scholarly journals The Zelenchuk 6m Telescope (BTA) of the USSR Academy of Sciences

1982 ◽  
Vol 67 ◽  
pp. 3-9 ◽  
Author(s):  
B.K. Ioannisiani ◽  
E.M. Neplokhov ◽  
I.M. Kopylov ◽  
V.S. Rylov ◽  
L.I. Snezhko
Keyword(s):  
Sea Level ◽  
Ussr Academy ◽  
North Caucasus ◽  
The South ◽  
The North ◽  
Academy Of Sciences

AbstractA description is given of the alt-azimuth mounted 6-meter telescope (BTA) installed in the North Caucasus at an altitude of 2070m above sea level and about 40km to the south of Zelenchukskaya village. Some details of the BTA instrumentation and the local astroclimate are also reported.

V.—On the Cretaceous Fossils found at Moreseat, Aberdeenshire

1898 ◽  
Vol 5 (1) ◽  
pp. 21-32
Author(s):  
A. J. Jukes-Browne ◽  
John Milne
Keyword(s):  
Sea Level ◽  
The South ◽  
The North ◽  
Cretaceous Fossils

Moreseat is in the parish of Cruden, in the east of Aberdeenshire. It lies at an elevation of 300 feet above sea-level, and the surface of the ground slopes to the sea at Cruden Bay, distant five miles to the south. On the north the ground rises gradually, reaching the height of 450 feet above sea in Torhendry Ridge, which is strewn with chalk-flintsingreat abundance.

BIODIVERSITY OF WILD RUMINANTS HELMINTHS IN ECOSYSTEMS OF THE SOUTH-EAST OF THE NORTH CAUCASUS

2021 ◽  
pp. 121-124
Author(s):  
M.M. ZUBAIROVA ◽  
A.M. ATAEV ◽  
N.T. KARSAKOV ◽  
T.N. ASHURBEKOVA ◽  
A.N. KHASAEV
Keyword(s):  
North Caucasus ◽  
The South ◽  
Wild Ruminants ◽  
The North

scholarly journals New records of megachilid bees (Hymenoptera: Megachilidae) from the North Caucasus and the south of European Russia

2020 ◽  
Vol 16 (2) ◽  
pp. 225-331
Author(s):  
A.V. Fateryga ◽  
◽  
M.Yu. Proshchalykin ◽  
Keyword(s):  
New Records ◽  
Distinct Species ◽  
European Part ◽  
European Russia ◽  
North Caucasus ◽  
The South ◽  
The North ◽  
The Family ◽  
European Part Of Russia ◽  
South Of European Russia

New data on 22 species of bees of the family Megachilidae from the North Caucasus and the south of European Russia are reported. Six species are new to Russia: Hoplitis curvipes (Morawitz, 1871), Osmia cinerea Warncke, 1988, O. ligurica Morawitz, 1868, O. cyanoxantha Pérez, 1879, Protosmia glutinosa (Giraud, 1871), and Coelioxys mielbergi Morawitz, 1880. Hoplitis turcestanica (Dalla Torre, 1896), sp. resurr. is treated as a distinct species, not a junior synonym of H. caularis (Morawitz, 1875). Megachile albocristata Smith, 1853 and M. alborufa Friese, 1911 are listed instead of previously recorded M. lefebvrei (Lepeletier de Saint-Fargeau, 1841) and M. pyrenaica (Lepeletier de Saint-Fargeau, 1841), respectively. Fourteen new regional records are reported: seven species are new to the North Caucasus, five ones are new to the south of European Russia, and two species are new to the European part of Russia as a whole. The numbers of megachilid bee species currently known in Russia, the North Caucasus, and the south of European Russia are 217, 130, and 71, respectively. The lectotype of Osmia proxima Morawitz, 1875 is designated.

Prehistoric Roads and Tracks in Somerset, England: 2. Neolithic

1970 ◽  
Vol 36 ◽  
pp. 125-151 ◽  
Author(s):  
John M. Coles ◽  
F. Alan Hibbert ◽  
Colin F. Clements
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
The Third ◽  
The North ◽  
South West ◽  
Extensive Region ◽  
Peat Deposits ◽  
Third Millennium ◽  
South West England

The Somerset Levels are the largest area of low-lying ground in south-west England, covering an extensive region between the highlands of Exmoor, the Brendon Hills and the Quantock Hills to the west, and the Cotswold and Mendip Hills to the east (Pl. XXIII, inset). The Quantock Hills and the Mendip Hills directly border the Levels themselves, and reach heights of over 250 metres above sea level. The valley between extends to 27 metres below sea level, but is filled to approximately the height of the present sea by a blue-grey clay. The Levels are bisected by the limestone hills of the Poldens, and both parts have other smaller areas of limestone and sand projecting above the peat deposits that cap the blue-grey clay filling. In this paper we are concerned with the northern part of the Levels, an area at present drained by the River Brue.The flat, peat-covered floor of the Brue Valley is some six kilometres wide and is flanked on the north by the Wedmore Ridge, and on the south by the Polden Hills (Pl. XXIII). In the centre of the valley, surrounded by the peat, is a group of islands of higher ground, Meare, Westhay, and Burtle. These islands, which would always have provided relatively dry ground in the Levels, are linked together by Neolithic trackways of the third millennium B.C. Several of these trackways formed the basis of a paper in these Proceedings in 1968 (Coles and Hibbert, 1968), which continued the work of Godwin and others (Godwin, 1960; Dewar and Godwin, 1963).

scholarly journals Biotic and sedimentologic comparison of patch reefs on the north and south shelf of Belize, Central America

1992 ◽  
Vol 6 ◽  
pp. 45-45 ◽  
Author(s):  
C. D. Burke ◽  
S. J. Mazzullo
Keyword(s):  
Central America ◽  
Sea Level ◽  
Patch Reef ◽  
Acropora Palmata ◽  
The South ◽  
Northern Shelf ◽  
Patch Reefs ◽  
The North ◽  
Species Specific ◽  
Specific Growth Rates

Holocene patch-reefs occur throughout the shallow marine platform, to the lee of the barrier reef in northern and southern Belize, Central America. Patch reefs on the northern shelf that occur within an areally extensive patch reef complex (Mexico Rocks) indicate that differences exist between reefs here and well-studied patch reefs on the southern shelf that have been used by workers as a general model for patch reef development throughout Belize. This model proposes that patch reefs on the Belizean shelf are dominated by typical Atlantic-Caribbean, biotically-zoned coral assemblages of Acropora palmata and A. cervicornis that kept up or caught up with Holocene sea level rise during the last 8000 years to form large “keep up” or in some instances “catch up” reefs.In contrast to those in the south, the northern patch reefs are not biotically zoned, are dominated by Montastrea annularis rather than Acropora spp., and are much younger (400 years old) than those in the south. In addition, northern shelf patch reefs developed predominantly by lateral growth in a milieu of static sea level and are herein called “accretion” type reefs. These differences in biotic and sedimentologic parameters between reefs on the northern and southern shelves imply fundamentally different ecologic and sea level history controls on patch reef formation from north to south. A leading contributor to the variation among the reefs along the Belizean shelf may be species-specific growth rates of the coral species that initiate each patch reef, and response to sea level fluctuation versus stasis through time.

Woodeaton

1917 ◽  
Vol 7 ◽  
pp. 98-119 ◽  
Author(s):  
M. V. Taylor
Keyword(s):  
Sea Level ◽  
The South ◽  
North East ◽  
The North ◽  
Dry Seasons ◽  
The Village

Woodeaton is a small Oxfordshire parish, four miles north-east of the centre of Oxford city and a little west of the wide marshy level of the ‘Plain of Otmoor.’ It stands on a low, detached and rounded hill, 315 feet above sea level, and 120 feet above Otmoor. In old days it must have been difficult of access, for Otmoor spreads away to the east of it; low pastures along the river Cherwell close it in on the north and west, while south-westwards, too, the land is low-lying and marshy. Even to the south-east a marshy hollow separates it from the wooded slopes of Beckley and Elsfield, once part of Shotover Forest. However, the well-known Roman road which connects Dorchester (Oxon.) with Alchester, and which passes along the foot of Shotover, and traverses the village of Beckley and the plain of Otmoor, runs within two miles of Woodeaton; in dry seasons it may have helped those who wished to get to the spot.

HELMINTS OF DOMESTIC RUMINANTS AND SPECIAL FEA TERES OF THEIR DISTRIBUTION IN THE SOUTH-EAST REGION OF THE NORTH CAUCASUS

2018 ◽  
Vol 2 ◽  
pp. 126-132
Author(s):  
M.M. ZUBAIROVA ◽  
◽  
A. M. ATAEV ◽  
N.T. KARSAKOV ◽  
Z.M. DGAMBULATOV ◽  
...  
Keyword(s):  
North Caucasus ◽  
The South ◽  
The North ◽  
East Region ◽  
Domestic Ruminants

Laconia

1950 ◽  
Vol 45 ◽  
pp. 261-298 ◽  
Author(s):  
J. M. Cook ◽  
R. V. Nicholls
Keyword(s):  
Sea Level ◽  
The Other ◽  
The South ◽  
The West ◽  
Urban Settlement ◽  
West Side ◽  
The North ◽  
The Village

The village of Kalývia Sokhás lies against the base of one of the massive foothills in which Taygetus falls to the plain three or four miles to the south of Sparta (Plate 26, 1). It is bounded by two rivers which flow down in deep clefts from the mountain shelf. The hillside above rises steeply to a summit which is girt with cliffs on all but the west side and cannot be much less than four thousand feet above sea level; this von Prott believed to be the peak of Taleton. Its summit is crowned by the ruins of a mediaeval castle which was undoubtedly built as a stronghold to overlook the Spartan plain; the only dateable object found there, a sherd of elaborate incised ware, indicates occupation at the time when the Byzantines were in possession of Mystra. The location of the other sites mentioned by Pausanias in this region remains obscure, but fortunately that of the Spartan Eleusinion has not been in doubt since von Prott discovered a cache of inscriptions at the ruined church of H. Sophia in the village of Kalývia Sokhás. In 1910 Dawkins dug trenches at the foot of the slope immediately above the village and recovered a fragment of a stele relating to the cult of the goddesses and pieces of inscribed tiles from the sanctuary. The abundance of water in the southern ravine led von Prott to conclude that the old town of Bryseai with its cult of Dionysus also lay at Kalývia Sokhás; but no traces of urban settlement have come to light at the village, and the name rather suggests copious springs such as issue from the mountain foot at Kefalári a mile to the north where ancient blocks are to be seen in the fields.

Sign in / Sign up

Export Citation Format

Share Document