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Wanzele
Lede () is a Municipalities of Belgium, municipality in the Belgium, Belgian province of East Flanders, in the Denderstreek near the cities of Ghent, Aalst, Belgium, Aalst and Dendermonde. In 2011, Lede had a population of 17,882 and area of 29.69 km², a population density of 575 inhabitants per km². The current mayor of Lede is Geertrui Van de Velde (Christen-Democratisch en Vlaams, CD&V). Geography The municipality comprises the deelgemeente, sub-municipalities of Impe, Lede proper, Oordegem, Smetlede, Wanzele, and the hamlet of Papegem. All the sub-municipalities and also the hamlet are crossed by the Molenbeek (Erpe-Mere Bovenschelde), Molenbeek. Sandstone The Lede Formation ( nl, Formatie van Lede; abbreviation: Ld) is a formation (stratigraphy), geologic formation in the Subsurface (geology), subsurface of Belgium. The formation is named after Lede. It consists of shallow-marine limestone and sandstone, deposited in the former sea that covered Belgium during the E ...
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Impe Lede Oordegem Papegem Smetlede Wanzele
Lede () is a municipality in the Belgian province of East Flanders, in the Denderstreek near the cities of Ghent, Aalst and Dendermonde. In 2011, Lede had a population of 17,882 and area of 29.69 km², a population density of 575 inhabitants per km². The current mayor of Lede is Geertrui Van de Velde (CD&V). Geography The municipality comprises the sub-municipalities of Impe, Lede proper, Oordegem, Smetlede, Wanzele, and the hamlet of Papegem. All the sub-municipalities and also the hamlet are crossed by the Molenbeek. Sandstone The Lede Formation ( nl, Formatie van Lede; abbreviation: Ld) is a geologic formation in the subsurface of Belgium. The formation is named after Lede. It consists of shallow-marine limestone and sandstone, deposited in the former sea that covered Belgium during the Eocene. The bluestone (for roads) and in particular the yellow-brown calcareous sandstone extracted from quarries in Lede and neighbouring areas, were widely used during the 15th ...
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