Castelo Branco em 1883. A estrutura profissional de uma pequena cidade interior Castelo Branco en 1883. Structure professionnelle d'une petite ville de l'intérieur
An interpretation of the 1883 cataclysmic eruption of Krakatau from geochemical studies on the partial melting of granite
The subject of this paper, derived from cooperative research carried out to date, in particular consists of a geochemical comparison between the 1883 Krakatau pumice flow and the so called « Shirasu » pumice flows prevailing over South Kyushu, Japan
100 let so dnja rozdenija akademika A.A. Grigor'eva (1883-1968). (A l'occasion du 100 anniversaire de la naissance de l'académicien A. A. Grigor'ev (1883-1968))
(1883-1981) ; France ; Géographie physique ; Hiver ; Lorraine ; Meurthe-et-Moselle ; Nancy ; Neige ; Précipitation ; Série chronologique ; Type de temps
Study of the number of days with snowfall, recorded between 1883 and 1981 in Nancy: 1. Monthly frequential analysis| 2. Multiple linear regression to explain the frequency of snowfalls or the number of days with steady snowcover, based
Settlement patterns on the Mescalero Apache reservation since 1883
Cinq périodes de la politique fédérale depuis 1883 sont le cadre pour identifier et analyser les éléments géographiques de l'évolution du système de peuplement apache de Mescalero, Nouveau Mexique. Actuellement, le maintien de la culture
Post-1883 ash fall on Panjang and Sertung and its ecological impact
This paper describes the post-1883 history of volcanic disturbance to the islands Panjang and Sertung, within the Krakatau group, Indonesia. The results of analyses of chemical, physical and particularly of mineral magnetic properties are presented
Re-assessment of the monthly naturalized flow record for the River Thames at Kingston since 1883, and the implications for the relative severity of historical droughts
A rainfall-streamflow modelling methodology is applied to the monthly flow record for the Thames at Kingston, one of the most important long records of river flow, from 1883. The results confirm that low flows during droughts before about 1950 have