132Goumois Parc Les Planchettes zone La Rasse des Pargots La Maison-Monsieur, Bif. Village Centre village 371 Biaufond, Centre sportif 21 Douane Tournant Theusseret Grande Rue 27 Bas du village Gare Les Joux-Derrière, Les Joux-Derrière, Les Joux-Derrière, Les Joux-Derrière, Biaufond, Les Avants Belfond 385 Village Sur-le-Ring Le Dazenet La Grébille restaurant 44 anc. collège Les Brenets Les 371 Les Brenets Brenetets zone 224 Pâquerettes 42 zone Point-du-Jour Swin Golf Le Graiteux La Chaux-de-Fonds Saignelégier 20 Rte de France Recorne Plaisance 310 Sombaille Montbrillant Électrices 22 Cantons Le Noirmont Saignelégier Vers Glovelier 236 301 Bassets-Croisée 237 Chapeau-Rablé Tête-de-Ran er zone Les Emibois Muriaux 1 Août Gare Les Frêtes Lycée Le Creux-des-Biches Vers Tramelan Malpierres Tilleuls Jolimont Collège Monts 31 Petits-Monts zone Blaise-Cendrars Succès Villa TurquePouillerel Tourelles Signal Les Breuleux-Eglise 341 Breguet 20 Bif, Bul-Va Les Breuleux zone Arc-en-ciel Nord Le Boéchet Gare 237 Tricentenaire Vers Tramelan Hôpital 22.131 La Chaux-des-Breuleux 21 Citadelle Bel-Air Chasseral Hôpital Les Breuleux Vers Morteau, Le Locle 304 Gare Bois du Combettes Le Chalet Le Locle 304 Est Besançon 224 Numaga Cernil-AntoineAmi-Girard Fusion Abeille Petit Château Stavay-Mollondin 223 223 Les Bois La Chaux-de-Fonds Bif. Les Cerneux Moulins souterrains Col-des-Roches Jura Vers Saint-Imier, Tramelan Paix Bibliothèque -
2. the D'entrecasteaux Zone—New Hebrides
Collot, J.-Y., Greene, H. G., Stokking, L. B., et al., 1992 Proceedings of the Ocean Drilling Program, Initial Reports, Vol. 134 2. THE D'ENTRECASTEAUX ZONE-NEW HEBRIDES ISLAND ARC COLLISION ZONE: AN OVERVIEW1 J.-Y. Collot2 and M. A. Fisher3 ABSTRACT The <TEntrecasteaux Zone, encompassing the North d'Entrecasteaux Ridge and the Bougainville Guyot, collide with the central New Hebrides Island Arc. The d'Entrecasteaux Zone trends slightly oblique to the 10-cm/yr relative direction of plate motion so that the ridge and the guyot scrape slowly (2.5 cm/yr) north, parallel to the trench. The North d'Entrecasteaux Ridge consists of Paleogene mid-ocean ridge basalt basement and Pliocene to Pleistocene sediment. The Bougainville Guyot is an andesitic, middle Eocene volcano capped with upper Oligocene to lower Miocene and Miocene to Pliocene lagoonal limestones. Geophysical and geologic data collected prior to Leg 134 indicate that the two collision zones differ in morphology and structure. The North d'Entrecasteaux Ridge extends, with a gentle dip, for at least 15 km eastward beneath the arc slope and has produced a broad (20-30 km), strongly uplifted area (possibly by 1500-2500 m) that culminates at the Wousi Bank. This tectonic pattern is further complicated by the sweeping of the ridge along the trench, which has produced a lobate structure formed by strike-slip and thrust faults as well as massive slumps north of the ridge. South of the ridge, the sweeping has formed large normal faults and slump scars that suggest collapse of arc-slope rocks left in the wake of the ridge. -
Qualité De L'eau 2018 Val-De-Ruz
QUALITE DE VOTRE EAU POTABLE Commune de Val-de-Ruz Qualité de l’eau L’eau du réseau de Val-de-Ruz est bien minéralisée. C’est une eau mi-dure à dure, en fonction de la ressource, char- gée en hydrogénocarbonates, calcique, sulfatée et en partie influencée par l’agriculture, car les teneurs en nitrates 2018 ont varié de 1 à 20.2 mg/L en 2018. Provenance Eau des sources et des puits des villages (69.9% en 2018), avec une partie fournie par des tiers (30.1% en 2018). Traitement Par rayonnement UV - Coffrane, Les Geneveys-sur-Coffrane, Montmollin, Boudevilliers, Malvilliers, Fontaines, Engollon, La Joux-du-Plâne. Par chloration: Cernier, Chézard-Saint-Martin, Dombresson, Villiers, Savagnier, Fenin, Vilars, Saules, Fontaines, Engollon, Fontainemelon, Les Hauts-Geneveys. Appoint et secours : Eau du SIVAMO, du SECH, de Neuchâtel et de Rochefort: par chloration. Qualité micro- Sur les 206 échantillons analysés, 4 dépassements de la valeur maximale (DVM) pour des germes aérobies mésophiles biologique et (norme de 300 UFC/ml) et 3 DVM pour la turbidité (valeur maximale de 1 FNU) ont été enregistrés. En dehors de ces chimique non-conformités sans danger pour la santé des consommateurs, la qualité de l’eau du réseau de Val-de-Ruz a globalement respecté les exigences légales en 2018. Le puits du Lion n’a pas été utilisé en raison d’un DVM pour les nitrates. de se l’e ly a a u Micropolluants Des recherches de micropolluants, parmi lesquels des pesticides et des résidus médicamenteux, ont été effectuées en n 26.06.2018 d A u juillet 2018 dans les eaux brutes. -
Subduction Zones
AccessScience from McGraw-Hill Education Page 1 of 11 www.accessscience.com Subduction zones Contributed by: R. J. Stern, S. H. Bloomer Publication year: 2019 Regions where portions of the Earth’s tectonic plates sink beneath other plates, into the Earth’s interior. Subduction zones are defined by deep oceanic trenches, lines of volcanoes parallel to the trenches and zones of large earthquakes that extend from the trenches landward. Plate tectonic theory recognizes that the Earth’s solid surface is composed of a mosaic of interacting lithospheric plates, with the lithosphere consisting of the crust (continental or oceanic) and associated underlying mantle, for a total thickness that varies with age but that is typically about 100 km (60 mi). Oceanic lithosphere is created by seafloor spreading at mid-ocean ridges (divergent, or accretionary, plate boundaries) and destroyed at subduction zones (at convergent, or destructive, plate boundaries). At subduction zones, the oceanic lithosphere dives beneath another plate, which may be either oceanic or continental. Part of the material on the subducted plate is recycled back to the surface (by being scraped off the subducting plate and accreted to the overriding plate, or by melting and rising as magma) and the remainder is mixed back into the Earth’s deeper mantle. This process balances the creation of lithosphere that occurs at the mid-ocean ridge system. The convergence of two plates occurs at rates of 1–10 cm∕yr (0.4–4 in.∕yr) or 10–100 km (6–60 mi) per million years (Fig. 1). During subduction, stress and phase changes in the upper part of the cold descending plate produce earthquakes in the upper portion of the plate, in a narrow band called the Wadati-Benioff zone (named after the Japanese and U.S.