scholarly journals NEW HAMPSHIRE HESPERIDÆ

1896 ◽  
Vol 28 (6) ◽  
pp. 162-164 ◽  
Author(s):  
W. K. Fiske
Keyword(s):  

All of the following species occur in the town of Webster, about ten miles north-west of Concord:—Carterocephalus Mandan, Edw.—This is one of the rarest species in this section. It occurs in but one locality—a grassy bank by the roadside. Middle of June.Ancyloxypha Numitor, Fab.—Common around very wet, grassy swamps in June and again in August.

1993 ◽  
Vol 24 ◽  
pp. 1-18 ◽  
Author(s):  
D. D. Gilbertson ◽  
C. O. Hunt ◽  
N. R. J. Fieller

AbstractThis paper describes an integrated series of sedimentological and palynological studies of the arenaceous deposits which infill the large alluvial basin of Grerat D'nar Salem, which is located on a limestone plateau in the semi-arid pre-desert of Tripolitania north-west of the town of Beni Ulid. This research shows that in the early and middle Holocene this depression was occupied by a large semi-permanent or permanent water body which was surrounded by a grass-steppe vegetation with some tree and shrub species, perhaps growing in wetter stream- and wadi-beds. Sometime in the mid-Holocene the region became much more arid, the lake disappeared, matching the pattern of environmental change observed elsewhere in northern Africa. The geomor-phic environment became dominated by aeolian processes, interrupted by occasional winter floods, in a landscape dominated by grass steppe — essentially the situation that has continued to the present day. It is clear from general biogeographical and geomorphic considerations that Romano-Libyan floodwater farming in the region must have brought about significant changes in the character of wadi floors. Field survey indicates that it has also left a legacy in the contemporary distribution of plants, animals and runoff in the modern landscape. Nevertheless, no clear evidence has emerged from this study that the widespread and intensive flood-water farming, evidenced by the archaeological remains in the area, was associated with either a climate or a landscape notably different from that of today. The new palynological evidence suggests that the nature of the related ancient cultivation at Grerat is better viewed as a monoculture, rather than the mixed farming deduced previously for wadi-floor areas. There is no evidence that any naturally-occurring environmental change was associated with the introduction or loss of floodwater farming in the region. There is some sedimentological evidence that such activity might have led to problems of soil salinity in this basin.


1973 ◽  
Vol 1 (4) ◽  
pp. 39-42
Author(s):  
Eric D. Howlett

The Carpentaria Kindergarten is the Community Preschool Centre at Normanton, in north-west Queensland. It was established in 1970 under the auspices of the Anglican Church with financial assistance from the Department of Aboriginal Affairs, Canberra. Of the fifty children enrolled approximately 80% are of Aboriginal descent. All children in the town are encouraged to attend after their third birthday. The younger children attend three afternoons a week, while the older children attend five morning sessions a week. In most cases children have two years of preschool education before they enter the primary school.The preschool is an instrument of integration in this community which has a 50% Aboriginal population. It is recognized that the principle of community integration is based on the movement of different types within a community together, with each group making a real contribution. Consequently the Aboriginal people must not disappear in a process of absorption, but move into the total community with a definite identity. The preschool plays a very real and definite support role in this process of integration in the following ways:


1946 ◽  
Vol 40 (5) ◽  
pp. 962-965
Author(s):  
Lashley G. Harvey

Although legally buried since 1891, the “precinct” in New Hampshire, like Banquo's ghost, continually arises to baffle students of New England local government. To the lawmakers, it is known as the village district; while in its annual report the state tax commission lists village districts as precincts, only adding to the confusion.In making a count of governmental areas in New Hampshire, one finds the state divided into ten counties. Within these, there are eleven municipalities classed as cities and 224 towns. The cities were once towns, but have been incorporated as cities by the legislature, not in accordance with a population prerequisite, but upon application. The first city to be incorporated was Manchester in 1846.All New Hampshire cities and towns include within their limits a great deal of rural land. Clusters of houses or settlements are sprinkled over these areas. Frequently, a settlement has several stores, a post office, and a railroad station and has the outward appearance of a village. Legally, however, such a settlement is not a village. It is administered entirely as a part of the town or city in which it is located, although it may be several miles from the principal urban center. New Hampshire has 639 such settlements, none of which is incorporated. Villages are not incorporated in New Hampshire as they are in Connecticut, Vermont, and Maine. Frequently they are referred to as places, but they should not be confused with the 23 so-called “unincorporated places” (found principally in the White Mountains), which are administered by the county and state governments almost completely. However, there are a few of the “villagelike” settlements within unincorporated places.


2018 ◽  
Vol 1 (123) ◽  
pp. 45-62
Author(s):  
Ahmed Abbas

The QADIS survey project is a joint initiative of the Alma Mater Studiorum - University of Bologna and the State Board of Antiquities and Heritage (SBAH). The findings presented here were analyzed in the frame of the EU funded project "EDUU - Educational and Cultural Heritage Enhancement for Social Cohesion in Iraq" (EuropeAid CSO-LA/2016/382-631). The first, second and third field seasons took place in January and October 2016 and in January 2017 respectively. We report here on the general survey activities of the first two seasons, providing detailed information on 40 sites newly identified in addition to Adams 1981. The survey area (Fig. 1) follows the administrative borders of the region of Qadisiyah to the South and East (including part of the Delmej basin), and it stops around the town of Afak to the North-West.1


Author(s):  
C Gouws ◽  
I Moeketsi ◽  
S Motloung ◽  
G Van Greuning ◽  
Llewellyn Van Zyl

In 2007 the residents of the town of Sannieshof in North West Province declared a dispute with the Tswaing Local Municipality on the grounds that the state of local service delivery left much to be desired. The ratepayers then formed the Sannieshof Inwoners Belastingbetalers Unie (SIBU) which literally took over the functions of local government of the town, functioning as a local government within a local government.This article provides a historical narrative of the conflict between SIBU and Tswaing Local Municipality, a dispute which was taken as far as the provincial High Court. Then follows an outline of conditions in Sannieshof and the townships of Agisanang and Phelindaba. Attention is given to the perceptions of local residents on the prevalent conditions, specifically in respect of water supply and sanitation service delivery. In the third section there are some theoretical perspectives on political culture, socialisation and happiness. A debate is provided on how these phenomena manifest under existing conditions in Sannieshof, and more particularly, in its adjacent townships of Agisanang and Phelindaba.


1982 ◽  
Vol 110 ◽  
pp. 38-43
Author(s):  
L.M Larsen ◽  
A.K Pedersen

In addition to the two large carbonatite complexes of Cambrian age occurring in southern West Greenland, the Sarfartôq and Qaqarssuk complexes (Secher & Larsen, 1980; Gothenborg & Pedersen, 1975) a third small intrusion of carbonatite was found in 1971 during regional prospecting by Kryolitselskabet Øresund A/S. This intrusion is situated approximately 50 km east of the town Sukkertoppen, only 11 km north-north-west of the Qaqarssuk complex of which it may be regarded as a satellite (fig. 13). The outcrop measures only 500 m by 200 m. It is situated on a gently south-east sloping, relatively vegegation covered hillside in a depression between 800 m and 1000 m high mountains, the most prominent of which is Tupertalik ('the place with a tent') after which the intrusion is named.


2019 ◽  
Vol 63 (4) ◽  
pp. 769-798
Author(s):  
Marcel Schlechtweg ◽  
Holden Härtl

Quotation marks are a tool to refer to the linguistic form of an expression. For instance, in cases of so-called pure quotation as in “Hanover” has three syllables, they point to the syllabic characteristics of the name of the town of Hanover. Cases of this nature differ from sentences like Hanover is a town in New Hampshire, in which Hanover is used denotationally and, thus, refers to the town of Hanover itself. Apart from quotation marks, other means such as italics, bold, capitalization, or air quotes represent potential means to signal a non-stereotypical use of an item in the written or gestural mode. It is far less clear, however, whether acoustic correlates of quotation marks exist. The present contribution aims at investigating this issue by focusing on instances of quotation, in which the conventionalized name of a lexical concept is highlighted by means of quotation marks, either together with or without an additional lexical quotational marker, such as so-called, on the lexical level (cf. The so-called “vuvuzela” is an instrument from South Africa vs. The “vuvuzela” is an instrument from South Africa). The data clearly show that quotation marks are pronounced, primarily triggering a lengthening effect, independently of whether they appear together with or without a name-informing context. The results of the experiments are interpreted against the background of a pragmatic implementation of quotation marks in general as well as in spoken discourse in particular.


Radiocarbon ◽  
2007 ◽  
Vol 49 (2) ◽  
pp. 625-637 ◽  
Author(s):  
Danuta Michalska Nawrocka ◽  
Danuta Joanna Michczyńska ◽  
Anna Pazdur ◽  
Justyna Czernik

Carbonate binders from mortars and plasters as well as charcoal fragments sampled at the ancient settlement of Hippos (Sussita) have been subjected to radiocarbon dating by gas proportional counting (GPC) and accelerator mass spectrometry (AMS). Hippos is situated on the east coast of the Sea of Galilee (32°46′N, 35°39′E) at the top of a hill in the Golan Heights area, Israel. According to historical-archaeological data, the town had functioned since the 3rd century BC until AD 749, when it eventually crumbled into ruins after an earthquake. The appropriate sample selection and preparation based on the results of petrographic observations permitted us to distinguish different phases involved in the expansion of the settlement. More than 200 samples were taken from the settlement and subjected to petrographic and chemical analyses. Of the 200 total samples, about 20 were selected for dating. Here, we present the first 10 results of 14C dating carried out for Hippos. The oldest sample dated thus far gave an age corresponding with the 2nd century BC to 1st century AD—probably indicating an old Roman temple, on the base of which the North-West church (NWC) was later erected. The next dates extend up to the 8th century AD, the age related to the last phase of settlement inhabitation. Research is continuing as new excavations take place.


2001 ◽  
Vol 23 (1) ◽  
pp. 71 ◽  
Author(s):  
PM Johnson ◽  
MDB Eldridge ◽  
V Kiernan ◽  
RJ Cupitt

IN 1982, the Queensland subspecies of the blackfooted rock-wallaby Petrogale lateralis purpureicollis was reported to occur around Mt Isa and south to around Dajarra (Briscoe et al. 1982). During 1991, the known range of this taxon was extended 300 km to the north-west when an adult female P. l. purpureicollis was collected from ?Ridgepole Waterhole? in the Musselbrook Resource Reserve near Lawn Hill National Park (Eldridge et al. 1993). In 1994 the range was further extended when P. l. purpureicollis was recorded from the Constance Ranges and the upper reaches of Stockyard and Elizabeth Creeks; around the town of Cloncurry and the following distances from the town: 85 km north west; 60 and 87 km west; 4, 23, 28 and 35 km south and 15 km east (Bell et al. 1995). Approaches by the Cannington Mining operation to the southwest of McKinley in October 1999 to confirm the presence of rock-wallabies on nearby Glenholme Station established the presence of P. l. purpureicollis; a 75 km range extension to the south-east.


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