Imposicions estructurals en el drenatge de la conca del riu Onyar (Girona)

The Onyar River basin is situated in the depression of la Selva. His origins are related to tectonic activity during Neogen in this region. In his evolution, we note a slowly and continuous downfall which directs the morphodinamical behaviour. In this sense, the drainage network has a directional trend towards the north, as consecuence of fault systems, and specially the N-S oriented one. A fault of this system has an important influence in the basin morphology, directs the drainage towards the north and avoids a closely drainage in the basin

Correlating Alpine glaciation with Adriatic sea-level changes through lake and alluvial stratigraphy

We compare lake and alluvial stratigraphy along a frame connecting the southern Alpine foothills and the Adriatic Sea, with the aim of matching the effects of Alpine glaciation and sea-level changes on sedimentation during the last glacial cycle. The palynostratigraphy of Lake Fimon provided proxies for regional vegetation and climate change and was coupled with sediment petrography, loss on ignition and magnetic susceptibility, disentangling alluvial phases from fluvioglacial activity related to culminations of the southeastern Alpine glaciers. The Fimon area was not reached by alluvial fans during the penultimate glacial maximum, nor by the sea transgression during the last interglacial, but a closed lake soon developed at the Eemian onset due to enhanced rainfall. Sea-level fall at glacial inception triggered the entrenchment of the drainage network in the plain reaching the outer Fimon Basin. Slow aggradation, but no sign of fluvioglacial activity, lasted to 38.2 +/- 1.45 cal. ka BP, when a major forest withdrawal took place, coeval to the spread of alluvial fans. By 27.5 perpendicular to 0.5 cal. ka BP the Fimon Basin was dammed by the Brenta outwash system. The main step of of forest recovery commenced at around (15.8) cal. ka BP, when apex trenching of the outwash fans was triggered by the glacier's decay. Copyright (C) 2011 John Wiley & Sons, Ltd.

Les “Millors famílies” de la Selva [Ressenya del llibre Notes de societat: La Selva 1768-1862, de Rosa Congost i Colomer]

Ressenya del llibre de Rosa Congost “Notes de societat”, interessant aportació al coneixement de les millors famílies de La Selva entre 1768 i 1862, entenent com a millors famílies les més benestants o amb major poder econòmic. L’estudi es fa a partir bàsicament de l’anàlisi sistemàtica de les dades del Registre d’Hipoteques

Planificació estratègica d’una xarxa de vies verdes a la comarca de la Selva

Les vies verdes són vies de comunicació autònomes reservades als desplaçaments no motoritzats. Per a la proposta de creació d’una xarxa per a la comarca de La Selva s’han utilitzat dues eines: els sistemes d’informació geogràfica i els seus indicadors complementaris, les quals han permès generar diversos possibles traçats, per triar una proposta final amb la seva valoració

La vegetació de la plana de la Selva

Article que estudia la vegetació i el clima de la comarca de la Selva (Catalunya)

La Selva, comarca de l'aigua

Parlar d’hidrografia a la comarca de la Selva és parlar del Ter i de la Tordera, dels dos cursos fluvials bàsics que estructuren la pràctica totalitat de la xarxa hídrica de la demarcació. Ambdós, amb les seves conques respectives, tenen un paper determinant a l’hora de definir les relacions que s’estableixen entre societat i medi. Tenint en compte aquest punt de partida, al llarg del text es farà una aproximació als aprofitaments i recursos que se n’obtenen, incidint sobretot en les seves singularitats. Pel cas del Ter el tema s’abordarà des de la perspectiva de la gran obra hidràulica ubicada dins els límits de la comarca, però tenint en compte que el seu abast transcendeix l’escala regional i que els recursos que proporciona, respecte a la Selva, són més de passada que d’estada. En canvi, quant a la Tordera, s’incidirà més com a conca, els recursos i explotació de la qual reverteixen de manera molt més directa dins la comarca i àrees veïnes com el Vallès Oriental i l’Alt Maresme. En darrer terme es farà esment d’algunes de les problemàtiques i contradiccions que comporta la gestió d’un recurs tan valuós com l’aigua

Aproximació a l'evolució del paisatge vegetal a les comarques de la Selva i del Vallès

L'objectiu d'aquest article és presentar les línies bàsiques de l'evolució del paisatge vegetal d'una part d'una àrea geogràfica que des de l'antiguitat ha estat un passadís històric d'assentaments i comunicacions i que comprèn les comarques de la Selva, del Vallès Oriental i del Vallès Occidental Biogeogràficament es tracta d'una zona de contacte entre el món mediterrani, representat a nivell climàtic per l'alzinar litoral, i l'eurosiberià, que té com a principals comunitats climàtiques la roureda de roure martinenc i la fageda amb el·lèbor verd

La Selva: una comarca singular per la seva heterogeneïtat

Sobre el creixement urbà, el desenvolupament i l'ordenació territorial de La Selva, comarca singular per la seva heterogeneïtat

Facies analysis of tertiary alluvial fan deposits in the Jundiai region, São Paulo, southeastern Brazil

This article presents an analysis of facies of sedimentary sequences that occur as discontinuous bodies in the Jundiai region, west of the main Tertiary continental basins of the southeastern Brazil continental rift. Nine identified sedimentary facies, grouped into four associations, suggest the existence of an ancient alluvial fan system whose source area was the Japi mountain range (Serra do Japi). The deposits are considered Tertiary in age and chronocorrelated with those identified in the Atibaia region and at other sites up to 100 km east and northeast of Jundiai. The depositional model adopted to explain the filling of the basin proposes that the alluvial fans, which directly derive from the source area, terminated in a braided channel longitudinal to the basin axis that flowed to northwest, in a similar configuration to that of the present day. This basin may have extended to the Atibaia region or formed a set of small basins laterally contiguous to the faults associated with the rift. Such occurrences show that the formation of rift basins was broader than the area presently occupied by the main deposits. (c) 2005 Elsevier Ltd. All rights reserved.

Hydrogeologic facies characterization of an alluvial fan near Fresno, California, using geophysical techniques /

Mode of access: Internet.

Contribution of geophysical surveys to groundwater modelling of a porous aquifer in semiarid Niger: An overview

Subsurface geophysical surveys were carried out using a large range of methods in an unconfined sandstone aquifer in semiarid south-western Niger for improving both the conceptual model of water flow through the unsaturated zone and the parameterization of numerical a groundwater model of the aquifer. Methods included: electromagnetic mapping, electrical resistivity tomography (ERT), resistivity logging, time domain electromagnetic sounding (TDEM), and magnetic resonance sounding (MRS). Analyses of electrical conductivities, complemented by geochemical measurements, allowed us to identify preferential pathways for infiltration and drainage beneath gullies and alluvial fans. The mean water content estimated by MRS (13%) was used for computing the regional groundwater recharge from long-term change in the water table. The ranges in permeability and water content obtained with MRS allowed a reduction of the degree of freedom of aquifer parameters used in groundwater modelling.

Glacial to paraglacial history and forest recovery in the Oglio glacier system (Italian Alps) between 26 and 15 ka cal BP

The integrated stratigraphic, radiocarbon and palynological record from an end-moraine system of the Oglio valley glacier (Italian Alps), propagating a lobe upstream in a lateral reach, provided evidence for a complete cycle of glacial advance, culmination and withdrawal during the Last Glacial Maximum and early Lateglacial. The glacier culminated in the end moraine shortly after 25.8 +/- 0.8 ka cal BP, and cleared the valley floor 18.3-17.2 +/- 0.3 ka cal BP. A primary paraglacial phase is then recorded by fast progradation of the valley floor.

As early as 16.7 +/- 0.3 ka cal BP, early stabilization of alluvial fans and lake filling promoted expansion of cembran pine. This is an unprecedented evidence of direct tree response to depletion of paraglacial activity during the early Lateglacial, and also documents the cembran pine survival in the mountain belt of the Italian Alps during the last glaciation. Between 16.1 and 14.6 +/- 0.5 ka cal BP, debris cones emplacement points to a moisture increase favouring tree Betula and Pinus sylvestris-mugo. A climate perturbation renewed paraglacial activity. According to cosmogenic ages on glacial deposits and AMS radiocarbon ages from lake records in South-Eastern Alps such phase compares favourably with the Gschnitz stadial and with the oscillations recorded at lakes Ragogna. Langsee and Jeserzersee, most probably forced by the latest freshening phases of the Heinrich Event 1.

A further sharp pine rise marks the subsequent onset of Bolling interstadial. The chronology of the Oglio glacier compares closely with major piedmont glaciers on the Central and Eastern Alpine forelands. On the other hand, the results of the present study imply a chronostratigraphic re-assessment of the recent geological mapping of the Central Italian Alps. (C) 2012 Elsevier Ltd. All rights reserved.

Assinatura tectono-sedimentar do auge da compressão bética em Portugal: a descontinuidade sedimentar Valesiano terminal-Turoliano

An Upper Miocene important sedimentary break can be accurately recognised in the Portuguese basins and is reflected by a drastic palaeogeographic change in relation to a large-scale tectonic event of probable uppermost Vallesian-Turolian (9,5 Ma; middle Tortonian) age. The characterisation of the sedimentary record of this tectonic event, as well as its relations with interpreted active faults is made for different situations: Douro (NW border), Mondego, Lower-Tagus and Sado Tertiary basins. The sedimentary record, considered upper Tortonian-Messinian ? (uppermost Vallesian-Turolian ?) is interpreted mainly as endorheic alluvial fans (internal drainage), developed along active NNE-SSW indent-linked strike-slip faults and NE-SW reverse faults. At NE Portugal, proximal fluvial systems of an endorheic hydrographic network drained eastwards to the Spanish Duero interior Basin. The main evidences of the betic compression clímax in Portugal mainland are presented; the interpreted active tectonic structures are in accordance with an intense NNW-SSE crustal shortening, but some regional differences are also documented.

Les colònies d'estiuejants (1865-1936)

Article dedicat a les colònies d'estiuejants de final del segle XIX i primeres dècades del XX a la comarca de la Selva

Els roders de les Guilleries [Ressenya del llibre El sindicalisme forestal dins del moviment obrer català: els roders de Roger Zamorano]

Ressenya del llibre 'El sindicalisme forestal dins del moviment obrer català: els roders' de Roger Zamorano, publicat l' any 2000 pel Museu Etnològic del Montseny. Estudi que reconstrueix la trajectòria del moviment associatiu dels roders de la comarca de la Selva (interior) des de final del segle XIX fins a la Guerra Civil del 1936 en base documentació escrita o oral