title: Quaternary stratigraphy, landscape, and soils of the Hamilton Basin

authors: Kamp, Peter J.J.

abstract: The Hamilton Basin is a roughly oval shaped depression 80 km north to south and 40 km wide centered about Hamilton City (Fig. 1). The basin is surrounded by ranges up to 300 m high developed mainly in Mesozoic basement strata. The physiographic basin is essentially a fault bounded basement depression of Late Tertiary and Pleistocene age. Throughout the Quaternary this basin has been a receptacle of terrestrial sedimentation; the materials have derived mainly from extrabasin sources and principally the Central Volcanic Region to the southeast. In addition, materials have been derived from erosion of the bounding ranges, and Coromandel Peninsula. The last major depositional episode involved flood deposit s of the Taupo Pumice. The present landscape has evolved through several episodes of deposition and incision. 
During the excursion it is intended to show the participants exposures of the major Quaternary units of basin infilling, and some aspects of the landscape and the soil pattern, within the environs of Hamilton City.
The standard geological reference covering the geology of Hamilton Basin is New Zealand Geological Survey Bulletin 88 (Kear & Schofield, 1978) . The surface features and soil pattern of the basin are succinctly covered by McCraw (1967) and Bruce (1979).

text: Quaternary stratigraphy, landscape, and soils of the Hamilton Basin The Hamilton Basin is a roughly oval shaped depression 80 km north to south and 40 km wide centered about Hamilton City (Fig. 1). The basin is surrounded by ranges up to 300 m high developed mainly in Mesozoic basement strata. The physiographic basin is essentially a fault bounded basement depression of Late Tertiary and Pleistocene age. Throughout the Quaternary this basin has been a receptacle of terrestrial sedimentation; the materials have derived mainly from extrabasin sources and principally the Central Volcanic Region to the southeast. In addition, materials have been derived from erosion of the bounding ranges, and Coromandel Peninsula. The last major depositional episode involved flood deposit s of the Taupo Pumice. The present landscape has evolved through several episodes of deposition and incision. 
During the excursion it is intended to show the participants exposures of the major Quaternary units of basin infilling, and some aspects of the landscape and the soil pattern, within the environs of Hamilton City.
The standard geological reference covering the geology of Hamilton Basin is New Zealand Geological Survey Bulletin 88 (Kear & Schofield, 1978) . The surface features and soil pattern of the basin are succinctly covered by McCraw (1967) and Bruce (1979).

year: 1981

title: Remote sensing of water quality – fact sheet

authors: Hicks, Brendan J.

abstract: Evaluating water quality is a key tool in lake management. Typically water quality samples are restricted to a limited number of point samples collected in situ in the field, which can be time consuming and costly. Also, the few in situ points sampled fail to capture the spatial variability, e.g., for the large Lake Waikare (3,400 ha; Figure. 1).

text: Remote sensing of water quality – fact sheet Evaluating water quality is a key tool in lake management. Typically water quality samples are restricted to a limited number of point samples collected in situ in the field, which can be time consuming and costly. Also, the few in situ points sampled fail to capture the spatial variability, e.g., for the large Lake Waikare (3,400 ha; Figure. 1).

year: 2015

title: Mana whenua, mana tangata: Raukawa ake, Raukawa iho

authors: Peni, Tamati

subjects: Raukawa

abstract: Mā te whakapapa, ngā tohu whenua, ngā pae whenua, ngā mātākōrero, ngā kōrero tuku iho, ka whakatere te takenga mai o ngā ariā me ngā mātāpono o Raukawa.  Ina te matapakinga, ka tīkaro hoki i ngā āhuatanga o tuawhakarere me ngā āhuatanga o te ao hurihuri kia tūhono i ngā matapakinga he aha rānei te Raukawatanga me te pātai he aha hoki ōna pānga ki te ao whai muri ake i te taunaha i ngā take Tiriti.  Nā te whānui rawa me te kaha tīni haere o te taiwhanga nei, ka whakawhāiti te rangahau ki ngā whakamautanga o Raukawa ki ngā pae whenua tawhito, ā, ka whītikihia te aronga ki nāianei, ki te ao hurihuri.

I seek to explore the ideological grounding of Raukawa through whakapapa, land marks, boundaries, oral history, and tradition.  Through this, a simultaneous extraction of traditional and contemporary themes are used to bridge new and old ways of being and what impact this has on being Raukawa in a post-settlement setting.  Because of the vastness and changing nature of this environment, I narrow my focus to how Raukawa maintained traditional boundaries and draw on its relevance to modern Raukawa development today.

text: Mana whenua, mana tangata: Raukawa ake, Raukawa iho Mā te whakapapa, ngā tohu whenua, ngā pae whenua, ngā mātākōrero, ngā kōrero tuku iho, ka whakatere te takenga mai o ngā ariā me ngā mātāpono o Raukawa.  Ina te matapakinga, ka tīkaro hoki i ngā āhuatanga o tuawhakarere me ngā āhuatanga o te ao hurihuri kia tūhono i ngā matapakinga he aha rānei te Raukawatanga me te pātai he aha hoki ōna pānga ki te ao whai muri ake i te taunaha i ngā take Tiriti.  Nā te whānui rawa me te kaha tīni haere o te taiwhanga nei, ka whakawhāiti te rangahau ki ngā whakamautanga o Raukawa ki ngā pae whenua tawhito, ā, ka whītikihia te aronga ki nāianei, ki te ao hurihuri.

I seek to explore the ideological grounding of Raukawa through whakapapa, land marks, boundaries, oral history, and tradition.  Through this, a simultaneous extraction of traditional and contemporary themes are used to bridge new and old ways of being and what impact this has on being Raukawa in a post-settlement setting.  Because of the vastness and changing nature of this environment, I narrow my focus to how Raukawa maintained traditional boundaries and draw on its relevance to modern Raukawa development today.

year: 2013