grammar, morphology

Issues in language study: origin of language, animals & human language, writing, phonetics, phonology, words & word-formation processes, morphology, grammar, syntax, semantics, pragmatics, discourse analysis, language and the brain, language acquisition, gestures and sign languages, languages and regional variation, language and social variation, language and culture.B&w illustrations, b&w photographs, mapslinguistics, sociolinguistics, history and language

Mt Greenock is an extinct volcano with lava flows associated with a deep lead. It is a tall scoria cone with a broad shallow crater open to the northwest. In the crater are blocks and bombs of scoriaceous basalt. Long lava flows extend both north and south from the cone. It is considered a significant geological site, and part of the Major Mitchell Trail, with a 1936 ‘Centenary of Major Mitchell ‘monument on the summit. The flow to the north has been eroded by McCallum Creek which is a lateral stream. On the eastern base of the cone, the stream valley exposes a lava flow and underlying sedimentary rocks. The lava flow and the scoria cone overlie the Greenock lead (a buried valley with auriferous gravels). A line of mine tailing and abandoned mining relics associated with the former Union Mine occur on the margins of the lava flow. Mount Greenock is a 120 hectare ‘Geological Reserve’, is one of the few large scoria cones on public land and contains abundant outcrop and morphological evidence of its volcanic origin. Colour Photographs of bluestone and brick buildings at Mt Greenock, near Talbot, Victoria. The photographs were taken in winter not long after the first post drought rains. mt greenock, mount greenock, mining, mullock heap, mt greenock geological reserve, union mine, volcanic grasslands, dunach

Mt Greenock is an extinct volcano with lava flows associated with a deep lead. It is a tall scoria cone with a broad shallow crater open to the northwest. In the crater are blocks and bombs of scoriaceous basalt. Long lava flows extend both north and south from the cone. It is considered a significant geological site, and part of the Major Mitchell Trail, with a 1936 ‘Centenary of Major Mitchell ‘monument on the summit. The flow to the north has been eroded by McCallum Creek which is a lateral stream. On the eastern base of the cone, the stream valley exposes a lava flow and underlying sedimentary rocks. The lava flow and the scoria cone overlie the Greenock lead (a buried valley with auriferous gravels). A line of mine tailing and abandoned mining relics associated with the former Union Mine occur on the margins of the lava flow. Mount Greenock is a 120 hectare ‘Geological Reserve’, is one of the few large scoria cones on public land and contains abundant outcrop and morphological evidence of its volcanic origin. Colour Photographs of Mt Greenock, near Talbot, Victoria. The photographs were taken in winter not long after the first post drought rains. Mt Greenock was climbed by Major Thomas Mitchell on 26 September 1936, and he gave it the current name. At that time the mount was part of Alexander McCallum's Dunach Forest Pastoral Run.mt greenock, mount greenock, mining, mullock heap, mt greenock geological reserve, union mine, volcanic grasslands, dunach

The toothed whales (also called odontocetes, systematic name Odontoceti) are a parvorder of cetaceans that includes dolphins, porpoises, and all other whales possessing teeth, such as the beaked whales and sperm whales. Seventy-three species of toothed whales are described. They are one of two living groups of cetaceans, the other being the baleen whales (Mysticeti), which have baleen instead of teeth. The two groups are thought to have diverged around 34 million years ago (mya). Toothed whales range in size from the 4.5 ft (1.4 m) and 120 lb (54 kg) vaquita to the 20 m (66 ft) and 55 t (61-short-ton) sperm whale. Several species of odontocetes exhibit sexual dimorphism, in that there are size or other morphological differences between females and males. They have streamlined bodies and two limbs that are modified into flippers. Some can travel at up to 20 knots. Odontocetes have conical teeth designed for catching fish or squid. They have well-developed hearing, that is well adapted for both air and water, so much so that some can survive even if they are blind. Some species are well adapted for diving to great depths. Almost all have a layer of fat, or blubber, under the skin to keep warm in the cold water, with the exception of river dolphins. Toothed whales consist of some of the most widespread mammals, but some, as with the vaquita, are restricted to certain areas. Odontocetes feed largely on fish and squid, but a few, like the killer whale, feed on mammals, such as pinnipeds. Males typically mate with multiple females every year, but females only mate every two to three years, making them polygynous. Calves are typically born in the spring and summer, and females bear the responsibility for raising them, but more sociable species rely on the family group to care for calves. Many species, mainly dolphins, are highly sociable, with some pods reaching over a thousand individuals. Once hunted for their products, cetaceans are now protected by international law. Some species are attributed with high levels of intelligence. At the 2012 meeting of the American Association for the Advancement of Science, support was reiterated for a cetacean bill of rights, listing cetaceans as nonhuman persons. Besides whaling and drive hunting, they also face threats from bycatch and marine pollution. The baiji, for example, is considered functionally extinct by the IUCN, with the last sighting in 2004, due to heavy pollution to the Yangtze River. Whales occasionally feature in literature and film, as in the great white sperm whale of Herman Melville's Moby-Dick. Small odontocetes, mainly dolphins, are kept in captivity and trained to perform tricks. Whale watching has become a form of tourism around the world. Reference: https://en.wikipedia.org/wiki/Toothed_whaleWhale teeth were much prized for use in scrimshaw work.Whale tooth. Significant staining and yellowing. Broken at base, and missing the root.Noneflagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, whale tooth, whaling, whaling industry, whales

This photograph captures a historically significant streetscape in Westmeadows, formerly known as Broadmeadows Township, looking north from Fawkner Street. The image features a dirt road with a vintage automobile parked along its path, flanked by trees and modest residential buildings in the background. A tall utility or signpost stands prominently, indicative of early infrastructure in the area. The scene reflects the semi-rural character of Westmeadows prior to its suburban expansion in the post-war period. The presence of unsealed roads and early 20th-century vehicles suggests a time when the township served as a quiet residential and agricultural community, before the development of the Broadmeadows Housing Commission estate in the late 1940s. Historically, Westmeadows was a key waypoint along the Old Sydney Road, and its built environment—including bluestone bridges and early civic buildings—offers insight into Melbourne’s colonial and interwar development. This photograph contributes to the visual documentation of the City of Hume’s transformation from rural township to suburban district.This photograph holds historical and cultural significance as a visual record of Westmeadows, a township in Melbourne’s north-west, during the early 20th century. Captured from Fawkner Street looking north, the image depicts a dirt road flanked by modest residential buildings and mature trees, with a vintage automobile parked in the foreground. The presence of a tall utility or signpost adds to the authenticity of the streetscape. The image is emblematic of Westmeadows’ semi-rural character prior to its suburban transformation in the post-war era. It reflects the township’s role as a quiet residential and agricultural community, shaped by its proximity to the Old Sydney Road and its historical function as a waypoint for travelers. The architectural style and infrastructure visible in the photograph provide insight into the urban morphology and transport conditions of the time. As a primary source, the photograph contributes to the documentation of Melbourne’s suburban expansion, offering valuable context for researchers, historians, and urban planners studying the evolution of the City of Hume. It is significant for its ability to convey the lived experience, landscape, and development patterns of a community in transition.Sepia tone photo. Two cars on road. Trees, some buildings behind. Open land. Street view.'Looking north Fawkner Street Westmeadows'/'PH-0018' (old catalogue number)westmeadows, fawkner street, north, car