The Climate, Environment and Industries of Stone Age Greece: Part III

1968 ◽  
Vol 33 ◽  
pp. 1-29 ◽  
Author(s):  
E. S. Higgs ◽  
C. Vita-Finzi ◽  
D. R. Harris ◽  
A. E. Fagg ◽  
S. Bottema
Keyword(s):  
Environmental Changes ◽  
Structural Factors ◽  
The South ◽  
Human Occupation ◽  
North West ◽  
North East ◽  
The North ◽  
Last Glaciation ◽  
South West ◽  
Maximum Elevation

In the second article of this series, brief mention was made of a cave at Kastritsa, near Lake Ioannina, whose talus had yielded an industry reminiscent of the last phase at the shelter of Asprochaliko. The evidence for an increase in the size of Lake Ioannina during the Last Glaciation was also outlined. The purpose of this paper is to consider the concomitant environmental changes in relation to the evidence for human occupation.Lake Ioannina lies at 469 metres above sea-level. To the north-east stands the Mitsikeli ridge, with a maximum elevation of 1,810 metres and separated from the Pindus range by the gorge of the upper Arakhthos (fig. 1). To the south-west lies the Tomarokhoria plateau, which in places rises to over 1,900 metres. The basin, a typical polje, is cradled by limestones which range in age from the Upper Triassic to the Upper Eocene. The Flysch of the Pindus borders it on the south-east. The lake lies along the axis of the Perama syncline, which runs north-west-south-east parallel to the Mitsikeli anticline and the Stavraki anticline; faulting is common. The basin would seem to owe its existence primarily to structural factors, although solution doubtless contributed to its present form.

Part VI. The Cyclopean Terrace Building and the Deposit of Pottery beneath It

1954 ◽  
Vol 49 ◽  
pp. 267-291
Author(s):  
Elizabeth B. Wace
Keyword(s):  
Contour Line ◽  
The South ◽  
Main Road ◽  
North West ◽  
North East ◽  
The North ◽  
South West

The Cyclopean Terrace Building lies to the north-west of the Lion Gate on the northern end of the Panagia Ridge and faces almost due west across the valley of the Kephissos and modern main road from Corinth to Argos. It lies just below the 200 m. contour line, and one terrace below the houses excavated in 1950–51 by Dr. Papadimitriou and Mr. Petsas to the east at the same end of the ridge. The area contains a complex of buildings, both successive and contemporary, and in view of the discovery of structures both to the south-west and, by the Greek Archaeological Service, to the north-east it is likely that this whole slope was covered by a portion of the outer town of Mycenae. This report will deal only with the structure to which the name Cyclopean Terrace Building was originally given, the so-called ‘North Megaron’, supported by the heavy main terrace wall.The excavation of this structure was begun in 1923. The main terrace wall was cleared and two L.H. IIIC burials discovered in the top of the fill in the south room. In 1950 it was decided to attempt to clear this building entirely in an endeavour to find out its date and purpose. The clearing was not, however, substantially completed until the close of the 1953 excavation season, and this report presents the available evidence for the date as determined by the pottery found beneath the building; the purpose is still a matter for study, though various tentative conclusions can be put forward.

III.—On the Discovery of a Quartzose Conglomerate at Caldon Low, Staffs

1919 ◽  
Vol 6 (2) ◽  
pp. 59-64 ◽  
Author(s):  
J. Wilfrid Jackson ◽  
W. E. Alkins
Keyword(s):  
The South ◽  
North West ◽  
Good Fortune ◽  
North East ◽  
The North ◽  
South West ◽  
Limestone Quarries ◽  
Strong Joint

During a visit to the limestone quarries at Caldon Low last September we had the good fortune to discover an interesting exposure of a quartzose conglomerate containing numerous fossils. The bed was exposed in a strong joint-face running approximately N.N.W. to S.S.E., at the northern extension of the quarry on the north-west flank of the Low, just beyond the mineral line of the North Staffordshire Railway. The altitude is about 900 feet O.D. The conglomerate apparently extended some little distance to the south-west before the opening of the quarry, as we ascertained that some 20 or 30 yards had been removed in gaining access to the limestone behind. It appears to extend for some distance round the flank of the Low towards the north-east.

scholarly journals Kos Astypalaia

1898 ◽  
Vol 4 ◽  
pp. 95-100
Author(s):  
Duncan Mackenzie
Keyword(s):  
The Other ◽  
Mountain Region ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
South West ◽  
The Village

From the modern town of Kos, on the site of the ancient capital at the north-east extremity of the island, to the village of Kephalos at the southwest end is a ride of eight hours.The village stands on a chalky plateau which beyond the isthmus marks the beginning of the mountain district of south-west Kos. This in turn is a repetition on a smaller scale of the mountain region, at the other end of the island, which forms the lofty termination to the long central tableland. The highest points of the mountain district are towards the south-east where the fall to the sea is very rapid. The highest neighbouring peak, Mount Ziní, is about an hour distant from the village in a south-easterly direction, while all that lies to the north-west of the main range is high pastoral country with many torrent beds.

scholarly journals Subnational estimates of maternal mortality in Nigeria: Analysis of female siblings’ survivorship histories. 

2021 ◽  
Author(s):  
Opeyemi Oluwatosin Babajide ◽  
Joshua Odunayo Akinyemi ◽  
Olusola Ayeni
Keyword(s):  
Maternal Mortality ◽  
Rural Areas ◽  
Small Area ◽  
Demographic And Health Surveys ◽  
The South ◽  
Mortality Trends ◽  
North West ◽  
North East ◽  
The North ◽  
South West

Abstract BACKGROUND High Maternal Mortality (MM) in Nigeria is further complicated by the lack of reliable estimates for subnational levels such as states and geopolitical regions. Disaggregating maternal mortality estimates by subnational levels is crucial to ensuring policy decisions and program implementation are adapted to areas with a high burden of mortality. This study involves a novel adaptation of small area estimation techniques to derive plausible estimates of levels and trends in Maternal Mortality rates and ratios for states and geopolitical regions in Nigeria. METHODS. Survivorship history data of 293,769 female siblings were provided by 114,154 women in the Nigeria Demographic and Health Surveys of 2008, 2013 and 2018. MM Rates and Ratios were estimated using the Empirical Bayesian technique for small area demographic estimates. The James-Stein estimator was used to shrink the estimates closer to the population mean values with 95% Confidence Interval (CI). RESULTS Levels of MMRatio were highest in the rural areas, States and regions in Northern Nigeria. MMRatio was consistently lower in the South West (2008=281; 2013=367; 2018=392) and higher among the Northern regions of the country, particularly the North-East (2008=654; 2013=612; 2018=901) for three consecutive surveys. Over the three surveys, mortality trends declined about 18% in the North West and 54.2% in the South East region. However, there was a 4.8% increase in MMRatio for South West between 2008 to 2018. CONCLUSIONS Nigeria has geopolitical and sub-national disparities that pose a burden to the country’s maternal health. Since several states in the Northern geopolitical zone still show high maternal mortality, targeted intervention at state levels should be explored to ensure that mothers who need help get it to ensure the sustainable development goals are met.

GEOGRAPHICAL VARIATION AND MIGRATION ANALYSIS OF HEIGHT, WEIGHT AND BODY MASS INDEX IN A BRITISH COHORT STUDY

2011 ◽  
Vol 43 (6) ◽  
pp. 733-749 ◽  
Author(s):  
MONIKA KRZYŻANOWSKA ◽  
C. G. NICHOLAS MASCIE-TAYLOR
Keyword(s):  
Body Mass Index ◽  
Body Mass ◽  
The South ◽  
Negative Effects ◽  
North West ◽  
North East ◽  
The North ◽  
South West ◽  
East Midlands ◽  
West Midlands

SummaryUsing a sample of 2090 father and son pairs, the regional variation in height, weight and body mass index (BMI) with intra- and inter-generational migration within Britain was examined. Highly significant regional differences in means were found only for fathers. The overall mean height difference between regions ranged from about 2.7 cm to 3.1 cm, with the tallest fathers being found in the East & South-East region and the shortest in Wales. The variation in mean weight between regions was less significant, with the difference between the heaviest region (West Midlands) and lightest (South-West) being about 3.5 kg. For BMI the highest mean was in the North and Wales and the lowest in the South-West (difference of about 1 kg m−2). Intra-generational migrants were, on average, significantly taller than non-migrants for both fathers (+1.4 cm) and sons (+2 cm), but BMI was only significant in fathers, with migrant fathers, on average, having a lower BMI. There were no significant differences in weight between geographically mobile groups for either fathers or sons. Differentiating between regional in- and out-migration revealed that in the fathers' generation in-migrants were taller, on average, in six of the nine regions. The tallest in-migrants among fathers came into the North region; the tallest out-migrants were from Yorkshire & Humberside and the shortest were from Scotland. The largest positive gain on fathers' height was in the West Midlands region and Scotland, while negative effects were found in the Yorkshire & Humberside, East Midlands and East & South-East regions. For sons in-migrants were taller in all regions except Wales, with the largest differences between in-migrants and non-migrants being in the South-East and South-West. For out-migrants, the tallest sons came from Wales, while the shortest came from the East Midlands region. The North, East Midlands, East & South-East and West Midlands regions were net gainers, while Wales and Scotland were net losers. For BMI among fathers, in-migrants were of lower BMI than non-migrants. For out-migrant fathers, the North-West and South-West regions were the only two regions showing positive values, with the largest negative values being found in the East Midlands and Yorkshire & Humberside. The net effect of migration indicated that the largest gains were in the East Midlands and Yorkshire & Humberside regions and the largest losses were in Scotland and Wales. The inter-generational migration for BMI showed that in-migrating sons into the North-West and Wales had higher BMI than sedentes, while in-migrants into Yorkshire & Humberside were lower in BMI. In all regions out-migrants had lower BMI than non-migrants. The net effect of migration revealed that six of the nine regions were net gainers, while the Yorkshire & Humberside region was a net loser.

scholarly journals IX-XII. FOSSIL LOCALITIES, FAUNAL LISTS & INDEX OF BRACHIOPOD GENERA AND SPECIES

1962 ◽  
Vol 3 (1) ◽  
pp. 255-256
Keyword(s):  
List Type ◽  
The South ◽  
North West ◽  
Eastern Side ◽  
North East ◽  
The North ◽  
North Side ◽  
South West ◽  
North Bank

ExcerptFossil collections have been obtained from a large number of localities in the Girvan area. Most of them have been referred to in the text, but those described below are localities from which figured material and types have been obtained.(a) AUCHENSOUL LIMESTONE AND CONFINIS FLAGS(1) Red mudstones and limestone breccias exposed on the south bank of the River Stinchar, 100 yards east of the bridge leading to Auchensoul Farm, 1i88 miles out of Barr on the Pinmore road (Auchensoul Limestone and Mudstones, Auchensoul Bridge).(2) Brown- and yellow-weathering calcareous confinis siltstones exposed on the hillside, 100 yards west of Struit Well, 300 yards west-north-west of Kirkdominae ruins on the north side of the Stinchar Valley, 1i89 miles west of Barr (confinis Flags, Kirkdominae Hill).(3) Brown-weathering calcareous confinis siltstones exposed in the bank of the pathway leading from the old limekiln to the quarry excavated in Stinchar Limestone, 450 yards west-south-west of Minuntion Farm on the north side of the River Stinchar and about 1i89 miles north-east of Pinmore bridge (confinis Flags, Minuntion).(4) Yellow-weathering, pebbly siltstones and impure nodular limestones transitional from confinis Flags to Stinchar Limestone, exposed on the eastern side of the water-filled quarry 300 yards south-west of Bougang Farm, 3 miles east of Ballantrae on the ColmoneU road (top of the confinis Flags, Bougang).(b) STINCHAR LIMESTONES AND SUPERSTES MUDSTONES (1) Mudstones with nodular limestones exposed on the north bank of the Water of Gregg, half a mile east of its junction with the

Leeuwin current and wind distributions on the southern part of the Australian North West Shelf between January 1982 and July 1983

1985 ◽  
Vol 36 (2) ◽  
pp. 123 ◽  
Author(s):  
PE Holloway ◽  
HC Nye
Keyword(s):  
Low Frequency ◽  
Maximum Speed ◽  
The South ◽  
Coastal Station ◽  
North West ◽  
Leeuwin Current ◽  
North East ◽  
The North ◽  
South West ◽  
Shelf Slope

Observations of the current and wind distributions on the southern part of the Australian North West Shelf between January 1982 and July 1983 are presented. Maps of monthly averages of winds and currents from a variety of locations are presented as well as some time series spanning 19 months of currents and water temperatures from a shelf-slope location and corresponding winds from a coastal station. The main feature of the observations is the strong flow to the south-west parallel to the bathymetry known as the Leeuwin Current. From the observations across the continental shelf, the low-frequency flow is strongest over the shelf break reaching a maximum speed of approximately 0 25 m s-1. The current is strongest between February and June. Reversals of the flow to the north- east are usually weak in strength and of short duration and are associated with strong south-west winds. However, observations of water temperature suggest the north-east currents cause weak upwelling events of cold deep water onto the shelf. The south-east trade winds blow from the south- east between March and August, but are shown to be inefficient in generating longshore currents to the south-west and hence in strengthening the Leeuwin Current.

scholarly journals The Igneous Complex of Y Foel Fras, Caernarvonshire

1922 ◽  
Vol 59 (3) ◽  
pp. 134-139 ◽  
Author(s):  
Norman L. Silvester
Keyword(s):  
Coastal Plain ◽  
Geological Survey ◽  
The South ◽  
The West ◽  
Igneous Complex ◽  
North West ◽  
North East ◽  
The North ◽  
South West

The area under consideration is a portion of the mountain massif bounded on the east by the Conway River, on the north by the narrow coastal plain between Conway and Bangor, and on the west and south by the popular tourist route through Nant.-Francon pass by Llyn Ogwen and down the Afon Llugwy to Bettws y coed. The investigation includes the horseshoe-shaped ring of mountains, of which the highest is Y Foel Frâs (3,091 feet), surrounding the upper course of the Aber River (Cwm yr Afon Goch). To the north-west this igneous complex is bounded by the precipitatious crags over which the above stream descends by leaps and bounds, forming the well-known Aber Falls. Upon Sheet 78, south-east of the old Geological Survey map the area is coloured as “Massive intrusive felspathic rocks”, surrounding two oval patches indicated as “Greenstones”, whilst a further elongated patch of the latter forms the south-west boundary. The north-east boundary is limited by the Aber-Llanbedr fault. Besides the hog-backed summit of Y Foel Frâs, the area includes the similarly outlined summits of Y Drosgl West (2,483 feet), Yr Arryg (2,875 feet), Llwydmor Bâch (2,256 feet), and the more rugged summits of Bera Mawr (2,587 feet), Bera Bâch and Llwydmor (2,749 feet).

The Metamorphosed Limestones and Associated Contaminated Igneous Rocks of the Carlingford District, Co. Louth

1932 ◽  
Vol 69 (5) ◽  
pp. 209-233 ◽  
Author(s):  
G. D. Osborne
Keyword(s):  
Igneous Rocks ◽  
The South ◽  
Ordnance Survey ◽  
Igneous Complex ◽  
North East ◽  
The North ◽  
South West ◽  
Carboniferous Limestone ◽  
Contamination Effects

THE Carlingford-Barnave district falls within the boundaries of Sheet 71 of the Ordnance Survey of Ireland, and forms part of a broad promontory lying between Carlingford Lough on the north-east and Dundalk Bay on the south-west. The greater part of this promontory is made up of an igneous complex of Tertiary age which has invaded the Silurian slates and quartzites and the Carboniferous Limestone Series. This complex has not yet been investigated in detail, but for the purposes of the present paper certain references to it are necessary, and these are made below. The prevalence of hybrid-relations and contamination-effects between the basic and acid igneous rocks of the region is a very marked feature, and because of this it has been difficult at times to decide which types have been responsible for the various stages of the metamorphism.

scholarly journals Regional Differences in Postnatal Care Service Utilisation and Child Morbidity in Nigeria: Evidence from 2018 Nigeria Demographic and Health Survey (NDHS)

2020 ◽  
Author(s):  
Endurance Uzobo ◽  
Aboluwaji D. Ayinmoro
Keyword(s):  
Socioeconomic Factors ◽  
Health Survey ◽  
Postnatal Care ◽  
Demographic And Health Survey ◽  
The South ◽  
North Central ◽  
North West ◽  
North East ◽  
South West ◽  
Child Morbidity

Abstract Introduction: Modern Postnatal Care Services (PNC) in Nigeria is vital tool for providing quality health for mothers and newborns. Nonetheless, many regions in Nigeria are still struggling to achieve optimum utilisation of modern PNC services due to variation in associated socioeconomic factors of mothers based on their regions. This study aims at assessing regional socioeconomic factors associated with PNC services utilisation and its relationship with child morbidity in Nigeria. Methods Data for this study was extracted from the Nigeria Demographic and Health Survey (NDHS) 2018 birth recoded file dataset, with a sample size of 30713 women (aged 15–49). Data were analysed using descriptive statistics, Chi-Square Test and logistic regression. The main predictor variable was the region, while others included the type of PNC service utilised and various demographic variables of the respondents – age, education, type of residence, religion, ethnicity among others. Results The average age of the respondents was 29.5 ± 6.8. The use of modern PNC services ranged from South-West (20.3%), South-South (10.9%), South-East (23.0%), North-Central (22.0%), North-East (13.0%) to North-West (10.9%). The prevalence of child morbidity ranged from South-West (8.5%), South-South (9.8%), South-East (11.4%), North-Central (15.3%), North-East (26.3%) to North-West (28.7%). Child morbidity is significantly higher in the South-South (OR = 1.46), South-East (OR = 1.50), North-Central (OR = 1.13), North-East (OR = 2.31) and North-West (OR = 1.35) compared to the South-West. Conclusion Majority of women in Nigeria are not using modern PNC services. Regional variations in the use of PNC services and socio-demographic characteristics of mothers influence child morbidity in Nigeria. There is need for regional-specific context sensitisation for mothers in the use of modern PNC services.

Sign in / Sign up

Export Citation Format

Share Document