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The study area consists of Flanders, which is the northern, Dutch-speaking regiof of Belgium.
The study area consists mostly of dense residential and industrial spaces.
The study area consists of 14 municipalities within the Vanajavesi catchment area located in Southern Finland.
The study area consists of limestone and marls-sandstone (flysch) patches.
The lithology of the study area consists of Late Cretaceous-aged sedimentary rocks, known as the Catak and Esiroglu formations, and the Late Cretaceous-aged Kackar Rhyodacite.
The study area consists of the Bykovsky Peninsula and the adjacent Khorogor Valley in the Kharaulakh Ridge situated a few kilometres southeast of the Lena Delta.
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The study area consisted of nine 300-ha pastures at a range of stocking rates, from very low to very high for the region.
The study area consisted of four contiguous agricultural sub-areas with a decreasing degree of intensification: irrigated, mixed (dry and irrigated), dry and environmentally protected (i.e. Special Protection Area, SPA) dry farmland.
The study area consisted of eight farms located within the Paraíba Valley in the state of São Paulo, Brazil (Fig. 1).
The study area consisted of 73 ha in the core zone, 115 ha in the buffer zone and 22 ha in the restoration zone.
Sedimentary rocks in the study area consist of dark conglomerate, sandstone, shale, limestone, dolomite and gypsum beds ranging from 4.5 to 1735.5 m in thickness.
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