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  2. Vaalserberg - Wikipedia

    en.wikipedia.org/wiki/Vaalserberg

    The Vaalserberg is located in the province of Limburg, at the south-easternmost edge of the country, near the town of Vaals (after which it is named). The Vaalserberg was the highest point anywhere in the Netherlands until the Caribbean island of Saba , with its 887-metre-high (2,910-foot) volcano , was incorporated into the country as a ...

  3. List of mountains and hills in the Netherlands - Wikipedia

    en.wikipedia.org/wiki/List_of_mountains_and...

    The following is a list of mountains and hills in the Netherlands. Cauberg (134 metres; 440 ft) [1] Eyserbosweg (193 metres; 633 ft) [2] Keutenberg (163 metres; 535 ...

  4. Cauberg - Wikipedia

    en.wikipedia.org/wiki/Cauberg

    Landal holiday village. The foot of Cauberg hill is situated almost in the center of Valkenburg, outside the medieval city gate of Grendelpoort. At the bottom of the hill is one of Valkenburg's main visitor attractions, Gemeentegrot, an abandoned chalk quarry offering guided tours through a labyrinth of man-made caves which include an underground lake, limestone sculptures of prehistoric ...

  5. List of extreme points of the Netherlands - Wikipedia

    en.wikipedia.org/wiki/List_of_extreme_points_of...

    Southernmost Point — boundary marker 12 along Rue de Beusdael, near Kuttingen in the municipality of Gulpen-Wittem, Limburg Westernmost Point — Sint Anna ter Muiden ( 51°18′57″N 3°21′30″E  /  51.31583°N 3.35833°E  / 51.31583; 3.35833  ( West: Sint Anna ter

  6. Mount Saint Peter - Wikipedia

    en.wikipedia.org/wiki/Mount_Saint_Peter

    Guided tours of these limestone quarries, some with ancient inscriptions, drawings and other works of art, constitute one of Maastricht's main tourist attractions. In modern times limestone from Mount Saint Peter continues to be quarried in surface mines, mainly for portland cement production. Abandoned quarries in the Belgian part of the hill ...

  7. Geology of the Netherlands - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Netherlands

    The modern Netherlands formed as a result of the interplay of the four main rivers (Rhine, Meuse, Schelde and IJssel) and the influence of the North Sea and glaciers during ice-ages. The Netherlands is mostly composed of deltaic , coastal and eolian derived sediments during the Pleistocene glacial and interglacial periods.

  8. Campus of Virginia Tech - Wikipedia

    en.wikipedia.org/wiki/Campus_of_Virginia_Tech

    The main campus of Virginia Tech is located in Blacksburg, Virginia; the central campus is roughly bordered by Prices Fork Road to the northwest, Plantation Road to the west, Main Street to the east, and U.S. Route 460 bypass to the south, although it also has several thousand acres beyond the central campus. The Virginia Tech campus consists ...

  9. Hokie Stone - Wikipedia

    en.wikipedia.org/wiki/Hokie_Stone

    Hokie Stone is a grey dolomite—limestone rock found near Blacksburg, in western Virginia. It gets its name from the traditional nickname attributed to students and alumni of Virginia Tech. Hokie Stone is quarried by Virginia Tech for campus projects and is prominently displayed on the majority of buildings throughout the Blacksburg campus.