This article presents the results of a study carried out in the Puck Bay concerning the alterations of pore water chlorinity, pore water (O 18, D) isotope composition and near-bottom water salinity caused by groundwater seepage. The groundwater
seepage decreases the chlorinity of interstitial water and the salinity of near-bottom water. The comparison of the oxygen and hydrogen isotope composition of underground, interstitial and near-bottom waters indicated a reduction of the content of heavy
late Cenozoic landform development in East Africa: the role of near base level planation within the dynamic etchplanation concept
near base level. It is therefore proposed to elaborate the etchplanation concept with fluvial dynamics. Late Cenozoic planation events in East Africa were triggered by a major base level rise due to the combined effects of eustatic sea level rise
The Quaternary sediments exposed on the banks of the river Aner which is a tributary of the river Tapti, near Piloda (district Dhule), western India, reveal 3 channel-fill structures, spatially at the same level. The AA. therefore present here
Peasants in the Tahuayo River basin near Iquitos, Peru earn cash incomes from swidden fallow, agroforestry, floodplain agriculture, fishing, livestock production, hunting and extracting rainforest products. Gross returns per hectares were highest
This paper compares the climates of wine growing areas in Central Europe and New Zealand, especially those that prevail near to the latitudinal limit. The southern limit of grape growing in New Zealand may be 45°S, european experience shows a limit
Five pre-Illinoian tills are recognized and named informally in northern Missouri, near the southernmost margin of the pre-Illinoian Laurentide ice sheet. The resolution of the stratigraphy of these pre-Illinoian tills in Missouri is needed
Tsunami magnitudes on the Imamura-Lida scale are investigated by the author's method (Hatori 1979, 1986) using the data of inundation heights near the source area and tide-gauge records observed in Japan. The regional characteristic of tsunami
of depositional processes on the morphologic characteristics of debris flow fans is studied through depositional model experiments. These experiments were conducted near a debris flow gully just after debris flows took place.
This study focuses on the rock crust that occurs in sheltered areas in the limestone cliffs along the lower Pecos River, the Rio Grande near the Pecos confluence, and canyon tributaries of the two rivers. A preliminary paleoclimate reconstruction