ceremonial gatherings – potlatches – were made illegal". In 1922, after mass arrests, the We-Wai-Kai people surrendered their masks and regalia to the government. The property was not returned to them for some 50 years, to the Nuuyumbalees Cultural Centre. The first school was built by the Kwagiulth people at Cape Mudge in 1893; the fishing fleet in operation at that time is still successful today. A copper and gold mine, the Lucky Jim, opened in 1903 but was destroyed by fire in 1941. In 1904, the island had "two post offices, a school, hotel, lumber camps, mills, and a mission", according to one report. A passenger ferry commenced service in 1949 and a ferry for vehicles started in 1960. By 1904, Quadra had two post offices, a school, hotel, lumber camps, mills, and a mission. Severe fires devastated Quadra over the years leading to a poor economy well into the 1930s. A passenger ferry started in 1949 and a car ferry in 1960. Geography Quadra Island is separated from Vancouver Island by Discovery Passage, and from Cortes Island by Read Island and the Sutil Channel, and is linked to that island by a ferry from Heriot Bay on its eastern shore. The island has many beaches, trails, lakes, and parks. Main Lake Provincial Park is located on the northern part of the island, and Rebecca Spit Marine Provincial Park is on the eastern shore, near Heriot Bay. Quadra Island is about from its northernmost point to its southernmost point. The island at its narrowest point, on its southern peninsula, is less than wide, and at its widest point, about wide. With an area of , Quadra Island is the largest island of the Discovery Islands and the second largest island in the Salish Sea after Whidbey Island in Washington. Geology Few of the island's soils are well suited to agriculture. Most are coarse and, outside of poorly drained areas, have classic podzol profile development; well-drained podzols are mapped as Kye loamy sand and Quinsam gravelly sandy loam. A small area of dark well-drained unpodzolized soil (Lazo loamy sand) is mapped around the southeast corner. Dashwood gravelly loamy sand, a brown podzolic trending to podzol, is commonly associated with Kye and Quinsam. Imperfectly drained areas have brown podzolic Bowser loamy sand or classic podzol Sayward loamy sand. The more moist Custer loamy sand, a groundwater podzol, is present locally. Poorly