Solr Search · GéoProdig, portail d'information géographique

weathering reported in this study itself offers possibilities for a new method of phytometric dating for very young rock surfaces.
2008

of senior citizens opens chances for such structurally weak regions which are characterized by net out-migration of younger groups of people. - (IfL)
2008

Education ; Educational level ; France ; Higher education ; Schooling ; Social inequality ; Young people
2008

. Their origin could only be wind or waves driven. Although many chevrons resemble narrow parabolic coastal dunes, a young aeolian genesis can be excluded where orientation contradicts main wind direction, or where no beach or sand deposit exists. Where storm
2008

The apatite fission track and apatite (U-Th)/He data measured on teschenite intrusions show that planation surfaces in the study area formed in post-Pannonian time and are therfore younger than traditionally believed. This contradicts the classical
2008

Geographies of children and youth

Children ; Cognitive space ; Daily life ; Identity ; Mobility ; Place ; Policy ; Production of space ; Residential environment ; Society ; Street ; Young people
2008

The paper features some recent results on the Young Quaternary floodplain development in the middle to lower catchment of the Komadugu Yobe, a main northeast-Nigerian tributary to Lake Chad. The major aim of the study was the reconstruction
2008

Behaviour ; British people ; Identity ; Journey ; Modernism ; Post-modernism ; Project ; Risk ; Third World ; Tourism ; Young people
2008

there - at least from dusk till dawn. The article analyses how child-headed households make their living in such an environment. The livelihood approach is used to identify the young people´s assents and vulnerability. The results give an insight into the country´s
2008

Attendance ; Enquiry ; France ; Ile-de-France ; Neighbourhood ; Paris ; Perception ; Place ; Public policy ; Town ; Young people
2008

Geomorphology of Pohorje mountains

The Pohorje mountain range, young mountains with prevailing metamorphic rocks and dacite, continues to uplift above the igneous laccolith in the area of the rapid rising asthenosphere in the transition to the Pannonian basin also due to changes
2008

of the Holocene is not closed. OLIVEIRA et al. (2008-this issue) attributes the variability in the stratigraphy of near-valley head deposits (including the Holocene) to climatic forcing. The archaeological site of Axum offers the opportunity to link human
activities such as ploughing and the induced soil loss (CIAMPALINI et al., 2008), to the age of human occupation and the land-use changes that have occurred ever since (SCHMID et al., 2008). Here, VAN DE WAUW et al. (2008)) could also demonstrate
that the current soilscape has not much in common with the soilscape before agriculture started, as it is governed by the presence of deeply eroded soil profiles and thick colluvial deposits which result in the presence of young soils in most places. One
of the major processes resulting in this rejuvenation of parent material in many tropical areas is the presence of ancient and active lanslide bodies (MOEYERSONS et al., 2008). TURKELBOOM et al. (2008) demonstrate the negative impacts of current land-use
intensification on the natural hydrological equilibrium. In contrast to this is the situation in north Ethiopia, where MUNRO et al.(2008) with repeat photography over a period of 30 years found decreased soil loss rates, which they link to the introduction of soil
2008

Résultats de la recherche (33 résultats)