scholarly journals George Henry Frederick Ulrich (1830–1900): pioneer mineralogist and geologist in Victoria

2015 ◽  
Vol 127 (1) ◽  
pp. 17
Author(s):  
William D. Birch ◽  
Thomas A. Darragh
Keyword(s):  
New Zealand ◽  
Geological Survey ◽  
New Mineral ◽  
Short Period ◽  
Personal Qualities ◽  
Mining Commission ◽  
Scientific Achievements

George Henry Frederick Ulrich (1830–1900) was educated at the Clausthal Mining School in Germany and arrived in Victoria in 1853. After a short period on the goldfields, he was employed on the Mining Commission and then on the Geological Survey of Victoria until its closure in 1868. In 1870 he was appointed Curator and Lecturer at the newly established Industrial and Technological Museum of Victoria. In 1878 he was appointed inaugural Director of the Otago School of Mines, New Zealand, a position he held until his death in 1900. His legacy includes detailed original maps of central Victorian goldfields, the foundation of the state’s geological collections, and among the first accounts of Victorian geology published in German periodicals, until now little known. As the only scientist of his times in Victoria with the qualifications and expertise to accurately identify and properly describe minerals, he provided the first comprehensive accounts of Victorian mineralogy, including the identification of the first new mineral in Australia, which he named maldonite. His contribution to mineralogy is recognised by the species ulrichite. Ulrich was universally respected for his scientific achievements and highly regarded for his personal qualities.

scholarly journals Preliminary paleoearthquake investigations of active faults on Awaji Island, Japan,
 in relation to the 1995 Great Hanshin (Kobe) earthquake

1996 ◽  
Vol 29 (3) ◽  
pp. 172-177
Author(s):  
R. Van Dissen ◽  
J. Begg ◽  
Y. Awata
Keyword(s):  
New Zealand ◽  
Active Fault ◽  
Active Faults ◽  
Geological Survey ◽  
Historical Records ◽  
Surface Rupture ◽  
Kobe Earthquake ◽  
Nojima Fault ◽  
One Year ◽  
Hanshin Earthquake

Approximately one year after the Great Hanshin (Kobe) Earthquake, two New Zealand geologists were invited to help with the Geological Survey of Japan's paleoearthquake/active fault studies in the Kobe/Awaji area. Trenches excavated across the Nojima fault, which ruptured during the Great Hanshin Earthquake, showed evidence of past surface rupture earthquakes, with the age of the penultimate earthquake estimated at approximately 2000 years. A trench across the Higashiura fault, located 3-4 km southeast of the Nojima fault, revealed at least two past surface rupture earthquakes. The timing of the older earthquakes is not yet known, but pottery fragments found in the trench constrain the timing of the most recent earthquake at less than 500-600 years. Historical records for this part of Japan suggest that within the last 700 years there has been only one regionally felt earthquake prior to the 1995 Great Hanshin Earthquake, and this was the AD 1596 Keicho Earthquake. It thus seems reasonable to suggest that the Higashiura fault was, at least in part, the source of the AD 1596 Keicho Earthquake.

VIII.—Note on a Species of Scymnus from the Upper Tertiary Formation of New Zealand

1888 ◽  
Vol 5 (7) ◽  
pp. 315-316 ◽  
Author(s):  
James W. Davis
Keyword(s):  
New Zealand ◽  
Geological Survey ◽  
Director General ◽  
Small Tooth ◽  
Royal Dublin Society ◽  
Fossil Fish ◽  
Fish Remains

In a Memoir recently published “On the Fossil Fish Remains of the Tertiary and Cretaceo-Tertiary Formations of New Zealand” (Transactions of the Royal Dublin Society, vol. iv. ser. II. p. 11, pl. vi. fig. 22) there is described a small tooth as an immature example of Carcharodon angustidens, Ag. The specimen was included amongst a large number of others forwarded for examination by Sir James Hector, Director-General of the Geological Survey of New Zealand; it is a small tooth, exquisitely preserved, and does not exhibit any signs of abrasion by use, which led to its being provisionally considered as the tooth of a young shark, and its form and minutely serrated margin appeared to indicate that its relationship was with Carcharodon.

scholarly journals Creating Synthetic Wind Speed Time Series for 15 New Zealand Wind Farms

2011 ◽  
Vol 50 (12) ◽  
pp. 2394-2409 ◽  
Author(s):  
Richard Turner ◽  
Xiaogu Zheng ◽  
Neil Gordon ◽  
Michael Uddstrom ◽  
Greg Pearson ◽  
...  
Keyword(s):  
Time Series ◽  
New Zealand ◽  
Wind Speed ◽  
Wind Farm ◽  
Central Government ◽  
Wind Farms ◽  
Practical Method ◽  
Wind Data ◽  
Regulatory Oversight ◽  
Short Period

AbstractWind data at time scales from 10 min to 1 h are an important input for modeling the performance of wind farms and their impact on many countries’ national electricity systems. Planners need long-term realistic (i.e., meteorologically spatially and temporally consistent) wind-farm data for projects studying how best to integrate wind power into the national electricity grid. In New Zealand, wind data recorded at wind farms are confidential for commercial reasons, however, and publicly available wind data records are for sites that are often not representative of or are distant from wind farms. In general, too, the public sites are at much lower terrain elevations than hilltop wind farms and have anemometers located at 10 m above the ground, which is much lower than turbine hub height. In addition, when available, the mast records from wind-farm sites are only for a short period. In this paper, the authors describe a novel and practical method to create a multiyear 10-min synthetic wind speed time series for 15 wind-farm sites throughout the country for the New Zealand Electricity Commission. The Electricity Commission (known as the Electricity Authority since 1 October 2010) is the agency that has regulatory oversight of the electricity industry and that provides advice to central government. The dataset was constructed in such a way as to preserve meteorological realism both spatially and temporally and also to respect the commercial secrecy of the wind data provided by power-generation companies.

New Zealand: A Current Analysis of the New Zealand Serious Fraud Office

1998 ◽  
Vol 6 (2) ◽  
pp. 195-199 ◽  
Author(s):  
Shaista Shameem
Keyword(s):  
New Zealand ◽  
Financial Crisis ◽  
Current Analysis ◽  
Department Of Justice ◽  
Corporate Fraud ◽  
Short Period ◽  
Set Up ◽  
A Current

The New Zealand Serious Fraud Office (NZSFO) was set up in 1989 in response to issues arising out of the 1980s financial crisis, in particular the share‐market crash of 1987. In the short period of about a year the total sum thought to be involved in corporate fraud schemes in New Zealand had increased dramatically, from NZ$10m–15m before 1988 to NZ$50m–70m in 1989. Consequently, the Department of Justice proposed setting up a specialist institution and legal mechanisms for the investigation of serious or complex fraud.

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