Real Property, Dunedin, New Zealand, 1896 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: The Survey Districts of North Harbour & Blueskin, Lower Harbour West, North East Valley, Upper Harbour West, Tomahawk, Sawyers Bay, Andersons Bay, Portobello Bay, Otago Peninsula & Upper Harbour East, drawn by G.P. Wilson, April 1896. It was published by N.Z. Lands and Survey in 1896. Covers the Dunedin region, New Zealand. Scale [ca. 1:63,360]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Universal Transverse Mercator (UTM Zone 59S, meters, WGS 1984) projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as property lot and block numbers, boundaries of survey districts and blocks, boroughs, townships and estates, drainage, selected roads, railroads and stations, selected buildings and industry locations, cemeteries, shoreline features, docks and wharves, and more. Relief shown by spot heights.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Chatham Islands, New Zealand, 1883 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the Chatham Islands, from surveys by S.P. Smith & John Robertson, 1868 & 1883. It was published by General Survey Office in 1887. Scale [ca. 1:126,720].The image inside the map neatline is georeferenced to the surface of the earth and fit to the World Miller Cylindrical projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, roads, shoreline features, and more. Relief shown by hachures. Includes inset: Waitangi; Plan of Rangiauria or Pitt Id. (part of Chatham Islands); Key map shewing the position of the Chatham Islands relative to New Zealand; Rangitutahi or Sister (part of Chatham Islands group).This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Latest Cretaceous to Late Paleocene radiolarian biostratigraphy from the New Zealand region

The scarcity of records of Early Paleocene radiolarians has meant that while radiolarian biostratigraphy is firmly established as an important tool for correlation, there has been a long-standing gap between established zonations for the Cretaceous and from latest Paleocene to Recent. It has also led to considerable speculation over the level of faunal change across the Cretaceous/Tertiary (K/T) boundary. Consequently, the discovery of rich and diverse radiolarian assemblages in well-delineated K/T boundary sections within siliceous limestones of the Amuri Limestone Group in eastern Marlborough, New Zealand, is of great significance for biostratigraphy and K/T boundary research. This initial report is restricted to introducing a new latest Cretaceous to mid Late Paleocene zonation based on the radiolarian succession at four of these sections and a re-examination of faunas from coeval sediments at DSDP Site 208 (Lord Howe Rise). Three new Paleocene species are described: Amphisphaera aotea, Amphisphaera kina and Stichomitra wero. Six new interval zones are defined by the first appearances of the nominate species. In ascending order these are: Lithomelissa? hoplites Foreman (Zone RK9, Cretaceous), Amphisphaera aotea n. sp. (Zone RP1, Paleocene), Amphisphaera kina n. sp. (RP2), Stichomitra granulata Petrushevskaya (RP3), Buryellaforemanae petrushevskaya (RP4) and Buryella tetradica (RP5). Good age control from foraminifera and calcareous nannofossils permits close correlation with established microfossil zonations. Where age control is less reliable, radiolarian events are used to substantially improve correlation between the sections. No evidence is found for mass extinction of radiolarians at the end of the Cretaceous. However, the K/T boundary does mark a change from nassellarian to spumellarian dominance, due to a sudden influx of actinommids, which effectively reduces the relative abundance of many Cretaceous survivors. An accompanying influx of diatoms in the basal Paleocene of Marlborough, together with evidence for an increase of total radiolarian abundance, suggests siliceous plankton productivity increased across the K/T boundary. Possible causes for this apparently localised phenomenon are briefly discussed.

FHWA study tour for highway safety management practices in Japan, Australia, and New Zealand.

Mode of access: Internet.

A concise statement of the principles of the only true church of Christ /

"A letter from James Whittaker": p. 16-23.

A Mandarin-Romanized dictionary of Chinese, with supplement of new terms and phrases, now current,

Chinese title at head of t.-p.

Meat production in Australia and New Zealand /

"From Yearbook of Department of Agriculture for 1914."

Presbyterian forms of service /

Mode of access: Internet.

Sunday near the Church of Saint-Philippe-du-Roule, Paris

Jean Beraud; 1 ft. 11 25/64 in.x 2 ft. 7 57/64 in.; oil on canvas