title: The nature and scope of student search strategies in using a web derived corpus for writing

authors: Franken, Margaret

subjects: online language corpus

abstract: The use of online language corpora in L2 teaching and learning is gaining momentum largely because corpora are an easily accessed source of language input that potentially provide rich and authentic lexico-grammatical data. This can be of particular use for students' writing as its incorporation can enhance the appearance of native-like fluency. We describe a particular online web-derived corpus constructed by means of digital library software, and we describe the nature of the concordancer that services it. This is a system we have named FLAX (Flexible Language Acquisition). Because the system incorporates not only a useful and authentic corpus but also linked databases, we maintain that it meets the need for an easily accessible online resource that gives explicit information about typical lexical and syntactic collocations. While online corpus-based resources are becoming more readily available, and their effective incorporation into language teaching is being documented, we seem to know little about how learners access them and make use of the results they generate. This paper reports on an exploratory investigation of the search strategies used by learners in a university general English course as they make use of FLAX, tracking the way they exploit the search results in their texts, and presenting their relevant comments about the system. In such a way, we seek to explain variation in students' use and effectiveness of search strategies to support their writing. This type of research, although exploratory, is critical if we are to acknowledge the need for students to become ‘research workers’.

text: The nature and scope of student search strategies in using a web derived corpus for writing The use of online language corpora in L2 teaching and learning is gaining momentum largely because corpora are an easily accessed source of language input that potentially provide rich and authentic lexico-grammatical data. This can be of particular use for students' writing as its incorporation can enhance the appearance of native-like fluency. We describe a particular online web-derived corpus constructed by means of digital library software, and we describe the nature of the concordancer that services it. This is a system we have named FLAX (Flexible Language Acquisition). Because the system incorporates not only a useful and authentic corpus but also linked databases, we maintain that it meets the need for an easily accessible online resource that gives explicit information about typical lexical and syntactic collocations. While online corpus-based resources are becoming more readily available, and their effective incorporation into language teaching is being documented, we seem to know little about how learners access them and make use of the results they generate. This paper reports on an exploratory investigation of the search strategies used by learners in a university general English course as they make use of FLAX, tracking the way they exploit the search results in their texts, and presenting their relevant comments about the system. In such a way, we seek to explain variation in students' use and effectiveness of search strategies to support their writing. This type of research, although exploratory, is critical if we are to acknowledge the need for students to become ‘research workers’.

year: 2012

title: Volcanic geology and hydrothermal alteration of the Onemana Area, Eastern Coromandel Peninsula

authors: Aldrich, Sean Mark

subjects: Volcanic Geology

abstract: The Onemana Peninsula is located on the eastern side of the Coromandel Peninsula north of the township of Whangamata. This study investigates the volcanology, structure and hydrothermal alteration of the northern half of the Onemana Peninsula. The study area is dominated by rhyolite domes and lava flows, with minor andesite lavas, rhyolite pyroclastics and lake sediments. The central region is extensively hydrothermally altered, with high levels of the original system preserved including hydrothermal eruption breccias and sinters.

The Onemana area is dominated by three rhyolite dome complexes: Pohakahaka, Pokohino, and Wharekawa. The Pohakahaka Dome Complex in the south of the study area consists of pyroxene rhyolite domes, lavas and autoclastic breccias. The Pokohino Dome Complex in the central region of the study area consists of biotite rhyolite domes, lavas and autoclastic breccias. Lavas appear to have erupted as coulees and have flowed in a SE direction from a NE-trending ridge. The Wharekawa Dome Complex and Eastern Flows are dominated by biotite rhyolites. Pyroclastic and epiclastic material is overlain by rhyolite lavas in coastal sections north of Pokohino Beach, suggesting explosive activity preceded the eruption of some lavas. Some Eastern Flow lavas have flowed into water and produced a hyaloclastite in the north of the area. The deposition of the Glassy Dome Pyroclastics is thought to have resulted from the collapse of a rhyolite dome. Andesite lavas occur in the west of the study area, and their compositions suggest that they are related to the McBeths Andesite which outcrops 6 km to the NW. A hornblende-biotite ignimbrite is exposed in the north of the area, and is thought to have been erupted from outside the area. Thick lake sediments occur between the Pokohino and Wharekawa dome complexes and infill a graben structure. A hydrothermal eruption breccia resulting from over-pressuring of a geothermal system overlies the lake sediments. 

The structure of the area is dominated by NW, N, and NE striking faults, and minor EW striking faults. The local structure plays an important role in controlling the locations of volcanism and hydrothermal activity. Older N-striking structures appear to have controlled vent locations for the pyroxene rhyolites, while NE-striking structures have controlled the location the biotite rhyolites and hydrothermal alteration. Mineralised structures are controlled by NW and N striking faults between the NE striking Whitipirorua and Pokohino Faults.

XRF analysis of selected volcanic rocks from Onemana show the area to be dominated by medium-K to high-K rhyolites (75-78 wt% SiO₂), with minor andesite (56-58 wt% SiO₂). On the basis of Zr abundance the rhyolites can be divided into high Zr (pyroxene rhyolites) and low Zr (biotite rhyolites, Glassy Dome Rhyolite). The rhyolites are thought to be closely associated with partial melting of the continental crust in a rifting environment.

Pervasive to weak alteration occurs within a NE-trending corridor bounded by the Whitipirorua and Pokohino Faults. There are two main alteration types in the area which represent different hydrothermal environments: alkaline and acid alteration. Alkaline alteration consists of an inner core of quartz silicification, surrounded by quartz+ K-feldspar alteration, which grades out into epidote and weak clay alteration assemblages. Zeolites also occur as an overprinting alteration assemblage. Acid alteration consists of pervasive kaolinite alteration, with small areas of quartz + illite/smectite ± pyrophyllite alteration and opaline quartz silicification.

The Onemana area shows many volcanic and hydrothermal features that are typical of caldera settings and are comparable with the rhyolite volcanic centres in the TVZ. It is suggested that the rhyolitic volcanism at Onemana resulted from late stage volcanism along the ring fracture of a large caldera structure.

text: Volcanic geology and hydrothermal alteration of the Onemana Area, Eastern Coromandel Peninsula The Onemana Peninsula is located on the eastern side of the Coromandel Peninsula north of the township of Whangamata. This study investigates the volcanology, structure and hydrothermal alteration of the northern half of the Onemana Peninsula. The study area is dominated by rhyolite domes and lava flows, with minor andesite lavas, rhyolite pyroclastics and lake sediments. The central region is extensively hydrothermally altered, with high levels of the original system preserved including hydrothermal eruption breccias and sinters.

The Onemana area is dominated by three rhyolite dome complexes: Pohakahaka, Pokohino, and Wharekawa. The Pohakahaka Dome Complex in the south of the study area consists of pyroxene rhyolite domes, lavas and autoclastic breccias. The Pokohino Dome Complex in the central region of the study area consists of biotite rhyolite domes, lavas and autoclastic breccias. Lavas appear to have erupted as coulees and have flowed in a SE direction from a NE-trending ridge. The Wharekawa Dome Complex and Eastern Flows are dominated by biotite rhyolites. Pyroclastic and epiclastic material is overlain by rhyolite lavas in coastal sections north of Pokohino Beach, suggesting explosive activity preceded the eruption of some lavas. Some Eastern Flow lavas have flowed into water and produced a hyaloclastite in the north of the area. The deposition of the Glassy Dome Pyroclastics is thought to have resulted from the collapse of a rhyolite dome. Andesite lavas occur in the west of the study area, and their compositions suggest that they are related to the McBeths Andesite which outcrops 6 km to the NW. A hornblende-biotite ignimbrite is exposed in the north of the area, and is thought to have been erupted from outside the area. Thick lake sediments occur between the Pokohino and Wharekawa dome complexes and infill a graben structure. A hydrothermal eruption breccia resulting from over-pressuring of a geothermal system overlies the lake sediments. 

The structure of the area is dominated by NW, N, and NE striking faults, and minor EW striking faults. The local structure plays an important role in controlling the locations of volcanism and hydrothermal activity. Older N-striking structures appear to have controlled vent locations for the pyroxene rhyolites, while NE-striking structures have controlled the location the biotite rhyolites and hydrothermal alteration. Mineralised structures are controlled by NW and N striking faults between the NE striking Whitipirorua and Pokohino Faults.

XRF analysis of selected volcanic rocks from Onemana show the area to be dominated by medium-K to high-K rhyolites (75-78 wt% SiO₂), with minor andesite (56-58 wt% SiO₂). On the basis of Zr abundance the rhyolites can be divided into high Zr (pyroxene rhyolites) and low Zr (biotite rhyolites, Glassy Dome Rhyolite). The rhyolites are thought to be closely associated with partial melting of the continental crust in a rifting environment.

Pervasive to weak alteration occurs within a NE-trending corridor bounded by the Whitipirorua and Pokohino Faults. There are two main alteration types in the area which represent different hydrothermal environments: alkaline and acid alteration. Alkaline alteration consists of an inner core of quartz silicification, surrounded by quartz+ K-feldspar alteration, which grades out into epidote and weak clay alteration assemblages. Zeolites also occur as an overprinting alteration assemblage. Acid alteration consists of pervasive kaolinite alteration, with small areas of quartz + illite/smectite ± pyrophyllite alteration and opaline quartz silicification.

The Onemana area shows many volcanic and hydrothermal features that are typical of caldera settings and are comparable with the rhyolite volcanic centres in the TVZ. It is suggested that the rhyolitic volcanism at Onemana resulted from late stage volcanism along the ring fracture of a large caldera structure.

year: 1995

title: Joseph Harris Smallman

authors: Hart, Philip

abstract: Born to a mining agent and trained as a mining surveyor, in 1864, less than a year after the birth of his first child, Smallman left England for New Zealand to establish a ‘Mining business’, promising that his family would join him once it was successful. But they were never asked to join him, and after 1870 he ceased to write to his wife. 
The ‘Mining business’ never eventuated, but in 1865 he prospected at Thames, unsuccessfully seeking alluvial gold. Although criticized for living off Maori and doing little prospecting, with his partner he investigated several areas of the Hauraki Peninsula, again unsuccessfully. When the Thames goldfield was opened, with his encouragement, two years later, he mined there for some years, proving himself to be a competent miner but not making his fortune. After working elsewhere, by the mid-1870s he was living with another man’s ‘half-caste’ wife on her land near Te Aroha, having five children with her. Happy to be described as a Pakeha Maori and closely associated with the local hapu, he supported them over land dealings and the development of the district. Despite spending most of his time farming, he remained interested in prospecting, and made some explorations in districts closed to Pakeha. After gold was found at Te Aroha, for a short time he worked with Maori partners in unprofitable claims.
Either before or after his second wife had a child by another man in 1886, he left New Zealand to return to his English family; and remarkably, despite his first wife knowing that his liaison had produced children, she accepted him back after his long absence, and they remained together for the rest of their lives.

text: Joseph Harris Smallman Born to a mining agent and trained as a mining surveyor, in 1864, less than a year after the birth of his first child, Smallman left England for New Zealand to establish a ‘Mining business’, promising that his family would join him once it was successful. But they were never asked to join him, and after 1870 he ceased to write to his wife. 
The ‘Mining business’ never eventuated, but in 1865 he prospected at Thames, unsuccessfully seeking alluvial gold. Although criticized for living off Maori and doing little prospecting, with his partner he investigated several areas of the Hauraki Peninsula, again unsuccessfully. When the Thames goldfield was opened, with his encouragement, two years later, he mined there for some years, proving himself to be a competent miner but not making his fortune. After working elsewhere, by the mid-1870s he was living with another man’s ‘half-caste’ wife on her land near Te Aroha, having five children with her. Happy to be described as a Pakeha Maori and closely associated with the local hapu, he supported them over land dealings and the development of the district. Despite spending most of his time farming, he remained interested in prospecting, and made some explorations in districts closed to Pakeha. After gold was found at Te Aroha, for a short time he worked with Maori partners in unprofitable claims.
Either before or after his second wife had a child by another man in 1886, he left New Zealand to return to his English family; and remarkably, despite his first wife knowing that his liaison had produced children, she accepted him back after his long absence, and they remained together for the rest of their lives.

year: 2016