Belgium in "the long nineteenth century" the small duchies, princedoms and counties which had traditionally been the basic territorial units. Aside from Zeelandic Flanders, part of Luxembourg, and Northern Limburg, which were ceded to the Dutch to compensate for the loss of the rest of the territory, the outline of Belgium in 1914 was virtually identical to that established by the French in 1795. The three ceded territories had a total of 300,000 inhabitants at the time. The northern half of Belgium, which would come to be known as Flanders, was a largely agricultural area containing the important port of Antwerp, the city of Ghent and
Geology of the Waikato-King Country Region position. The Waipapa Morrinsville Terrane greywacke lies beneath the Waikato-King Country region on the eastern side, south of the Hunua Ranges, and east of the Waipa Fault. It was formed in Late Jurassic to Early Cretaceous times (160-120 Ma). The Te Kuiti Group rocks overlie the basement rocks, and are present in Northland, Auckland, the Waikato, and King Country, although they have often been eroded or covered. Rocks containing coal were formed from swampland in Late Eocene times (37-34 Ma). The land sunk and the sea transgressed, and calcareous sandstone, mudstone, and limestone were deposited in Oligocene times (34-24 Ma).