{"id":1065,"date":"2022-10-23T21:49:14","date_gmt":"2022-10-24T01:49:14","guid":{"rendered":"https:\/\/umaine.edu\/watershedresearch\/?p=1065"},"modified":"2022-11-14T17:13:13","modified_gmt":"2022-11-14T22:13:13","slug":"wpes-hosts-seminar-w-dr-frank-pazzaglia-on-catchment-erosion-in-eastern-north-america","status":"publish","type":"post","link":"https:\/\/umaine.edu\/watershedresearch\/2022\/10\/23\/wpes-hosts-seminar-w-dr-frank-pazzaglia-on-catchment-erosion-in-eastern-north-america\/","title":{"rendered":"WPES Hosts Seminar w\/ Dr. Frank Pazzaglia on Catchment Erosion in Eastern North America"},"content":{"rendered":"<div><span style=\"color: #000080\"><b>Uplift history\u00a0of the eastern North American margin from\u00a0an\u00a0inversion\u00a0of\u00a0fluvial\u00a0topography<\/b><\/span><\/div>\n<div><span style=\"color: #000080\"><strong>Dr. Frank Pazzaglia, Lehigh University<\/strong><\/span><\/div>\n<div><span style=\"color: #000080\"><strong>Wednesday Oct. 26 at Noon<\/strong><\/span><\/div>\n<div><i>This talk explores how the long term record of base level fall (rock uplift) is encoded in the steepness of river long profiles, and how the profiles of an entire catchment can be inverted to extract an uplift history.\u00a0 The Delaware River that drains the mid-Atlantic margin contains classic erosional landforms like wind and water gaps that speak to drainage adjustments to structure, and unsteady base level fall during the Cenozoic.\u00a0 A fluvial inversion of all of the channels in the Delaware catchment that accounts for variable rock type, indicates that base level fall was slow and steady at rates ~20 m\/Myr pre-Miocene, but increased to ~60 m\/Myr in the Miocene, and has been unsteady since then, including base level changes probably associated with glacio-eustatic and GIA processes. The Miocene pulse in base level fall is probably dynamic in nature and matches other records of sedimentation and erosion preserved on the Atlantic Coastal Plain.<\/i><\/div>\n<div>\n<div>Questions regarding the seminar:\u00a0 sean.m.smith@maine.edu<\/div>\n<\/div>\n<div><\/div>\n<div><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-1067\" src=\"https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2022\/10\/Pazzaglia-Seminar_102622-1-300x237.jpg\" alt=\"\" width=\"393\" height=\"310\" \/><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Uplift history\u00a0of the eastern North American margin from\u00a0an\u00a0inversion\u00a0of\u00a0fluvial\u00a0topography Dr. Frank Pazzaglia, Lehigh University Wednesday Oct. 26 at Noon This talk explores how the long term record of base level fall (rock uplift) is encoded in the steepness of river long profiles, and how the profiles of an entire catchment can be inverted to extract an [&hellip;]<\/p>\n","protected":false},"author":644,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_kad_blocks_custom_css":"","_kad_blocks_head_custom_js":"","_kad_blocks_body_custom_js":"","_kad_blocks_footer_custom_js":"","_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"footnotes":""},"categories":[1],"tags":[],"class_list":["post-1065","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v26.9 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>WPES Hosts Seminar w\/ Dr. Frank Pazzaglia on Catchment Erosion in Eastern North America - Watershed Process and Estuary Sustainability Research Group<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, 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