A pattern of arrests for drink driving in Hobart,Tasmania

The locations of arrests for drink driving in Hobart show a distinct concentration in the city centre. It is suggested that the distribution and characteristics of alcohol outlets and the related behaviour of certain groups led to a spatial and temporal clustering of impaired drivers. Disposition of breath testing units probably gives a simultaneous concentration of police activity in the city centre. Examination of home/arrest distances hints at the presence of parochial drinkers and drinkers using relatively distant venues which has some implications for intervention strategies. Long‐distance drivers are mainly young and attending hotels in the city centre whilst local drinkers are older.     

PETROLOGICAL CHARACTER OF THE LUNA 16 SAMPLE FROM MARE FECUNDITATIS

We have classified 1858 lithic and vitreous fragments from the Luna 16 core-tube sample. They were taken from the soil fractions ranging in size from 150 to 425 μ, at levels A and G (γ). No important differences are observed between the proportions of particle types in levels A and G, nor between the soils of Luna 16 and those from the Apollo 11 landing site in the nearby Mare Tranquillitatis. Luna 16 basalts are texturally and mineralogically similar to Apollo 11 basalts, though the former are characterized by more Fe-rich olivines and pyroxenes and by lower ilmenite contents than are Apollo 11 basalts. The atomic ratio Al/Ti in Luna 16 basalt pyroxenes in about 1.5; Apollo 11 basalt pyroxenes have Al/Ti = 2.0, indicating the possibility of a lower mean valence for Ti in the Luna 16 material than in the Apollo 11 material. Most light-colored lithic fragments are anorthositic rather than noritic in character and are comparable to Apollo 11 anorthosites in mineral chemistry. We believe they are samples of terra regions to the north of the Luna 16 landing site. Triangular diagrams plotting normative plagioclase, normative mafics plus oxides, and normative orthoclase plus apatite neatly separate the three major types of lunar materials — mare basalts, anorthosites, and noritic rocks — and reveal that the Luna 16 regolith is composed of mare basalt and anorthosite, with very little norite component. Colorless-to-greenish glass occurs in the Luna 16 sample, which has high Fe and low Ti; it may represent gabbroic rock related to the anorthosites     

Solar flares in the extreme ultraviolet

Solar-flare observations in the extreme ultraviolet (300–1350 Å) are reported. Some 269 flares observed by the Harvard College Observatory (HCO) experiment on OSO 4 and 211 flares observed by the HCO experiment on OSO 6 have been analyzed. The flares were observed in spectral lines and continua emitted by many ionic species over a temperature range from 10⁴ to 3.5 × 10⁶ K. The EUV data have been correlated with X-ray, H, and radio observations, and a significant number of EUV bursts not associated with reported H, X-ray, or radio bursts have been iden tified and investigated. The results indicate that these latter EUV events are less energetic by about a factor of 2 than EUV bursts associated with — F subflares.     

Coast erosion at Aberystwyth; the geological and human factors involved

The northern portion of the promenade at Aberystwyth is at present dangerously vulnerable to wave attack. The main factor involved is the geological evolution of the coastline which now strictly limits the available protective shingle and sand cover. The action of man, in building harbour protection works, protective sea walls and groynes, has had unforeseen consequences.