{"id":605454,"date":"2026-04-15T10:24:09","date_gmt":"2026-04-15T10:24:09","guid":{"rendered":"https:\/\/www.newsbeep.com\/ca\/605454\/"},"modified":"2026-04-15T10:24:09","modified_gmt":"2026-04-15T10:24:09","slug":"contours-of-the-james-bay-lowlands","status":"publish","type":"post","link":"https:\/\/www.newsbeep.com\/ca\/605454\/","title":{"rendered":"Contours of the James Bay Lowlands"},"content":{"rendered":"<p>Early spring around Hudson Bay in northern Canada is largely indistinguishable from winter. Sea ice still clings to land, and the boggy lowlands remain frozen. In the dulled tones of the boreal landscape, however, snow helps accentuate the area\u2019s subtle topography. In late March 2026, an astronaut aboard the International Space Station captured this photo of frozen channels feeding Hannah Bay\u2014a southern offshoot of James Bay, which is itself an extension of Hudson Bay.<\/p>\n<p>Some of the patterns visible in the photo relate to the region\u2019s ice age history. During the Pleistocene Epoch, the <a href=\"https:\/\/www.antarcticglaciers.org\/glacial-geology\/laurentide-ice-sheet\/laurentide-ice-sheet-at-the-last-glacial-maximum\/\" rel=\"nofollow noopener\" target=\"_blank\">Laurentide Ice Sheet<\/a> covered most of present-day Canada. It centered on <a href=\"https:\/\/www.ebsco.com\/research-starters\/earth-and-atmospheric-sciences\/hudson-bay#geology\" rel=\"nofollow noopener\" target=\"_blank\">Hudson Bay<\/a>, where its immense weight depressed the land. Since the Last Glacial Maximum about 20,000 years ago, the ice has retreated and the land has been bouncing back. Glacial isostatic adjustment,\u00a0or <a href=\"https:\/\/nsidc.org\/learn\/cryosphere-glossary\/isostatic-rebound\" rel=\"nofollow noopener\" target=\"_blank\">isostatic rebound<\/a>, is relatively rapid around southern Hudson Bay; the surface continues to rise about <a href=\"https:\/\/grace.jpl.nasa.gov\/data\/get-data\/gia-trends\/#:~:text=ongoing%20glacial%20isostatic%20rebound%20of%20the%20crust\" rel=\"nofollow noopener\" target=\"_blank\">10 millimeters (0.4 inches) per year<\/a>, or 1 meter per century.<\/p>\n<p>The process has left a fingerprint on the newly emerged land. In this photo, faint, closely spaced ridges parallel the shore of ice-covered James Bay at the terminus of the Harricana river. These <a href=\"https:\/\/uwaterloo.ca\/wetlands-hydrology\/sites\/default\/files\/uploads\/files\/b88-350.pdf\" rel=\"nofollow noopener\" target=\"_blank\">beach ridges<\/a> formed from tidal action reworking sands and silts along the shore, with newer ridges developing along the water as land rises and relative sea level drops.<\/p>\n<p>The Harricana and adjacent waterways flow through boreal peat bogs, or muskeg, in the Hudson Bay Lowlands on their journey out to sea. As the world\u2019s <a href=\"https:\/\/esajournals.onlinelibrary.wiley.com\/doi\/10.1002\/fee.2437\" rel=\"nofollow noopener\" target=\"_blank\">second largest peatland complex<\/a>, the lowlands store significant amounts of soil carbon. Elsewhere around the bay, the landscape retains features <a href=\"https:\/\/doi.org\/10.1016\/j.qsa.2023.100123\" rel=\"nofollow noopener\" target=\"_blank\">carved by glaciers<\/a>, such as <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/drumlin-field-in-northern-canada-85506\/\" rel=\"nofollow noopener\" target=\"_blank\">drumlins<\/a> and <a href=\"https:\/\/www.nps.gov\/articles\/outwashplainsandeskers.htm\" rel=\"nofollow noopener\" target=\"_blank\">eskers<\/a>.<\/p>\n<p>With the approach of summer, the muted colors of the frozen months give way to a more varied palette. Peatlands take on a lush, green appearance, and partially decayed organic matter in the peat releases <a href=\"https:\/\/www.fs.usda.gov\/wildflowers\/ethnobotany\/tannins.shtml\" rel=\"nofollow noopener\" target=\"_blank\">tannins<\/a> that stain the water dark brown <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/some-tea-with-your-river-88843\/\" rel=\"nofollow noopener\" target=\"_blank\">like a strong tea<\/a>. Sea ice that has remained attached to the James Bay shoreline for several months typically begins to break up in mid- to late-May, with <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/james-bay-melts-out-151472\/\" rel=\"nofollow noopener\" target=\"_blank\">melting<\/a> complete by the end of July.<\/p>\n<p>Astronaut photograph\u00a0<a href=\"https:\/\/eol.jsc.nasa.gov\/SearchPhotos\/photo.pl?mission=ISS074&amp;roll=E&amp;frame=417241\" target=\"_blank\" rel=\"noreferrer noopener nofollow\">ISS074-E-417241<\/a> was acquired on March 26, 2026, with a Nikon Z9 digital camera using a focal length of 200 millimeters. It was provided by the ISS Crew Earth Observations Facility and the Earth Science and Remote Sensing Unit at NASA Johnson Space Center. The image was taken by a member of the\u00a0<a href=\"https:\/\/www.nasa.gov\/mission\/expedition-74\/\" target=\"_blank\" rel=\"noreferrer noopener nofollow\">Expedition 74<\/a>\u00a0crew. The image has been cropped and enhanced to improve contrast, and lens artifacts have been removed. The\u00a0<a href=\"https:\/\/www.nasa.gov\/international-space-station\/\" target=\"_blank\" rel=\"noreferrer noopener nofollow\">International Space Station Program<\/a>\u00a0supports the laboratory as part of the\u00a0<a href=\"https:\/\/www.nasa.gov\/international-space-station\/space-station-research-and-technology\/iss-national-laboratory\/\" target=\"_blank\" rel=\"noreferrer noopener nofollow\">ISS National Lab<\/a>\u00a0to help astronauts take pictures of Earth that will be of the greatest value to scientists and the public, and to make those images freely available on the Internet. Additional images taken by astronauts and cosmonauts can be viewed at the NASA\/JSC\u00a0<a href=\"https:\/\/eol.jsc.nasa.gov\/\" target=\"_blank\" rel=\"noreferrer noopener nofollow\">Gateway to Astronaut Photography of Earth<\/a>. Story by Lindsey Doermann.<\/p>\n<p>\t\t\t\t\t<img width=\"4128\" height=\"2752\" src=\"https:\/\/www.newsbeep.com\/ca\/wp-content\/uploads\/2026\/04\/ISS074-E-417243_lrg.jpg\" class=\"attachment-thumbnail size-thumbnail\" alt=\"A snowy landscape in northern Canada reveals frozen river channels as well as ridges parallel to the shore of an icy bay in the upper right.\" style=\"transform: scale(1.2); transform-origin: 50% 50%; object-position: 50% 50%; object-fit: cover;\" block_context=\"nasa-block\" loading=\"lazy\" data-video-loop=\"\" decoding=\"async\"  \/>\t\t\t\t<\/p>\n<p>EBSCO Research Starters (2024) <a href=\"https:\/\/www.ebsco.com\/research-starters\/earth-and-atmospheric-sciences\/hudson-bay\" rel=\"nofollow noopener\" target=\"_blank\">Hudson Bay<\/a>. Accessed April 14, 2026.<\/p>\n<p>GRACE Tellus, <a href=\"https:\/\/grace.jpl.nasa.gov\/data\/get-data\/gia-trends\/\" rel=\"nofollow noopener\" target=\"_blank\">Glacial Isostatic Adjustment (GIA)<\/a>. Accessed April 14, 2026.<\/p>\n<p>NASA Earth Observatory (2023, June 17) <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/james-bay-melts-out-151472\/\" rel=\"nofollow noopener\" target=\"_blank\">James Bay Melts Out<\/a>. Accessed April 14, 2026.<\/p>\n<p>NASA Earth Observatory (2016, October 1) <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/some-tea-with-your-river-88843\/\" rel=\"nofollow noopener\" target=\"_blank\">Some Tea With Your River?<\/a> Accessed April 14, 2026.<\/p>\n<p>Price,\u00a0J.S., et al. (1988) <a href=\"https:\/\/doi.org\/10.1139\/b88-350\" rel=\"nofollow noopener\" target=\"_blank\">Vegetation patterns in James Bay coastal marshes. II. Effects of hydrology on salinity and vegetation<\/a>.\u00a0Canadian Journal of Botany,\u00a066(12): 2586-2594.\u00a0<\/p>\n<p>Rice, J.M., et al. (2024) <a href=\"https:\/\/doi.org\/10.1016\/j.qsa.2023.100123\" rel=\"nofollow noopener\" target=\"_blank\">The surficial geology record of ice stream catchment dynamics and ice-divide migration in the Quebec-Labrador sector of the Laurentide Ice Sheet<\/a>. Quaternary Science Advances, 13, 100123.<\/p>\n","protected":false},"excerpt":{"rendered":"Early spring around Hudson Bay in northern Canada is largely indistinguishable from winter. Sea ice still clings to&hellip;\n","protected":false},"author":2,"featured_media":605455,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[49,48,143020,312,66,306,44716],"class_list":{"0":"post-605454","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-space","8":"tag-ca","9":"tag-canada","10":"tag-earth-observatory","11":"tag-international-space-station-iss","12":"tag-science","13":"tag-space","14":"tag-topography"},"_links":{"self":[{"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/posts\/605454","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/comments?post=605454"}],"version-history":[{"count":0,"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/posts\/605454\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/media\/605455"}],"wp:attachment":[{"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/media?parent=605454"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/categories?post=605454"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.newsbeep.com\/ca\/wp-json\/wp\/v2\/tags?post=605454"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}