{"id":3626,"date":"2010-06-16T09:57:55","date_gmt":"2010-06-16T09:57:55","guid":{"rendered":"http:\/\/all-geo.org\/highlyallochthonous\/2010\/06\/the-intimate-coupling-of-hydrologic-and-geomorphic-evolution-of-basalt-landscapes\/"},"modified":"2010-06-16T09:57:55","modified_gmt":"2010-06-16T09:57:55","slug":"the-intimate-coupling-of-hydrologic-and-geomorphic-evolution-of-basalt-landscapes","status":"publish","type":"post","link":"https:\/\/all-geo.org\/highlyallochthonous\/2010\/06\/the-intimate-coupling-of-hydrologic-and-geomorphic-evolution-of-basalt-landscapes\/","title":{"rendered":"The intimate coupling of hydrologic and geomorphic evolution of basalt landscapes"},"content":{"rendered":"

\"A<\/span>\"ResearchBlogging.org\"<\/a><\/span>
\nHow does a landscape go from looking like this…<\/p>\n

\"<2000<\/a>
\n~1500 year old basaltic lava landscape with no surface drainage<\/div>\n

to looking like this?<\/p>\n

\"2<\/a>
\n2 Million year old landscape on basaltic lava. Note steep slopes and incised valleys<\/div>\n

Find out in my new paper in Earth Surface Processes and Landforms<\/a>.
\nHint: Using a chronosequence of watersheds in the Oregon Cascades, we argue that the rates and processes of landscape evolution are driven by whether the water sinks into the lava flows and moves slowly toward springs with steady hydrographs or whether the water moves quickly through the shallow subsurface and creates streams with flashy hydrographs. Further, we suggest that this water routing is controlled by an elusive landscape-scale permeability which decreases over time as processes like chemical weathering create soil and clog up pores in the rock. And as a bonus, because of the high initial permeability of basaltic landscapes, the formation of stream networks and the dissection of the landscape appears to take far longer than in places with less permeable lithologies.
\nJefferson, A., Grant, G., Lewis, S., & Lancaster, S. (2010). Coevolution of hydrology and topography on a basalt landscape in the Oregon Cascade Range, USA Earth Surface Processes and Landforms, 35<\/span> (7), 803-816 DOI: 10.1002\/esp.1976<\/a><\/span><\/p>\n","protected":false},"excerpt":{"rendered":"

In a new paper, I show that, on basalts, flowpaths, hydographs, and landscapes coevolve over a million years or more.
\n Continue reading →<\/span><\/a><\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[46,144,49,11,12],"tags":[],"class_list":["post-3626","post","type-post","status-publish","format-standard","hentry","category-by-anne","category-geomorphology","category-hydrology","category-paper-reviews","category-volcanoes"],"_links":{"self":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/3626","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/comments?post=3626"}],"version-history":[{"count":0,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/3626\/revisions"}],"wp:attachment":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/media?parent=3626"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/categories?post=3626"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/tags?post=3626"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}