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Showing items 1 through 9 of 9.Desde el inicio de la ocupación española, el Camino del Sur, último tramo de una red a escala continental, constituyó la vía de comunicación entre la ciudad de Buenos Aires y el pago de la Magdalena a la vez que en sus proximidades se originaban incipientes núcleos urbanos.
Europe is characterized not only by large geomorphological variability but also by a long history of land use. This resulted in a highly variegated landscape.
To conserve and manage wetland resources, it is important to inventory and monitor wetlands and their adjacent uplands. Satellite remote sensing has several advantages for monitoring wetland resources, especially for large geographic areas.
Human-induced desertification in the Horqin sandy land in the north-eastern part of China has been reversed since the mid-1970s through re-vegetation. This land cover change affects surface energy and water transfer processes.
The United Nations Environment Programme (UNEP) has proposed methods and thematic areas for data collection that are appropriate to the evaluation of biodiversity. The Heritage Council has identified a paucity of data on habitats in Ireland.
Un mapa de deforestación del território mexicano, derivado de Ia sobreposición de dos cartografias de uso del suelo y vegetación de 1993 y 2000, se comparo con variables espaciales como el aislamiento (distancias a Ias carreteras y a Ias poblaciones), Ia topografia (altitud y pendiente), el tipo
A methodology is developed to relate urban growth studies to distributed hydrological modeling using an integrated approach of remote sensing and GIS. This linkage is possible because both studies share land-use and land-cover data.
This paper explores the possibility of using non-geometric cadastral maps from the 17th and 18th century together with aerial photographs from 1945 and 1981 to analyse land-cover change in south-east Sweden.
Counter intuition, an analysis of tree‐line position across the Swiss Alps based on a geographical information system (GIS) with a spatial resolution of 100 m (2.5 million points) revealed no difference in climatic tree‐line altitude with slope exposure.