#: locale=en ## Action ### URL PopupWebFrameBehaviour_78E22E88_6048_44B9_41C2_0A0D105819A5.url = https://en.wikipedia.org/wiki/Sondrestrom_Upper_Atmospheric_Research_Facility PopupWebFrameBehaviour_11979D0B_3A34_4AC4_4187_8917B2F06AE2.url = //www.youtube.com/embed/Acg2g7Oq9WY PopupWebFrameBehaviour_B260E823_9CB3_F631_41D8_D9E654307650.url = //www.youtube.com/embed/TqqCPQpWgAE PopupWebFrameBehaviour_B2A4A95D_9CB2_B611_41D8_40C874A8398D.url = //www.youtube.com/embed/attUNSESGbQ WebFrame_6990A1C4_7622_CE68_41C7_18300617D417.url = //www.youtube.com/embed/tqfLDN_2BHg PopupWebFrameBehaviour_B130190C_9CAE_77F7_41B4_82A87467775F.url = //www.youtube.com/embed/zDPb58ZAbMw ## Hotspot ### Text HotspotPanoramaOverlayTextImage_F5BEDE28_FD6F_BC53_41BE_2F3E91C4BE24.text = The Watson River carves a channel that meanders through the landscape. HotspotPanoramaOverlayTextImage_F5BFFE25_FD6F_BC5D_41DD_73A03A4DE340.text = A communications building that stores data loggers, receivers and instrumentation used to monitor the rapidly changing weather. It is managed by Metar (the local airport). \ HotspotPanoramaOverlayTextImage_F5BE7E2A_FD6F_BC57_41E4_D6CD48BC9C38.text = Arctic Foxes can also be found in the Watson River watershed. HotspotPanoramaOverlayTextImage_F5BE4E2B_FD6F_BC55_41B5_300FB0025652.text = As we approach the terminus of the glacier, the river bed is steeper, creating cascades in the channel as the water descends. HotspotPanoramaOverlayTextImage_F5BDEE2C_FD6F_BC53_41E0_9C3A13F106BC.text = Can you identify the terminal moraines in this image? Moraines are composed of poorly sorted material including silt, sand, pebbles, cobbles, and boulders, known as till. HotspotPanoramaOverlayTextImage_F5BD8E2C_FD6F_BC53_41E7_40F262735F84.text = Glacial erratic on bedrock: rounded boulders transported long distances by the glacier and then deposited when it melts. HotspotPanoramaOverlayTextImage_F5BE6E2A_FD6F_BC57_41EB_322427083C96.text = Musk oxes can be spotted along the Watson River watershed. HotspotPanoramaOverlayTextImage_F5BF5E27_FD6F_BC5D_41DB_FC176584FF8C.text = Note the striations on the rock are directed up/down valley and indicate the direction of ice flow when the ice sheet covered this area. \ \ HotspotPanoramaOverlayTextImage_CF4A9F18_D41F_6665_41AA_A361989E7799.text = Scene 1.1 HotspotPanoramaOverlayTextImage_C834B685_D41A_A66F_41E9_D9F039144ED9.text = Scene 1.1 HotspotPanoramaOverlayTextImage_CFBDB2AF_D41E_9FBB_41DA_E6537E51037E.text = Scene 1.2 HotspotPanoramaOverlayTextImage_C8670A8C_D40B_6E7D_41E2_A864BD98AD5D.text = Scene 10 HotspotPanoramaOverlayTextImage_CFE3FA98_D41E_EE65_41C4_1B163AB23F46.text = Scene 2 HotspotPanoramaOverlayTextImage_CF52196C_D40E_AABD_41E6_C1AB33CBC4B2.text = Scene 2 HotspotPanoramaOverlayTextImage_CF469B21_D41A_AEA7_41D1_ABB23F49E632.text = Scene 2 HotspotPanoramaOverlayTextImage_CF3DB737_D419_A6AB_41E5_F494D9466FC6.text = Scene 3 HotspotPanoramaOverlayTextImage_CEC6F935_D419_AAAF_41B6_228612700A82.text = Scene 3 HotspotPanoramaOverlayTextImage_C8A022F0_D409_BFA5_41E9_CBCA0ECAB9D0.text = Scene 4.1 HotspotPanoramaOverlayTextImage_C8A4DB70_D409_EEA5_41D7_4BE6CC4ED3AB.text = Scene 4.1 HotspotPanoramaOverlayTextImage_CEC4D1D5_D40A_BDEF_41C5_3E376D56C596.text = Scene 4.1 HotspotPanoramaOverlayTextImage_C8099907_D406_AA6B_41D1_5FFF111901B7.text = Scene 4.2 HotspotPanoramaOverlayTextImage_C87480F2_D479_FBA5_418F_0E218CB78251.text = Scene 5 HotspotPanoramaOverlayTextImage_CFB3F024_D479_9AAD_41BA_C1268E0CD7C1.text = Scene 5 HotspotPanoramaOverlayTextImage_CF3A1F6F_D47B_66BB_41E5_96540D711897.text = Scene 6 HotspotPanoramaOverlayTextImage_CF2A47C4_D40A_E5ED_41E4_0F6EE5B781AD.text = Scene 6 HotspotPanoramaOverlayTextImage_CECB9617_D406_E66B_41E8_FF3DD8E7D001.text = Scene 7.1 HotspotPanoramaOverlayTextImage_CF393A81_D47B_6E67_41E9_A88673DB1F78.text = Scene 7.1 HotspotPanoramaOverlayTextImage_CFF46A72_D406_EEA5_41D3_B5C235C666CB.text = Scene 7.2 HotspotPanoramaOverlayTextImage_C8574FAB_D479_65BB_41DC_6450870C7D8D.text = Scene 7.2 HotspotPanoramaOverlayTextImage_CF493F69_D40A_A6A7_41C9_47286DAC177B.text = Scene 8 HotspotPanoramaOverlayTextImage_C80C19FA_D47B_6DA5_41C2_724B1B18EB74.text = Scene 8 HotspotPanoramaOverlayTextImage_C82D19F7_D407_ADAB_41E8_810105DB5ECF.text = Scene 9 HotspotPanoramaOverlayTextImage_CF503F38_D409_A6A5_41DD_1D2F98A616CB.text = Scene 9 HotspotPanoramaOverlayTextImage_F5BE9E27_FD6F_BC5D_41EA_9C80A800FAE4.text = Sled dog kennels. Sled dogs are commonly used in the winter for transportation in the Arctic over snow and snow covered sea ice. \ \ HotspotPanoramaOverlayTextImage_F5BF6E26_FD6F_BC5F_41D0_38744FE3AD59.text = The Greenland Ice Sheet, the headwaters of the Watson River, can be seen in the distance. HotspotPanoramaOverlayTextImage_F5BE2E29_FD6F_BC55_419F_B4B42659041A.text = The Watson River flows past the town of Kangerlussuaq. HotspotPanoramaOverlayTextImage_F5BDCE2C_FD6F_BC53_41D9_90C1B70C4841.text = The fairly smooth surface on the bedrock beneath your feet was formed due to glacial abrasion and polish. The grooves in the gneiss shows the flow direction of the glacier, as the bed of the glacier ground over the top of it. HotspotPanoramaOverlayTextImage_F5BEFE28_FD6F_BC53_41E9_9D00E601DD66.text = The mouth of the Watson River can be seen in the distance. HotspotPanoramaOverlayTextImage_F5BF3E26_FD6F_BC5F_41D3_DC3A5A2B69B8.text = The site is being decommissioned. Mosquitos are a menace in the summer downstream of the ice sheet. HotspotPanoramaOverlayTextImage_F5BFCE25_FD6F_BC5D_41B0_D7A34EA23F5C.text = When PFS staff mentioned a study that showed that zebra stripes repelled mosquitos to a stateside PFS employee, they received zebra outfits in the mail soon after. They found the suits were effective at protecting their skin from the mosquitos! ### Tooltip HotspotPanoramaOverlayArea_8B7C0A68_C2DB_9D78_41E2_4EDE5F6F8506.toolTip = . 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media/popup_F0D40E55_E60C_E6ED_41E6_406380820B0D_en_0_2.jpeg imlevel_0983F7A4_0503_2FFF_4185_F0126F4DD380.url = media/popup_F0D40E55_E60C_E6ED_41E6_406380820B0D_en_0_3.jpeg imlevel_0983C7A4_0503_2FFF_4160_48FE4937DBA6.url = media/popup_F0D40E55_E60C_E6ED_41E6_406380820B0D_en_0_4.jpeg ### Popup Image ### Subtitle panorama_6D1E2025_79FA_6DB1_41DB_B873D0799133.subtitle = Additional perspective of meltwater flowing from the Greenland Ice Sheet as it forms the headwaters of the Watson River. \ \ panorama_5841BF09_560C_546C_41CB_9B57BB2E0055.subtitle = Continuing to travel along the road from the harbor to the town of Kangerlussuaq. \ \ panorama_4302C7E6_5591_EA0F_41BA_8D68F264B67A.subtitle = Traveling on the road from the harbor to the town of Kangerlussuaq. panorama_76A28E71_6048_446B_41C2_DF40119E340F.subtitle = Continuing to travel along the road from the harbor to the town of Kangerlussuaq. panorama_546CD5C4_5FC9_C4A9_41C1_0E8A785762C2.subtitle = Continuing to travel along the road from the harbor to the town of Kangerlussuaq. \ \ panorama_79281EA1_6078_44EB_41D3_A3CBAF6FB644.subtitle = Overview of the Watson River and the town of Kangerlussuaq. \ \ panorama_7CE04959_6048_CC5B_41CF_D3471FB6D598.subtitle = The Watson River seen from ‘Little Sugar Loaf’ hill panorama_6B0F7A60_79A6_9DAF_41DA_553FD6040517.subtitle = The terminus of the Greenland Ice Sheet. \ \ panorama_44F41CC2_5596_1E07_41D3_CDEB6597E7CD.subtitle = Traveling on the road from the harbor to the town of Kangerlussuaq. panorama_409F3DCB_5596_7E05_41D1_6B801952C2EF.subtitle = Traveling on the road from the harbor to the town of Kangerlussuaq. \ panorama_6BD52FC2_79BA_B2F0_41DD_13A7BE7FAE6A.subtitle = Watson River with the Russel Glacier in the background. panorama_7F53CEF4_60C8_4469_41D7_E89571C5E8B2.subtitle = Watson River with the Russel Glacier in the background. panorama_765D48D2_79A6_BE93_41DB_6228F9B07227.subtitle = Watson River with the Russel Glacier in the background. ### Title 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P1: Proglacial lakes often form at the terminus of the ice sheet. These lakes are dynamic and evolve over the melt season as well as year to year.






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Aerial view of supraglacial stream network in the ablation region of the Greenland Ice Sheet.
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Proglacial lakes often form at the terminus of the ice sheet. These lakes are dynamic and evolve over the melt season as well as year to year.




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P1: Supra-glacial melt carves channels in the top of the ice.


P2: Supra-glacial melt carves channels in the top of the ice.


P3: Aerial view of supraglacial stream network in the ablation region of the Greenland Ice Sheet.


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Supra-glacial melt leaves behind deep channels that can be walked in once the meltwater season has ended. One would want to avoid walking in these at the beginning of the melt season as the meltwater could return, or find a new path to flow.



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Looking upstream at the Watson River, just before it flows past the town of Kangerlussuaq.



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The Watson River creates braided channels as it meanders down the watershed.



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The headwaters of the Watson River are at the ice sheet terminus.





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Supra-glacial melt leaves behind deep channels that can be walked in once the meltwater season has ended. One would want to avoid walking in these at the beginning of the melt season as the meltwater could return, or find a new path to flow.



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P1: Cryoconite holes can also be formed due to localized melt when ‘cryoconite’ (a combination of dust, black carbon and biological material) aggregate.




P2: Ice algae growing on the ice sheet.


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P1: Researchers sometimes camp at the ice sheet terminus while conducting fieldwork.


P2: Terminal moraines are left behind as the glacier melts.
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Water can flow through englacial channels in the ice sheet to the glacier terminus.




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Aerial view of crevasses in the ablation region of the Greenland Ice Sheet.
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Supraglacial melt carves channels in the top of the ice.





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Terminal moraines are left behind as the glacier melts.



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## Tour ### Description ### Title tour.name = 1.1 – Traveling to the Glacier Terminus