Many stocks are cupolas of hidden batholiths. These form several intrusive bodies such as batholiths and stocks. Similar ages and sequences of types apply to the other batholiths. In some cases, granite intrusions formed large batholiths and charnockite. Associated igneous activity resulted in batholiths (620 Ma) and pyroclastics (633 Ma). Proterozoic anorthosites typically occur as extensive stocks or batholiths. This type of hybrid source might also explain the features of the monzogranitic batholiths. It consists of a series of batholiths in Sweden and Norway forming a ca. Common examples are igneous dikes, sills, plutons, and batholiths. Different types of intrusions include stocks, laccoliths, batholiths, sills and dikes. Many of the major batholiths date from the late Cretaceous. Two more batholiths, the Karamea-Paparoa and Hohonu Batholiths, are also found on the West Coast. In central Europe, smaller bodies are described as batholiths and larger bodies as plutons. Three large batholiths are in the north east&colon; Scottsdale, Eddystone and Blue Tier. In the batholiths there are quartz-feldspar porphyry and dolerite dykes.