Pesquisando por: "Malaspina Glacier" - Fotoarena - Agência de fotojornalismo

2T5P1GK Alaska Ketchikan, Ward Cove harbour, MV Malaspina named after the Malaspina Glacier

2WM0YFB Color satellite image of Malaspina Glacier, Alaska in 1986 and 2022, showing how the glacier has been melting over the years.

2WM0YEJ Color satellite image of Malaspina Glacier, Alaska in 2022.

2S8GWTE Aerial View of Malaspina Glacier in Saint Elias National Park and Reserve, Wrangell, Alaska

2NP1FH6 Aerial View of Malaspina Glacier in Saint Elias National Park and Reserve, Wrangell, Alaska

2HK3FD4 USA, Alaska, Chugach Mountain Range. Aerial view of mountains and Malaspina Glacier.

2GJ1R1R USA, Alaska, Chugach Mountain Range. Aerial view of mountains and Malaspina Glacier.

P423PT Malaspina Glacier, Yakutat Bay, Alaska, USA, Sunday, May 20, 2018.

P423N7 Malaspina Glacier, Yakutat Bay, Alaska, USA, Sunday, May 20, 2018.

P423M7 Malaspina Glacier, Yakutat Bay, Alaska, USA, Sunday, May 20, 2018.

P423NG Malaspina Glacier, Yakutat Bay, Alaska, USA, Sunday, May 20, 2018.

P423MR Malaspina Glacier, Yakutat Bay, Alaska, USA, Sunday, May 20, 2018.

P423NF Malaspina Glacier, Yakutat Bay, Alaska, USA, Sunday, May 20, 2018.

MFCH2N Malaspina Glacier in Alaska seen from space - contains modified Copernicus Sentinel data from ESA

2R77YJ2 Aerial photos, aerial images of Alaska

3B2GRPJ April 30, 2015 - EARTH Greenland -- 24 Sep 2014 -- The ice of a piedmont glacier spills from a steep valley onto a relatively flat plain, where it spreads out unconstrained like pancake batter. Elephant Foot Glacier in northeastern Greenland is an excellent example; it is particularly noted for its symmetry. But the largest piedmont glacier in North America (and possibly the world) is Malaspina in southeastern Alaska. On September 24, 2014, the Operational Land Imager (OLI) on Landsat 8 acquired this image of Malaspina Glacier. The main source of ice comes from Seward Glacier, located at the t

WPBG57 Malaspina Glacier, a piedmont glacier, southeastern Alaska, September 24, 2014, by NASA/Jesse Allen/DPA

KRHDNK IDL TIFF file Malaspina Glacier, Alaska (22800052331)

FF077T Malaspina Glacier, Alaska

H3D602 Aerial view of the Malaspina Glacier in Alaska, the world's largest piedmont glacier spilling from the Saint Elias Mountains

FR9WTR Aerial view of the Malaspina Glacier in the Coastal Range, Southeast Alaska, USA, Summer

FG6N2X Aerial view of the Malaspina Lake and Glacier in the Coastal Range, Southeast Alaska, USA, Summer

FG6N2T Aerial view of snow covered mountains and the Malaspina glacier in the Coastal Range, Southeast Alaska, USA, Summer

FG6N2W Aerial view of snow covered mountains and the Malaspina glacier in the Coastal Range, Southeast Alaska, USA, Summer

KRB7N6 Malaspina Glacier in Southeastern Alaska

T806M9 Malaspina Glacier

2BDY0X5 Malaspina Glacier

EKWHPK View of the tidal plains near the Malaspina Glacier Southeast Alaska, Spring

AD3GYX Malaspina Glacier AERIAL Alaska Classic example of Piedmont Glacier

AD3H0P Malaspina Glacier AERIAL Alaska Classic example of Piedmont Glacier

B18K6J Aerial view of vast Malaspina glacier Alaska USA

B18K6D Aerial view of section of Malaspina glacier Alaska USA

A5BRE8 Malaspina glacier Alaska USA

A5BRDF Aerial view of section of Malaspina glacier Alaska USA

AMH19B Malaspina glacier detail aerial view Alaska

BCJKT1 Malaspina Glacier & Coast MTS / Southeast, Alaska/naerial

2WM0YF6 Color satellite image of Malaspina Glacier, Alaska in 1986.

2WE0EDB Alaska - Malaspina Glacier through Matanuska

2WE0ED1 Alaska - Malaspina Glacier through Matanuska

2WE0EBB Alaska - Malaspina Glacier through Matanuska

2WE0EBD Alaska - Malaspina Glacier through Matanuska

2WE0EAT Alaska - Malaspina Glacier through Matanuska

2WE0EAB Alaska - Malaspina Glacier through Matanuska

2WE0EA4 Alaska - Malaspina Glacier through Matanuska

2WE0E9X Alaska - Malaspina Glacier through Matanuska

2WE0E9N Alaska - Malaspina Glacier through Matanuska

2WE0E9K Alaska - Malaspina Glacier through Matanuska

2W70Y8R Willow trees on Yakutat Bay near the Malaspina Glacier, Alaska, June 1899 (HARRIMAN 55).

2P3H3P1 Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3H32C Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3H321 Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3H310 Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3H31D Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3FHM0 Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3FHKB Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3FHKT Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3FHKD Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2P3FHKE Alaska - Malaspina Glacier through Matanuska, Aerial Photograph.

2M0PWTT Malaspina Glacier. Alaska Task Force Photographs

2M0PW9T Malaspina Glacier. Alaska Task Force Photographs

2M0PT97 Malaspina Glacier. Alaska Task Force Photographs

2M0PNAT Malaspina Glacier. Alaska Task Force Photographs

2M0PMMH Mount Saint Elias above Malaspina Glacier. Alaska Task Force Photographs

2M0PJEJ Malaspina Glacier. Alaska Task Force Photographs

2M0PEP4 Malaspina Glacier. Alaska Task Force Photographs

2M0PDTX Tree cover near Malaspina Glacier. Alaska Task Force Photographs

2M0PDW6 Mount Saint Elias above Malaspina Glacier. Alaska Task Force Photographs

2M0PDR0 Malaspina Glacier. Alaska Task Force Photographs

2M0P86N Malaspina Glacier. Alaska Task Force Photographs

2M0P77H Malaspina Glacier. Alaska Task Force Photographs

2M0P4N2 Malaspina Glacier. Alaska Task Force Photographs

2M0P34F Malaspina Glacier. Alaska Task Force Photographs

2M0P2YY Malaspina Glacier. Alaska Task Force Photographs

2M0P24T Malaspina Glacier. Alaska Task Force Photographs

2M0P091 Malaspina Glacier. Alaska Task Force Photographs

2M0NY5F Malaspina Glacier. Alaska Task Force Photographs

2M0NXWD Malaspina Glacier. Alaska Task Force Photographs

2M0NTC0 Malaspina Glacier. Alaska Task Force Photographs

2M0NP01 Sea lions on rocks near Sitkagi Point along Malaspina Glacier. Alaska Task Force Photographs

2M0NKPF Sea lions on rocks near Sitkagi Point along Malaspina Glacier. Alaska Task Force Photographs

2M0NFK8 Malaspina Glacier. Alaska Task Force Photographs

2M0NBAK Malaspina Glacier. Alaska Task Force Photographs

2M0N8R4 Outwash plain, Malaspina Glacier. Alaska Task Force Photographs

2M0N60D Malaspina Glacier. Alaska Task Force Photographs

2M0MTNP Wright and crew along beach on Malaspina Glacier. Alaska Task Force Photographs

2M0MNNG Mount Saint Elias from Malaspina Glacier. Alaska Task Force Photographs

2M0MNB3 Wright & crew along beach on Malaspina Glacier. Alaska Task Force Photographs

2M0MM7N Beach along Malaspina Glacier. Alaska Task Force Photographs

2M0MDP2 Malaspina Glacier moraine, Mount Saint Elias in background. Alaska Task Force Photographs

2M0MDMB Malaspina Glacier moraine, Mount Saint Elias in background. Alaska Task Force Photographs

2M0M9FN Malaspina Glacier. Alaska Task Force Photographs

2M0M967 Malaspina Glacier. Alaska Task Force Photographs

2CEEPTN . Seal and salmon fisheries and general resources of Alaska. an undertaking of great dif-ficulty. The Yakutats are the northernmost branch of theThlinget race, whichinhabits southeast Alaska. Like the rest of the Thlingets, and also theAleuts, they are expert basket weavers; in some of the houses we sawmagnificent robes made of down from the breast of the eagle. During the afternoon the clouds lifted, revealing the St. Elias Alps,and during the remaining hours of daylight we skirted the 60-milefront of the Malaspina glacier, with the sea dashing against its icecliffs. The unbroken sweep of mou

2CE2REE . Elementary physical geography . Fig. 179.Ice cave at terminus of a glacier. GLACIERS. 313 level plain. The slope of the plain is so slight, and the supplyof ice so limited, that this part of the united glaciers is almoststagnant. There is hardly any perceptible movement; andnear the margin, morainal material accumulates on the surfaceof the ice in such quantities as to completely bury it, forminga soil on its surface, upon which vegetation grOws. We haveon this, the Malaspina glacier, an instance of a well-developedforest, almost as luxuriantas some of those found inthe temperate latitudes,b

2CE2RD0 . Elementary physical geography . glacier. A forest alsoextends up to the verybase of the glacier (Fig.180). This form of an , :s , ice sheet has been Called Forest at the margin of Malaspina glacier, a piedmont glacier, because Alaska. it is developed at the foot of mountains. Continental Glaciers.—In the arctic and antarctic zones,the long winter, and the coolness of the summer, conspireto bring about extensive accumulations of snow and ice.As a result of this, some of the lands in these cold regionsare covered with great sheets of ice; and these are generallyin movement, from the central po

2CDGXJH . Review of reviews and world's work . ngues of theAl[)s, like the Mer de Glace, Rhone, and Gor-ner Glaciers, are no wider than Central Park,which would occupy a very small portion ofthe width of Columbia Glacier. Yet this isnot one of the largest ice tongues in Alaska,which has a single glacier larger than RhodeIsland, Malaspina Glacier, fed by many tribu-taries of the magnitude of Columbia Glacier.Imagine yourself on Governors Island.The accompanying photograph of Columbia terminus. It is of interest to know what be-comes of the ice. The photograph on thefacing page is a more intimate view o

2AWG25W Guide books of excursions in Canada1-10 . 141 ice. Just west of the Hayden the great Marvine glacierdescends from the mountains and supplies the ice whichforms the eastermost of the four lobes of Malaspina glacier.The low ice cliff of this glacier lies just back of the westcoast of Yakutat bay, extending from near Point Manby tothe Kwik river, and being separated from the sea by afringe of alluvial fans across which flow many large, swift,glacial streams. The Marvine lobe of the Malaspinaglacier is of distinct present interest because of a change Excursion C 8.. Three of the largest ice tongue

2AWG20H Guide books of excursions in Canada1-10 . Three of the largest ice tongues of the Swiss Alps superposed on the same scaleover Hubbard glacier. from stagnation to activity between 1905 and 1906. Theother three lobes of Malaspina glacier, called Seward,Agassiz, and Guyot, are fed by valley glaciers of the samenames. East of the Malaspina glacier, and between it andYakutat bay, are three glaciers which extend beyond their. H3 mountain valleys and spread out in piedmont bulbs. Thelargest and westernmost of these, the Lucia, is now separ-ated from Malaspina glacier, of which it was undoubtedlya for

2AKN56R The ice age in North America and its bearing upon the antiquity of man5th edwith many new maps and illus., enland rewritten to incorporate the facts that bring it up to date, with chapters on Lake Agassiz and the Probable cause of glaciation . advance of glaciers inAlaska are deserving of the most careful consideration in ourinterpretation of the significance of the facts which are beinghere detailed. * N. H. Winchell in Geologj^ of Minnesota, vol. i of Final Re-port, p. 36.3, 606 THE ICE AGE IX NORril AMERICA. Along both the Atrevida ami the Malaspina glacier mar-gins, the glacier and glacial

2AFTM7J . America, picturesque and descriptive. ua^ Zlrail, masM. THE KLONDYKE AND CAPE NOME. 507 TIh Alaskan roast hry,nu tlic Muir (Jlac-icr isbdnlered l»v the }j:;nat St. Klias mountain ran<i( ri.s-ini^ in Mount Logan to nineteen tliousand iie liun-dreil and thirty-nine feet, the highest of tiie locd<ies,and in ]Iount St. Elias nearer the coast to eighteentliou.sand and twenty-four feet. From the broadflanks of St. Klias the vast ^Malaspina GLacier flowsdown to Icy JJay on the Pacific Ocean. There aremountains all altt»ut tiiis region, which the otlicialgcograpliers are naming after publ