Memoir on the Character and Prospects of the Copper Region of Gibara, and a Sketch of the Geology of the North-East Part of the Island of Cuba

1845 ◽  
Vol 9 (2) ◽  
pp. 204 ◽  
Author(s):  
Rich. C. Taylor
Keyword(s):  
East Part ◽  
North East ◽  
The North

TBE in Italy

2019 ◽  
Author(s):  
Valentina Tagliapietra ◽  
Flavia Riccardo ◽  
Giovanni Rezza
Keyword(s):  
Case Series ◽  
East Part ◽  
Mountainous Regions ◽  
North East ◽  
The North ◽  
Tick Borne Encephalitis ◽  
Low Incidence

Italy is considered a low incidence country for tick-borne encephalitis (TBE) in Europe. Areas at higher risk for TBE in Italy are geographically clustered in the forested and mountainous regions and provinces in the north east part of the country, as suggested by TBE case series published over the last decade.

SEJNEŃSKI OŚRODEK KOŚCIELNY (WYBRANE ZAGADNIENIA)

2016 ◽  
Vol 10 (2) ◽  
pp. 87-97
Author(s):  
Wojciech W Guzewicz
Keyword(s):  
East Part ◽  
North East ◽  
The North ◽  
Registered Office

Sejny is situated in the north-east part of Poland, in the diocese Elk. Here among othersa parish is located near a sanctuary of NMP hitting and the registered office of the Sejny deanery.It is a city of the borderland, cultures and nations. Presenting landmarks in the life to thecongregation, describing the infrastructure and populations are a purpose of the article, as well asdiscussing the most important punished monuments of this earth.

scholarly journals PHENOLIC PROFILE OF HONEYDEW HONEYS FROM THE NORTH-EAST PART OF ROMANIA

2016 ◽  
Vol 73 (2) ◽  
pp. 105
Author(s):  
Mircea OROIAN ◽  
Sorina ROPCIUC ◽  
Amalia BUCULEI ◽  
Sergiu PADURET ◽  
Elena TODOSI
Keyword(s):  
European Union ◽  
Moisture Content ◽  
The European Union ◽  
Free Acidity ◽  
Glucose Content ◽  
Phenolic Profile ◽  
East Part ◽  
North East ◽  
The North ◽  
Acidic Nature

The aim of this study is to determine the physicochemical (moisture content, pH, free acidity, electrical conductivity, colour (L*, a*, b*, chroma, hue angle), ash content, fructose and glucose content) and to determine the phenolic profile (quercetin, apigenin, myricetin, isorhamnetin, kaempherol, caffeic acid, chrysin, galangin, luteolin, p-coumaric acid, gallic acid and pinocembrin) of five samples of honeydew honeys from the North East part of Romania. The honey samples analysed respected the maximum allowable level of the moisture content, which is established by the European Union at 20%. The acidic nature of the honeydew is confirmed by the level of the pH and free acidity of the samples, and is influenced in principal by the organic acids; all the samples had a free acidity lower than 50 meq acid/kg. The honey colour is dark which is confirmed by the level of the CIE L*a*b* parameters (lower values of L*, a* and b*). The inverted sugar level (fructose and glucose content) is higher than 60 g/ 100g, respecting the European Union directive. The phenolic profile of the honeydew samples do not presented one compound that can be considered a chemical marker, the major polyphenols presented into the honeydew honeys are quercetin and pinocembrin.

scholarly journals Aircraft measurements of aerosol black carbon from a coastal location in the north-east part of peninsular India during ICARB

2008 ◽  
Vol 117 (S1) ◽  
pp. 263-271 ◽  
Author(s):  
S. Suresh Babu ◽  
S. K. Satheesh ◽  
K. Krishna Moorthy ◽  
C. B. S. Dutt ◽  
Vijayakumar S. Nair ◽  
...  
Keyword(s):  
Black Carbon ◽  
Aircraft Measurements ◽  
Peninsular India ◽  
East Part ◽  
North East ◽  
The North

scholarly journals LXXXIX. Observations on the same eclipse

1761 ◽  
Vol 52 ◽  
pp. 543-543
Keyword(s):  
East Part ◽  
North East ◽  
The North

A discernible penumbra on the north-east part of the Moon’s limb.

scholarly journals K/Ar age determinations from western Greenland II. The Ivigtut region

1968 ◽  
Vol 15 ◽  
pp. 87-91
Author(s):  
O Jørgensen
Keyword(s):  
Fold Belt ◽  
East Part ◽  
North East ◽  
The North ◽  
Fold Belts ◽  
Age Determinations

The Ivigtut region is particularly remarkable for providing one of the best known examples of the transition between two Precambrian fold belts (Henriksen, in press; Allaart, Bridgwater and Henriksen, in press). In the north-east part of the area sediments and volcanics of the Ketilidian fold belt lie with a pronounced unconformity on gneisses and schists of the pre-Ketilidian basement. Traced southwards the Ketilidian supracrustal rocks show an increasing grade of metamorphism and the unconformity with the underlying basement is gradually obliterated as the basement becomes increasingly reactivated.

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