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Journal articles on the topic 'Eskort'

Author: Grafiati

Published: 4 June 2021

Last updated: 13 February 2022

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1

Chen, Xi, Xavier Comas, Andrew Reeve, and Lee Slater. "Evidence for glacial geological controls on the hydrology of Maine (USA) peatlands." Geology 48, no. 8 (2020): 771–76. http://dx.doi.org/10.1130/g46844.1.

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Abstract Freshwater pools commonly form eccentric crescent patterns in peatlands, an important atmospheric methane (CH4) source, and show an apparent spatial association with eskers in some deglaciated regions. However, the role of underlying permeable glacial deposits such as eskers in regulating hydrogeology, and perhaps even carbon cycling, in peatlands is rarely considered. In this study, ground-penetrating radar imaging and direct coring confirmed that clustered pools coincide with buried esker crests in contact with peat soil in Caribou Bog and Kanokolus Bog in Maine (USA). Hydraulic hea

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2

Allard, Michel. "Géomorphologie des eskers abitibiens." Cahiers de géographie du Québec 18, no. 44 (2005): 271–96. http://dx.doi.org/10.7202/021195ar.

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La région étudiée se situe dans le Nord-Ouest québécois entre les latitudes 48° et 49° 30' N. et les longitudes 77° 15' et 79° W. Les eskers dans cette région atteignent des dimensions de l'ordre de 100 km de longueur et de 50 m de hauteur. Entre les eskers s'étend une plaine argileuse formée par sédimentation au fond du lac glaciaire Barlow-Ojibway. Certains éléments de structure du socle précambrien ont influencé la mise en place des eskers de deux façons : parfois en leur faisant barrière, parfois en les canalisant le long de lignes de failles. Les modifications morphologiques des eskers pa

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3

Livingstone, Stephen J., Emma L. M. Lewington, Chris D. Clark, et al. "A quasi-annual record of time-transgressive esker formation: implications for ice-sheet reconstruction and subglacial hydrology." Cryosphere 14, no. 6 (2020): 1989–2004. http://dx.doi.org/10.5194/tc-14-1989-2020.

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Abstract. We identify and map chains of esker beads (series of aligned mounds) up to 15 m high and on average ∼ 65 m wide in central Nunavut, Canada, from the high-resolution (2 m) ArcticDEM. Based on the close 1 : 1 association with regularly spaced, sharp-crested ridges interpreted as De Geer moraines, we interpret the esker beads to be quasi-annual ice-marginal deposits formed time-transgressively at the mouth of subglacial conduits during deglaciation. Esker beads therefore preserve a high-resolution record of ice-margin retreat and subglacial hydrology. The well-organised beaded esker net

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4

Hooke, Roger LeB, and James Fastook. "Thermal conditions at the bed of the Laurentide ice sheet in Maine during deglaciation: implications for esker formation." Journal of Glaciology 53, no. 183 (2007): 646–58. http://dx.doi.org/10.3189/002214307784409243.

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The University of Maine Ice Sheet Model was used to study basal conditions during retreat of the Laurentide ice sheet in Maine. Within 150 km of the margin, basal melt rates average ∼5 mm a−1 during retreat. They decline over the next 100 km, so areas of frozen bed develop in northern Maine during retreat. By integrating the melt rate over the drainage area typically subtended by an esker, we obtained a discharge at the margin of ~1.2 m3 s-1. While such a discharge could have moved the material in the Katahdin esker, it was likely too low to build the esker in the time available. Additional wa

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Sharpe, David R., Susan E. Pullan, and Timothy A. Warman. "A Basin Analysis of the Wabigoon Area of Lake Agassiz, a Quaternary Clay Basin in Northwerstern Ontario." Géographie physique et Quaternaire 46, no. 3 (2007): 295–309. http://dx.doi.org/10.7202/032916ar.

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ABSTRACT Information from a wide range of sources is integrated in a basin analysis of the Wabigoon Basin, a Quaternary clay basin located on the Canadian Shield in northwestern Ontario. The basin sediments were deposited between 10.9 ka and 9.5 ka, along the margin of the Rainy Lobe of the Laurentide Ice Sheet, which formed the northern boundary of proglacial Lake Agassiz. The basin architecture is dominated by four major elements: end moraines, eskers, kames and a clay plain, all of which overlie irregular bedrock topography. End moraines, eskers and kames are composed mainly of a fining upw

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6

Punkari, Mikko, and Lars Forsström. "Organic Remains in Finnish Subglacial Sediments." Quaternary Research 43, no. 3 (1995): 414–25. http://dx.doi.org/10.1006/qres.1995.1047.

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AbstractMany sites in Fennoscandia contain pre-Late Weichselian beds of organic matter, located mostly in the flanks of eskers. It is a matter of debate whether these fragmentary beds were deposited in situ, or whether they were deposited elsewhere and then picked up and moved by glacial ice. The till-mantled esker of Harrinkangas includes a shallow depression filled with sand and silt containing, for example, several tightly packed laminar sheets of brown moss (Bryales) remains. It is argued that these thin peat sheets were transported at the base of the ice sheet, or englacially, and were de

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Lewington, Emma L. M., Stephen J. Livingstone, Chris D. Clark, Andrew J. Sole, and Robert D. Storrar. "A model for interaction between conduits and surrounding hydraulically connected distributed drainage based on geomorphological evidence from Keewatin, Canada." Cryosphere 14, no. 9 (2020): 2949–76. http://dx.doi.org/10.5194/tc-14-2949-2020.

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Abstract. We identify and map visible traces of subglacial meltwater drainage around the former Keewatin Ice Divide, Canada, from high-resolution Arctic Digital Elevation Model (ArcticDEM) data. We find similarities in the characteristics and spatial locations of landforms traditionally treated separately (i.e. meltwater channels, meltwater tracks and eskers) and propose that creating an integrated map of meltwater routes captures a more holistic picture of the large-scale drainage in this area. We propose the grouping of meltwater channels and meltwater tracks under the term meltwater corrido

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8

Brennand, T. A., and D. R. Sharpe. "Ice-sheet dynamics and subglacial meltwater regime inferred from form and sedimentology of glaciofluvial systems: Victoria Island, District of Franklin, Northwest Territories." Canadian Journal of Earth Sciences 30, no. 5 (1993): 928–44. http://dx.doi.org/10.1139/e93-078.

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On Victoria Island, tunnel channels, eskers, and associated fans and extended deposits together constitute channelized glaciofluvial systems. Flutes and drumlinoid ridges, interpreted as residuals left by erosive, catastrophic, subglacial meltwater sheet flows, lie adjacent to these systems. One tunnel channel is described in detail. It exhibits deep scours, a discontinuous thalweg, sculpted margins, and flutes on the downflow side of one wall, features indicative of complex flow and possibly several flow events. The tunnel channel is interpreted as the product of erosion by catastrophic, subg

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9

Bergvall, M., H. Grip, J. Sjöström, and H. Laudon. "Modeling subsurface transport in extensive glaciofluvial and littoral sediments to remediate a municipal drinking water aquifer." Hydrology and Earth System Sciences 15, no. 7 (2011): 2229–44. http://dx.doi.org/10.5194/hess-15-2229-2011.

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Abstract. Few studies have been carried out that cover the entire transport process of pesticides, from application at the soil surface, through subsurface transport, to contamination of drinking water in esker aquifers. In formerly glaciated regions, such as Scandinavia, many of the most important groundwater resources are situated in glaciofluvial eskers. The purpose of the present study was to model and identify significant processes that govern subsurface transport of pesticides in extensive glaciofluvial and littoral sediments. To simulate the transport processes, we coupled a vadose zone

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10

Bergvall, M., H. Grip, J. Sjöström, and H. Laudon. "Modeling subsurface transport in extensive glaciofluvial and littoral sediments to remediate a municipal drinking water aquifer." Hydrology and Earth System Sciences Discussions 8, no. 1 (2011): 1729–64. http://dx.doi.org/10.5194/hessd-8-1729-2011.

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Abstract. Few studies have been carried out that cover the entire transport process of pesticides, from application at the soil surface, through subsurface transport, to contamination of drinking water in esker aquifers. In formerly glaciated areas, such as Scandinavia, many of the most important groundwater resources are situated in glaciofluvial eskers. The purpose of the present study was to model and identify significant processes that govern subsurface transport of pesticides in extensive glaciofluvial and littoral sediments. To simulate the transport processes, we coupled a vadose zone m

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11

Basasoro Ciganda, Maitane, Iñaki Karrera Juarros, and Andoni Arguiñano Madrazo. "Antzuola Herri Eskola. Eskola ongizatearen eraikuntzan kontzeptua mugatuz eta zabalduz." Tantak 30, no. 1 (2018): 135–51. http://dx.doi.org/10.1387/tantak.19559.

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Hezkuntzako erronka nagusienetako bat egungo aniztasunari modu positiboan aurre egin eta inklusiora bidea irekitzea da. Bide honetan, hezkuntzako marko legalak dio gizabanakoen ongizatea bermatu behar duela eskola inklusiboak. Horretarako, eskola ongizatearen garrantzia azpimarratzen da lan honetan, zehazki eskola ongizatea komunitateko kide ororentzako espazio aproposago bat bilatzeko bidean martxan jartzen diren ezaugarri multzo gisa ulertuz. Lan honetan, ongizatea helburu nagusitzat duen eskola bat aztertu ondoren, eskola ongizateak besteak beste biltzen dituen ezaugarri multzo bat osatu na

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12

Shvarev, S. V. "Postglacial seismogenic deformations of an esker in the Northern Karelian Isthmus (south-east Fennoscandia)." Geomorphology RAS, no. 3 (September 11, 2019): 19–35. http://dx.doi.org/10.31857/s0435-42812019319-35.

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The research area is located in the Northern part of the Karelian Isthmus between Lake Ladoga and the Gulf of Finland of the Baltic Sea. The terrain features are closely related to the tectonic structure of the crystalline basement, partially covered with thin deposition layer of the Last Glaciation and Holocene mostly. Accumulative forms are rarely but strongly correlated with the tectonic structure also. Most expressive features of accumulative topography are esker ridges that stretch for tens of kilometers. Analysis of eskers spatial distribution shows their close connection with the struct

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13

Grube, Alf. "Zur Struktur von Eskern in Schleswig-Holstein, unter besonderer Berücksichtigung des „Esker-Kames-Systems Forst Steinburg“ in morphologischer Hochlage." E&G Quaternary Science Journal 60, no. 4 (2011): 425–33. http://dx.doi.org/10.3285/eg.60.4.03.

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Abstract. Die unterschiedlichen Esker-Formen Schleswig-Holsteins wurden für das Geotop-Kataster des Landes mittels Literatur- und Feldarbeiten neu bearbeitet: Esker i.e.S., Aufpressungs-Esker mit Kern aus Geschiebemergel oder Beckensedimenten, Perlenschnur-Esker, Till-bedeckte Esker, sich kreuzend überlagernde Esker, verwachsen- und getrennt-parallele Esker-Rücken sowie Esker mit und ohne begleitende Rinnenbildungen. Esker sind häufig räumlich vergesellschaftet bzw. genetisch verflochten mit Drumlins oder drumlinoiden Formen, angrenzenden Aufpressungsstrukturen aus Till, Eisrandlagen, Kames-Bi

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14

Niemi, R. M., A. Kytövaara, J. Pääkkönen, and K. Lahti. "Removal of F-specific RNA bacteriophages in artificial recharge of groundwater - a field study." Water Science and Technology 50, no. 1 (2004): 155–58. http://dx.doi.org/10.2166/wst.2004.0046.

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Artificial recharge of groundwater offers a semi-natural means to produce raw water for drinking-water plants. Surface water works are increasingly being replaced by artificial groundwater works in Finland. Two municipalities, one serving 30,000 and the other 170,000 inhabitants, have considered filtering river water through eskers for the production of potable water. In this study the removal of bacteriophages during infiltration of river water was estimated, for the evaluation of treatment adequacy in a field study. A 5-m-deep column of sand was constructed and used to mimic the percolating

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15

Brennand, Tracy A. "Macroforms, large bedforms and rhythmic sedimentary sequences in subglacial eskers, south-central Ontario: implications for esker genesis and meltwater regime." Sedimentary Geology 91, no. 1-4 (1994): 9–55. http://dx.doi.org/10.1016/0037-0738(94)90122-8.

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16

Aranburu, Ane, Alaitz Tresserras, Rakel Gamito, and Ainhoa Gomez. "Bestelako eskola eredu bat posible da: Bizilore, eskola komunitate berri baten lehen urratsak." Tantak 30, no. 1 (2018): 9–36. http://dx.doi.org/10.1387/tantak.18122.

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Gaur egunean, gero eta gehiago, bestelako eskola eredu baten aldeko aldarriak eta esperientziak loratzen ari dira batean eta bestean. Besteak beste, eta mantso bada ere, ikasleak ez du irakasleak erakusten diona bakarrik ikasten; edota ikasle talde bateko partaideek mugarri berbera lortu beharra ere, indarra galtzen ari da. Gradu Amaierako Lan honek, Azkoitiko Bizilore eskola aktiboan bizi duten esperientziaren ikerketa kualitatiboaren bitartez, bestelako eskola eredu baten inguruan hausnarketa egitera eramaten gaitu. Ikerketa, eskolako eguneroko bizitzaren behaketa parte-hartzailean, irakasle

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17

Rodriguez-Miñambres, Paloma. "Idazlan klasikoak eta eskola." Tantak 31, no. 1 (2019): 9–25. http://dx.doi.org/10.1387/tantak.20115.

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Artikulu honetan, haur eta gazte literaturako lan klasiko eta tradizionalei buruz haus- nartzen da, haien definizioaz eta osagai bereizgarriez, bai eta haien jatorriari buruz ere, dela unibertsal- tzat hartzen diren lanen kasuan, dela euskal literatur tradiziokoak ere. Orobat, lan klasiko horien molda- keten eta berridazketen auzia aztertzen da, batez ere moldaketa horietako batzuek, zenbaitetan helburu didaktikoz eginak, berekin dakartzaten galeren eta irabazien ildotik. Lan klasiko eta tradizional horiek egungo eskola-testuinguruan irakasten jarraitzearen beharra eta onurak azpimarratzen dit

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18

Fitzsimons, Sean J. "Supraglacial eskers in Antarctica." Geomorphology 4, no. 3-4 (1991): 293–99. http://dx.doi.org/10.1016/0169-555x(91)90011-x.

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19

Haila, Yrjö. "Antti Eskola (1934-2018)." Tiede & edistys, no. 3 (March 1, 2018): 261–62. http://dx.doi.org/10.51809/te.105296.

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20

Levasseur, Denis. "Les eskers : essai de synthèse bibliographique." Géographie physique et Quaternaire 49, no. 3 (2007): 459–79. http://dx.doi.org/10.7202/033066ar.

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RÉSUMÉ L'essai propose une revue de la littérature sur les eskers. On y expose les informations de base (définition, terminologie, dimensions, distribution et caractères sédimentologiques généraux, incluant granulomere, fabriques, paléocourants, déformations et composition pétrographique) avant de présenter un historique des théories sur l'origine de ces constructions (hypothèses sous-glaciaire, supra- et intraglaciaire, de marge glaciaire et autres). De plus, on examine les différents modèles de sédimentation des eskers (chenal subaérien, canalisation forcée, deltaïque) et quelques généralité

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Lundqvist, Jan. "Periodical sedimentation in Scandinavian eskers." GFF 121, no. 3 (1999): 175–81. http://dx.doi.org/10.1080/11035899901213175.

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Garmendia Zaldua, Joana, Itxaso Marti Carrera, and Andone Sistiaga Berrondo. "Adin erlatiboaren efektua eskola-garaian." Uztaro. Giza eta gizarte-zientzien aldizkaria, no. 113 (April 29, 2020): 93–109. http://dx.doi.org/10.26876/uztaro.113.2020.5.

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Gordon, Jennifer L., Susan S. Girdler, Samantha E. Meltzer-Brody, et al. "Response to Eskola et al." American Journal of Psychiatry 172, no. 8 (2015): 797. http://dx.doi.org/10.1176/appi.ajp.2015.15030377r.

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24

Cummings, Don I., Bruce A. Kjarsgaard, Hazen A. J. Russell, and David R. Sharpe. "Eskers as mineral exploration tools." Earth-Science Reviews 109, no. 1-2 (2011): 32–43. http://dx.doi.org/10.1016/j.earscirev.2011.08.001.

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25

Sutanto, E. L. "Visitor from ESKOM." IEEE Power Engineering Review 13, no. 12 (1993): 31. http://dx.doi.org/10.1109/mper.1993.245829.

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26

Burke, Matthew J., John Woodward, Andrew J. Russell, and P. Jay Fleisher. "Structural controls on englacial esker sedimentation: Skeiðarárjökull, Iceland." Annals of Glaciology 50, no. 51 (2009): 85–92. http://dx.doi.org/10.3189/172756409789097568.

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AbstractWe have used ground-penetrating radar (GPR) to observe englacial structural control upon the development of an esker formed during a high-magnitude outburst flood (jökulhlaup). The surge-type Skeiðarárjökull, an outlet glacier of the Vatnajökull ice cap, Iceland, is a frequent source of jökulhlaups. The rising-stage waters of the November 1996 jökulhlaup travelled through a dense network of interconnected fractures that perforated the margin of the glacier. Subsequent discharge focused upon a small number of conduit outlets. Recent ice-marginal retreat has exposed a large englacial esk

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Christiansen, E. A. "Verendrye valley and the Glidden esker, Saskatchewan: subglacial and ice-walled features in southwestern Saskatchewan, Canada." Canadian Journal of Earth Sciences 24, no. 1 (1987): 170–76. http://dx.doi.org/10.1139/e87-014.

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Verendrye valley is more than 100 km long, about 1 km wide, and at least 225 m deep. Southward, the valley grades into the Glidden esker, the surface of which rises about 280 m above the lowest point in the valley. The sediments in the valley and esker are 205 and 75 m thick, respectively, and form a fining-upward sequence from sand and gravel at the base to silt with sand interbeds in the upper part of the sequence, which, in turn, is covered by a blanket of glacial lake clay.The concave-upward longitudinal profile of Verendrye valley, the genetic relationship between Verendrye valley and the

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Escalante Mateos, Naiara, Arantza Fernández-Zabala, Eider Goñi Palacios, and Iker Izar de la Fuente Diaz de Cerio. "Eskola giroa: definizioa, domeinuak, beste aldagaiekin harremana eta ebaluazioa." Tantak 32, no. 1 (2020): 117–36. http://dx.doi.org/10.1387/tantak.21268.

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Eskola giroa aztertzea interesgarria da ikasleen ebaluazioaren testuinguruaren ikuspegitik. Dena den, eskola giroa lantzeko eta ebaluatzeko zaila den konstruktua da, batez ere hainbat ikuspegitatik ikertu izan den dimentsio anitzeko egitura delako. Gaur egun, oraindik, terminologia nahasmen handia dago haren inguruan, eta haren barne egitura ez dago argi zehaztuta. Beraz, gai hori argitu ahal izateko asmoz, lan honen helburu nagusia da eskola giroa konstruktuaren berrikuspen teorikoa egitea, bai eta hura neurtzeko bideratutako tresnak aztertzea ere. Ondorioztatzen da herrialde anglosaxoietan a

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SHREVE, RONALD L. "Esker characteristics in terms of glacier physics, Katahdin esker system, Maine." Geological Society of America Bulletin 96, no. 5 (1985): 639. http://dx.doi.org/10.1130/0016-7606(1985)96<639:ecitog>2.0.co;2.

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Suoranta, Juha. "Jäähyväistarinoita." Aikuiskasvatus 18, no. 4 (1998): 326–27. http://dx.doi.org/10.33336/aik.92530.

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Sagardia, Irati, and Agurtzane Martinez. "Ikasleen ahotsak: guztiontzako eskola eraikitzeko gakoa." Tantak 31, no. 1 (2019): 121–47. http://dx.doi.org/10.1387/tantak.20479.

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Ikastetxe guztietan dagoen aniztasunaren aurrean, indarra hartu du kalitatezko eta ekitatezko hezkuntza inklusiboaren ikuspegiak. Artikulu honetan, ikerketa proiektu baten prozesu eta emaitzak aurkezten dira eta proiektu honetan orain arte sisteman isilduak izan diren protagonisten aho- tsak jaso dira. Proiektuan parte hartu dute Gipuzkoan kokatzen den eskola bateko Lehen Hezkuntzako ikasle guztiek eta helburua izan da ezagutzea ikasleek eskolan dituzten sentimendu eta bizipenak. Ho- rretarako, galdetegiak, ikasleen ahotsa azaleratzen laguntzen duten teknikak eta eztabaida-taldeak era- bili di

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Gartzia Santamaria, Mikel, and Jon Bustillo Bayón. "Eskola eta irratia: EHko 5 haur-irrati, Arabako 6 eskola-irrati eta Gasteizko Alai Bediren esperientzia." Tantak 28, no. 1 (2016): 49–64. http://dx.doi.org/10.1387/tantak.16338.

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En este artículo se ha analizado la utilidad de la radio como recurso didáctico y el uso que actualmente se le da en 6 centros educativos de Álava, tanto en Educación Infantil como, en mayor medida, en Primaria. También se describen en otros territorios de Euskal Herria 4 casos en los que radios profesionales ofrecen sus servicios a las escuelas. Por último, se explica cómo durante el curso académico 2014-2015 se creó un nuevo programa infantil en la radio Hala Bedi de Vitoria-Gasteiz que permitió experimentar las posibilidades educativas de este medio de comunicación.

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Suoranta, Juha. "Sosiologinen evankeliumi." Aikuiskasvatus 21, no. 1 (2001): 61–63. http://dx.doi.org/10.33336/aik.93340.

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Kemppainen, Heikki. "Vapaaehtoistyö oppimisen ja auttamisen areenana." Aikuiskasvatus 22, no. 2 (2002): 152–54. http://dx.doi.org/10.33336/aik.93415.

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Huotari, Vesa. "Sotaa ja sorron merkkejä!" Aikuiskasvatus 28, no. 1 (2008): 68–70. http://dx.doi.org/10.33336/aik.93804.

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SANZ, JOSU, Maialen Sistiaga, Pello Urkidi, Irati Andoño, and Kakun Orbegozo. "Baso-eskola proiektu pilotuko haurren ebaluazio hezigarria burutzeko adierazleen definizioa." Tantak 30, no. 2 (2019): 63–78. http://dx.doi.org/10.1387/tantak.19322.

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ABSTRACTThree early childhood schools (Langile Ikastola from Hernani, Amara Berri from Donostia and the school from Alkiza) will develop their 2017-2018 school year as a pilot project in basoeskola from Ekogunea (Fundación Kutxa). The main objective of this work is to present is to present the evaluation model developed for measuring the potential benefits of the participant children in their continous contact with nature. Among the developed or adapted indicators, it can be mentioned the measurement of the cognitive and affective development of the participant children, the suitability of the

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LASUT, LIANA, YURI M. MARUSIK, and HOLGER FRICK. "First description of the female of the spider Savignia zero Eskov, 1988 (Araneae: Linyphiidae)." Zootaxa 2267, no. 1 (2009): 65–68. http://dx.doi.org/10.11646/zootaxa.2267.1.5.

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Savignia is a relatively large and well defined Holarctic spider genus (see Eskov 1988). It includes 23 species, of which seven are known by males only (Platnick 2009). Thirteen species, including many endemics, have been recorded from the Far East Palaearctic (Eskov 1991).

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Marttila, H., M. Aurela, L. Büngener, et al. "Quantifying groundwater fluxes from an aapa mire to a riverside esker formation." Hydrology Research 52, no. 2 (2021): 585–96. http://dx.doi.org/10.2166/nh.2021.064.

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Abstract Water flows in peatland margins is an under-researched topic. This study examines recharge from a peatland to an esker aquifer in an aapa mire complex of northern Finland. Our objective was to study how the aapa mire margin is hydrogeologically connected to the riverside aquifer and spatial and temporal variations in the recharge of peatland water to groundwater (GW). Following geophysical studies and monitoring of the saturated zone, a GW model (MODFLOW) was used in combination with stable isotopes to quantify GW flow volumes and directions. Peatland water recharge to the sandy aquif

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Auton, Clive A. "Scottish landform examples — 6: The Flemington eskers." Scottish Geographical Magazine 108, no. 3 (1992): 190–96. http://dx.doi.org/10.1080/00369229218736865.

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Storrar, Robert D., Marek Ewertowski, Aleksandra M. Tomczyk, et al. "Equifinality and preservation potential of complex eskers." Boreas 49, no. 1 (2019): 211–31. http://dx.doi.org/10.1111/bor.12414.

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Hewitt, Ian J., and Timothy T. Creyts. "A Model for the Formation of Eskers." Geophysical Research Letters 46, no. 12 (2019): 6673–80. http://dx.doi.org/10.1029/2019gl082304.

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Butcher, Frances E. G., Susan J. Conway, and Neil S. Arnold. "Are the Dorsa Argentea on Mars eskers?" Icarus 275 (September 2016): 65–84. http://dx.doi.org/10.1016/j.icarus.2016.03.028.

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Marusik, Yuri, and Seppo Koponen. "New biogeographical records of spiders and harvestmen (Arachnida: Araneae & Opiliones) from West Siberia, including an annotated list of species." Entomologica Fennica 26, no. 4 (2015): 165–70. http://dx.doi.org/10.33338/ef.53371.

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Fifty-three species of spiders and one species of harvestmen were found in the previously unstudied Gydansky Peninsula, northwestern Siberia. Distribution for each species is given. Records of certain species are of a special interest: Xysticus viduus (the northernmost locality in its range), Crosbylonia borealis (the westernmost), Oreoneta eskovi (the northernmost and the westernmost), Clubiona norvegica (the easternmost in Asia), Pachygnatha listeri , Helophora insignis and Mitopus morio (the northernmost in Asia) and Oreoneta leviceps (the southernmost in the Palaearctic). Three species, Or

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Setién Echenique, Oihane, and Carol Pascual Ortiz. "Urtarokobiltegiratze termikoko sistemen bideragarritasun tekno-ekonomikoaren azterketa." EKAIA Euskal Herriko Unibertsitateko Zientzi eta Teknologi Aldizkaria, no. 30 (October 27, 2016): 71–79. http://dx.doi.org/10.1387/ekaia.15854.

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Gaur egun, Europako energiaren kontsumo osoaren %40 eraikinek eragiten dute.Kontsumo horren barnean, eraikinetako berokuntza eta ur bero sanitarioaren (UBS) erabilera nabarmentzen da, batik bat. Espainiaren kasuan, berokuntza %50 da, eta UBSa, berriz, %27. Proiektu honen bitartez, Espainia mailan Urtarokobiltegiratze termikoko sistemen (STES)bideragarritasun ekonomiko zein energetikoa aztertu da. Espainiako hainbat hiritako eskari termikoak simulatu dira, eta STESaren bitartez berogailuko eta UBSko eskari osoaren %45-60 artean asetzeko saiakera egin da. Beraz, ikusita eraikinetan kontsumo ener

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Suyadi, Yanu Madawanto, and Salim. "Pengaruh Pelatihan Dan Disiplin Kerja Terhadap Kinerja Prajurit Satuan Kapal Eskorta Koarmada II." Coopetition : Jurnal Ilmiah Manajemen 12, no. 2 (2021): 279–88. http://dx.doi.org/10.32670/coopetition.v12i2.480.

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Escort ship is a warship designed for the duties of guarding and protecting a main body or not of high value when a formation is carrying out sea crossing tasks. The Escort ship is also the main element of the convoy's protection. The crew member factor is a determinant of the ability level of the Escort Ship Unit and the readiness of other equipment. As the main factor, human resource must have high quality, readiness and discipline. Each individual and group must be skilled and work, and have good discipline. The existence of discipline and individual performance of the Escort Ship Unit and

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46

Lindstrom, Erling. "Esker Enlargements in Northern Sweden." Geografiska Annaler. Series A, Physical Geography 75, no. 3 (1993): 95. http://dx.doi.org/10.2307/521028.

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Mills, Donald, Kenneth T. Chow, and Scott L. Marshall. "Design-Construction of Esker Overhead." PCI Journal 36, no. 6 (1991): 44–51. http://dx.doi.org/10.15554/pcij.09011991.44.51.

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Lindström, Erling. "Esker Enlargements in Northern Sweden." Geografiska Annaler: Series A, Physical Geography 75, no. 3 (1993): 95–110. http://dx.doi.org/10.1080/04353676.1993.11880388.

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Wirahayu, Arwinda Yuhan, and Prijono Satyabakti. "Prevention of HIV/AIDS in Indonesian Navy views of Knowledge, Attitude, and Practice." Jurnal Berkala Epidemiologi 2, no. 2 (2014): 161. http://dx.doi.org/10.20473/jbe.v2i2.2014.161-170.

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ABSTRACTHIV/AIDS is a disease that is spreading rapidly in many countries, including in Indonesia. HIV/AIDS can affect anyone regardless of social status, race, religion, gender and age groups, including in Indonesian Navy personnel and their families. This study to identify the prevention of HIV/AIDS views of knowledge, attitudes and practice. The methods used in this research was descriptive observasional with the entire population in Indonesian Navy (Study at Satuan Kapal Eskorta Komando Armada RI Kawasan Timur). Sample size was 87 respondents were selected by purposive sampling technique.

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Wirahayu, Arwinda Yuhan, and Prijono Satyabakti. "Prevention of HIV/AIDS in Indonesian Navy views of Knowledge, Attitude, and Practice." Jurnal Berkala Epidemiologi 2, no. 2 (2014): 161. http://dx.doi.org/10.20473/jbe.v2i22014.161-170.

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ABSTRACTHIV/AIDS is a disease that is spreading rapidly in many countries, including in Indonesia. HIV/AIDS can affect anyone regardless of social status, race, religion, gender and age groups, including in Indonesian Navy personnel and their families. This study to identify the prevention of HIV/AIDS views of knowledge, attitudes and practice. The methods used in this research was descriptive observasional with the entire population in Indonesian Navy (Study at Satuan Kapal Eskorta Komando Armada RI Kawasan Timur). Sample size was 87 respondents were selected by purposive sampling technique.

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