Late Wisconsin groundwater discharge environments of the southwestern Indian Springs Valley, southern Nevada
This report presents the results of a comparative study of the sedimentologic and faunal evidence from late Wisconsin sediments in the Indian Springs Valley and existing groundwater discharge environments of the Steptoe and Butte Valleys
Dutch Catholic immigrant settlement in Wisconsin, 1850-1905.
Assimilation ; Culturel ; Etats-Unis ; Fox River Valley ; Green Bay ; Groupe ethnique ; Géographie de l'Amérique ; Géographie historique ; Identité culturelle ; Immigration ; Intégration sociale ; Néerlandais ; Religion ; Wisconsin
An historical geography of the immigration of Dutch from the Noord-Brabant municipalities of Uden, Zeeland and Boekel to the Green Bay-Fox River Valley area of northeastern Wisconsin. The Dutch part of their heritage rapidly assimilated
Corrélation négative hautement significative entre le nombre de décès par infarctus du myocarde (surtout chez l'homme de plus de 60 ans) et la température moyenne journalière. Exemple du Wisconsin. - (JPB)
Culturel ; Etats-Unis ; Exploitation agricole ; Ferme laitière ; Finlandais ; Finnois ; Groupe ethnique ; Géographie culturelle ; Géographie de l'Amérique ; Lake Superior region ; Michigan ; Minnesota ; Peuplement ; Peuplement rural ; Wisconsin
The Finns who immigrated to the northern parts of Minnesota, Wisconsin and Michigan built hay barns of logs in which hay was stored in much the same way as those in Finland. In a second stage, those Finnish Americans who later became commercial
En examinant les indicateurs du passage des glaciers dans la péninsule de Bonavista située au nord-est de Terre-Neuve, cet article décrit les deux styles de glaciation à l'oeuvre dans cette région. La limite extrême des glaciers du Wisconsin est
. Tills in the headwaters region of the ancient Mississippi drainage system in Minnesota and Wisconsin occur in the appropriate stratigraphic position and have colors and mineralogic compositions that suggest they could be the parent till of the Roxana.
that the Beardmore drift limit is late Wisconsin (isotope stage 2) and the Meyer limit Stage 6 in age. The Beardmore and Meyer drift sheets represent thickening of the Beardmore Glacier in response to Ross Ice Shelf grounding during the last two global glaciations
Glacier have thickened considerably during the last two global glaciations (late Wisconsin and marine isotope stage 6). The effect of ice-shelf grounding probably was the major control of these changes of Hatherton Glacier. Holocene ice-surface lowering
and a very thin layer of sediment over crystalline basement or older sediments. A reconstruction of the glacial history of Marguerite Bay since the last glacial maximum shows grounded ice filling the bay in late Wisconsin time. Rising sea level caused