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	Dronning Maud Land - Wikipedia, the free encyclopedia
		Dronning Maud Land (or Queen Maud Land) is the part of Antarctica lying between the terminus of Stancomb-Wills Glacier, at 20°W, and Shinnan Glacier, at 44° 38'E, with a land area of approximately 2,500,000 km², mostly covered by the Antarctic ice sheet.
		This territory was claimed by Norway on January 14, 1939, but this claim, like all others in the Antarctic, is not universally recognized and the area is subject to the terms of the Antarctic Treaty.
		Dronning Maud Land was named by Roald Amundsen in honour of Queen Maud of Norway.
	en.wikipedia.org /wiki/Dronning_Maud_Land (204 words)

	Encyclopedia: Dronning Maud Land (Site not responding. Last check: 2007-10-21)
		Queen Maud (nee HRH Princess Maud of Wales) (Maud Charlotte Mary Victoria) (26 November 1869-20 November 1938) was the Queen consort of King Haakon VII of Norway.
		Queen Sonja of Norway (nÃ©e Sonja Haraldsen, born July 4, 1937 in Oslo) is the queen consort of Norway, wife of King Harald V of Norway.
		Flag of the British Antarctic Territory The British Antarctic Territory is the British claim to land and islands in Antarctica, and is the oldest territorial claim on the continent.
	www.nationmaster.com /encyclopedia/Dronning-Maud-Land (824 words)

	DRONNING MAUD LAND
		Dronning Maud Land (20°W - 45°E) whose name was given for Queen Maud of Norway when the Norwegian Captain Hjalmar Riiser-Larsen discovered it in 1930, is without doubt one of the Jewels in the Crown of the Antarctic "Far Side".
		No less awe-inspiring is Dronning Maud Land's more than 3000 km -long coastline, where the striking unbroken white wall of the "barrier" presented by the seaward edge of immensely-thick, floating ice-shelves, mark the birthplace of enormous tabular icebergs.
		The Schirmacher Oasis (70°46'S; 011°50'E) of central Dronning Maud Land is an Antarctic desert oasis comprising a low lying ~ 50 km² area of undulating ice-free hills interspersed with a number of glacial lakes.
	www.astronomicaltours.net /Antarctica2/AddONs/MountainCamp.htm (2133 words)

	Jacobs & Thomas, 1996
		The continental crust of western Dronning Maud Land was thermally rejuvenated by thermal blanketing of Jurassic basalts at ~180, Ma until the Lower Cretaceous (~140 Ma) before the lava pile was eroded again.
		The sedimentation on the marine plateau of western Dronning Maud Land is charaterized by 2000 m of sediments deposited at rates of >60 m/Ma during the Upper Jurassic.
		The fact that Proterozoic basement at Heimefrontfjella, western Dronning Maud Land, is unconformably overlain by a maximum thickness of 160 m of Beacon supergroup sedimentary rocks and Jurassic lava flows indicates that the basement cooled to surface temperatures during the Palaeozoic.
	www.joachimjacobs.de /Abstracts_neu.html (6590 words)

	Stockholm Glaciology - Jens-Ove Näslund
		I have focused mainly on glacial geology, and the impact that glaciers and ice sheets have on the landscape.
		In Dronning Maud Land I have also worked on mass balance by radar and differential GPS measurements.
		I am also running a project were we are quantifying the ice flux across a 500 km portion of the grounding-line in Dronning Maud Land, Antarctica, using satellite remote sensing data and field-information on ice depth and ice velocity.
	www.glaciology.su.se /people/JO/JO.html (383 words)

	Dronning Maud Land Biography
		Also Dronning Maud Land rise from a phase of abstinence lasting five years.
		With their new material Dronning Maud Land consequently continue their doing after their apparently definite split in 1996: emotions shake hands with hypnotic, progressive, almost conjuring rock-songs without drifting into derisority caused by brutality or pathos being out of place.
		Without calculation or virtuosity Dronning Maud Land come from the heart and hit the pit of your stomach.
	www.dronning-maud-land.de /biographie-e.htm (203 words)

	AWI: Glaciology
		The EPICA campaign in Dronning Maud Land1999/2000 was the 5th and probably final part of the pre-site survey for the planned EPICA deep ice core drilling in Dronning Maud Land (Fig.
		The aim of the pre-site survey was to investigate all the parameters needed for a physical description of the firn and ice body in Dronning Maud Land.
		1: Timetable of the 1999/2000 Dronning Maud Land traverse.
	www.awi-bremerhaven.de /GPH/www_gla2_EPICA-Vpresite.html (1629 words)

	PERMAFRO.HTM (Site not responding. Last check: 2007-10-21)
		The area studied belongs to the Vestfjella mountains in Dronning Maud Land, near the Finnish base station Aboa (73º03'S, 13º25'W; fl rectangle in Fig 2a).
		The main aim of the geophysical measurements was to study the bedrock geology between the nunataks.
		Grind, H., Siivola, J. and Luttinen, A. A geological overview of the Vestfjella Mountains in Western Dronning Maud Land, Antarctica.
	www.gsf.fi /~truotois/public/permafro/permafro.htm (3862 words)

	Dronning Maud Land - rFind.net (Site not responding. Last check: 2007-10-21)
		Dronning Maud Land är en del av Antarktis mellan 20° v.l.
		Efter kontinent och land i bokstavsordning-1.1 Afrika-1.2 Antarktis-1.3 Asien-1.4 Europa-...
		Centerledaren Maud Olofsson valde på fredagskvällen att ta upp frågorna om internationellt samarbete och kamp mot fattigdom i det tal hon höll i Almedalen i Visby.
	www.rfind.net /info/Dronning_Maud_Land (289 words)

	Karsten Adriaan Kaspers: Chemical and physical analyses of firn and firn air : from Dronning Maud Land, Antarctica
		Chemical and physical analyses of firn and firn air : from Dronning Maud Land, Antarctica / Karsten Adriaan Kaspers - [S.l.] : [s.n.], 2004 - Tekst.
		Firn air is the air that is trapped in the porous medium of firn, which is typically the first one hundred meters of an ice core.
		In this thesis the firn air analyses of Site M in Dronning Maud Land, Antarctica (15°E, 75°S, 3453 m.a.s.l) are described.
	igitur-archive.library.uu.nl /dissertations/2004-1119-103649/index.htm (666 words)

	Stockholm Glaciology - Jens-Ove Näslund
		Glazovskiy, A., Näslund, J.-O. and Zale, R., 1992: Deglaciation and shoreline displacement on Alexandra Land, Franz Josef Land.
		Holmlund, P. and Näslund, J.-O., 1994: The glacially sculptured landscape in Dronning Maud Land, Antarctica, formed by wet-based mountain glaciation and not by the present ice sheet.
		Näslund, J.-O., 1997: Airborne radar soundings of ice depth, GPS measurements of ice velocity and studies of landform evolution in central Dronning Maud Land, East Antarctica.
	www.glaciology.su.se /people/JO/JO_refs.html (1437 words)

	BEDMAP ICE THICKNESS METADATA SUMMARY (Site not responding. Last check: 2007-10-21)
		JARE 26 oversnow traverse in East Queen Maud Land toward the inland plateaux and Sor Rondane Mountains, 1985-86.
		BAS geophysical expedition in Ellsworth Land and James Ross Island in the 1985/86 and 1986/87 seasons.
		Alfred Wegener Institute airborne RES surveys of Dronning Maud Land and Princess Martha Coast between the Greenwich meridian and 15 degrees E..
	www.antarctica.ac.uk /aedc/bedmap/database/metadata.html (2660 words)

	AMALGAMATION OF COATS LAND/WESTERN DRONNING MAUD LAND WITH THE EAST ANTARCTIC CRATON: EVIDENCE FROM HEIMEFRONTFJELLA, ... (Site not responding. Last check: 2007-10-21)
		Previous workers have suggested that Grenvillian rocks of Coats Land and parts of western Dronning Maud Land (DML) were not part of East Antarctic Craton (EAC) until the late Precambrian — Cambrian.
		We report new field, petrographic and U-Pb age data from a transect across the central Heimefrontfjella Range in western Dronning Maud Land that document widespread late Cambrian metamorphism and deformation that we also relate to amalgamation with EAC.
		The oldest rocks in the transect are pre-1.10 Ga granitic and supracrustal gneisses that underwent early Grenville deformation and migmatisation (D1/M1) prior to the intrusion of ca.
	gsa.confex.com /gsa/2002AM/finalprogram/abstract_46269.htm (469 words)

	Dronning Maud Land : Queen Maud Land (Site not responding. Last check: 2007-10-21)
		Dronning Maud Land (or Queen Maud Land) is the part of Antarctica lying between 20°W and 45°E. Dronning Maud Land (or Queen Maud Land) is the part of Antarctica lying between 20°W and 45°E. This territory was claimed by Norway on January 14, 1939, but this claim, like others in the Antarctic, isn't universally recognised.
		All is still licensed under the GNU FDL.
		Whereupon being not a little discomforted, we were eight persons in it; whereof one of them had in his hand a tipstaff of without any show of distrust at all.
	www.termsdefined.net /qu/queen-maud-land.html (127 words)

	International GeoMaud Expedition of the BGR to Central Dronning Maud Land in 1995/96 - Volume I: Geological Results. ...
		The crust of central Dronning Maud Land is composed of late Mesoproterozoic metavolcanic and metasedimentary rock sequences which experienced Grenville deformation and metamorphism.
		Additionally, during the Pan-African events (600-500 Ma) the metamorphic crust in central Dronning Maud Land was intruded by a huge amount of igneous rock as discordant plutons ranging in composition from anorthosite to granite/syenite, some of which may now be metaplutonic rocks.
		The mountains and nunataks of central Dronning Maud Land (cDML) were discovered by the air-borne German Schwabenland expedition in 1939.
	www.schweizerbart.de /pubs/books/bgr/geologisch-186029600-desc.html (542 words)

	Papers (Site not responding. Last check: 2007-10-21)
		A mass-balance programme was initiated on Jutulstraumen ice stream, western Dronning Maud Land, Antarctica, during the austral summer 1992-93.
		As a part of the mass-balance programme, accumulation rate was measured along the centre line of Jutulstraumen from the shelf edge up to the plateau at about 2500 m a.s.l.
		The large variation in accumulation is important when selecting new core sites and for interpretation of temporal and spatial variations in accumulation derived from firn cores.
	www.glaciology.gfy.ku.dk /papers/abstracts/52.htm (224 words)

	Weir High School's Cyber Atlas: Dronning Maud Land and Peter I Island (Site not responding. Last check: 2007-10-21)
		Norway has three dependencies in the Antarctic: Bouvetoya (Bouvet Island), which lies outside the area of application of the Antarctic Treaty, and Peter I Oy (Peter I Island), and Dronning Maud Land (Queen Maud Land), which lies within it.
		Norway's efforts were focused on studies in oceanography and marine geology in the far south of the Weddell Sea, marine biological studies off the coast of Queen Maud Land, and surveys and studies of glaciers and bird life on land.
		Means of transportation in Queen Maud Land were upgraded, and Hägglund snowmobiles are currently stationed at Troll and Tor.
	whs.hanc.k12.wv.us /cyberatlas/Antarctica/Norway/index.html (414 words)

	Pan-African extension and near-isothermal exhumation of a granulite facies terrain, Dronning Maud Land, Antarctica -- ...
		Pan-African extension and near-isothermal exhumation of a granulite facies terrain, Dronning Maud Land, Antarctica
		Maud Land, Antarctica, consist of series of granitoid igneous
		central Dronning Maud Land is characterized by a near-isothermal
	geolmag.geoscienceworld.org /cgi/content/abstract/141/6/649 (215 words)

	Theses from Uppsala University : 4219 - Force Budget Analysis of Glacier Flow
		This thesis contributes to the understanding of glacier response to climate change by ice dynamical studies on Storglaciären, Sweden, and Bonnevie-Svendsenbreen, Kibergbreen and Plogbreen in Dronning Maud Land, Antarctica.
		Ice surface velocities, ice geometry and temperature information is fed through a force budget model to calculate ice mass outflux of these glacial systems via three-dimensional stress distributions for a flux-gate.
		Force Budget Analysis of Glacier Flow: Ice Dynamical Studies on Storglaciären, Sweden, and Ice Flow Investigations of Outlet Glaciers in Dronning Maud Land, Antarctica [Kraftbudgetanalys av glacialt flöde: Isdynamiska studier på Storglaciären, Sverige, och isflödesundersökningar av utlöparglaciärer i Drottning Maud Land, Antarktis].
	publications.uu.se /theses/abstract.xsql?dbid=4219 (601 words)

	Alfred Wegener Institute (Aeromagnetic Investigations in Dronning Maud Land)
		In preparation for the EU-project EPICA (EUROPEAN PROJECT FOR ICE CORING IN ANTARCTICA) large scale reconnaissance surveys are flown in Dronning Maud Land, Antarctica, using the airborne EMR system.
		During the next season EPICA 95/96 was carried out from the russion base Novolazarevskaya and a field camp near the Kottas Mountains.
		The geomagnetic data set that is being obtained from these surveys, covers a large, partially unmapped region in between 30 W and 15 E of Dronning Maud Land.
	www.awi-bremerhaven.de /GPH/www_antmag.html (201 words)

	NOAA Paleoclimatology Program - Dronning Maud Land
		Click here to download Dronning Maud Land data
		Climate records from shallow firn cores,Dronning Maud Land, Antarctica.
		A century of accumulation and temperature changes in Dronning Maud Land, Antarctica.
	www.ncdc.noaa.gov /paleo/icecore/antarctica/maud/maud.html (240 words)

	Queen Maud Land - Encyclopedia, History, Geography and Biography (Site not responding. Last check: 2007-10-21)
		Queen Maud Land - Encyclopedia, History, Geography and Biography
		This page was last modified 15:51, 25 February 2002.
		This encyclopedia, history, geography and biography article about Queen Maud Land contains research on
	www.arikah.com /encyclopedia/Queen_Maud_Land (48 words)

	DRONNING MAUD LAND (Site not responding. Last check: 2007-10-21)
		DRONNING MAUD LAND, Essence of a Decade Part 1 (Best Of)
		Middle Pillar Review: Dronning Maud Land were the pioneers of the second generation German Dark Wave/Gothic Rock-scene of the 1990's.
		Since their recent reformation, demand has been high for their earlier out of print albums.
	www.middlepillar.com /catalog/browse.pl/artist/DRONNING_MAUD_LAND (66 words)

	Analysis of bedrock geology and thermal gradients using geophysical ground measurements on glaciated terrain in Queen ... (Site not responding. Last check: 2007-10-21)
		Analysis of Bedrock Geology and Thermal Gradients Using Geophysical Ground Measurements on Glaciated Terrain in Queen Maud Land, Antarctica.
		The area studied belongs to the Vestfjella mountains in Dronning Maud Land, near the Finnish base station Aboa (73º03'S, 13º25'W; fl rectangle in Fig 1a).
		A geological overview of the Vestfjella Mountains in Western Dronning Maud Land, Antarctica.
	www.gsf.fi /~truotois/public/antarctic-sienna/siennatx.htm (2062 words)

	Noone and Simmonds, Dronning Maud Land accumulation characteristics, 1999 (Site not responding. Last check: 2007-10-21)
		With the planned European Program for Ice Coring in Antarctica in Dronning Maud Land it is important to understand the processes leading to accumulation for successful interpretation of core data.
		Because it is impractical to obtain precipitation observations with a large spatial coverage and on a daily timescale in Antarctica, model-generated precipitation must be considered for a comprehensive study of the region.
		Citation: Noone, D., J. Turner, and R. Mulvaney, Atmospheric signals and characteristics of accumulation in Dronning Maud Land, Antarctica, J. Geophys.
	paos.colorado.edu /~dcn/reprints/NooneEtAl_DMLprec_JGR1999_ABSTRACT.html (324 words)

	Temporal and spatial variability of the surface energy balance in Dronning Maud Land, East Antarctica
		Temporal and spatial variability of the surface energy balance in Dronning Maud Land, East Antarctica
		We present data of nine Automatic Weather Stations (AWS), which are located in Dronning Maud Land (DML), East Antarctica, since the austral summer of 1997.
		Citation: Reijmer, C., and J. Oerlemans (2002), Temporal and spatial variability of the surface energy balance in Dronning Maud Land, East Antarctica, J.
	www.agu.org /pubs/crossref/2002/2000JD000110.shtml (298 words)

	Joachim Jacobs
		Structural evolution of the Proterozoic basement of central Dronning Maud Land.
		Tectono-thermal evolution of the continental margin of central Dronning Maud Land, East Antarctica: apatite fission-track thermochronology.
		Bauer, W., Thomas, R.J. and Jacobs, J. Proterozoic to Cambrian history of central to western Droning Maud Land, SE Africa and surrounding areas in the context of Gondwana assemble.
	www.joachimjacobs.de (1424 words)

	Seasonal cycles of nonmethane hydrocarbons and methyl chloride, as derived from firn air from Dronning Maud Land, ...
		This paper presents atmospheric concentrations of ethane, propane, acetylene, and methyl chloride, inferred from firn air by using a numerical one-dimensional firn diffusion model.
		The firn air was collected on the Antarctic plateau in Dronning Maud Land during the Norwegian Antarctic Research Expedition (NARE) 2000/2001.
		The influences of seasonal variations in temperature and pressure and the variation in accumulation rate were studied and are not negligible, but appear to cancel each other out if all variability is taken into account.
	www.agu.org /pubs/crossref/2004/2004JD004629.shtml (468 words)

	IngentaConnect Late Proterozoic to Early Palaeozoic tectonism in Dronning Maud L... (Site not responding. Last check: 2007-10-21)
		Late Proterozoic to Early Palaeozoic tectonism in Dronning Maud Land, Antarctica: supercontinental fragmentation and amalgamation
		The Mid-Proterozoic–Early Palaeozoic tectonic development of western Dronning Maud Land is examined in the light of recent proposals that suggest geological continuity between Laurentia and Gondwana during the Middle Proterozoic (the SWEAT hypothesis).
		The Mid-Proterozoic–Early Palaeozoic tectonic development of western Dronning Maud Land was significantly different to that observed in the Transantarctic Mountains, and the c.
	api.ingentaconnect.com /content/geol/jgs/1993/00000150/00000005/15050833 (299 words)

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