{"id":1599,"date":"2011-05-08T08:29:23","date_gmt":"2011-05-08T12:29:23","guid":{"rendered":"http:\/\/geraldguild.com\/blog\/?p=1599"},"modified":"2024-01-17T06:17:58","modified_gmt":"2024-01-17T11:17:58","slug":"geology-western-central-new-york","status":"publish","type":"post","link":"https:\/\/geraldguild.com\/blog\/2011\/05\/08\/geology-western-central-new-york\/","title":{"rendered":"The Grand Story of Time Told in the Beauty of Today: The Geology of Western and Central New York"},"content":{"rendered":"<p>The geology of Western and Central New York tells an incredible story, the words of which, are laid out in the rolling hills, picturesque valleys, and the seemingly banal roadside cuts throughout this region.\u00a0 The stunningly beautiful cascading waterfalls of Watkins Glen and Ithaca along with the equally dramatic rock city formations of Cattauraugus and Chautauqua Counties round out this tale with a worthy exclamation point.<\/p>\n<figure id=\"attachment_2000\" aria-describedby=\"caption-attachment-2000\" style=\"width: 434px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2000\" title=\"devonian 1\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-1.jpg\" alt=\"\" width=\"434\" height=\"154\" srcset=\"https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-1.jpg 434w, https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-1-300x106.jpg 300w\" sizes=\"auto, (max-width: 434px) 100vw, 434px\" \/><\/a><figcaption id=\"caption-attachment-2000\" class=\"wp-caption-text\">Figure 1: Devonian World View (The proto US is labeled as Laurasia)<\/figcaption><\/figure>\n<p>The nascent bedrock of this region was laid down over 380 million years ago (mya) on what was then an equatorial continent rotated about 45<sup>o<\/sup> clockwise from its current orientation (see Figure 1).\u00a0 The fossil remains and geological features also indicate that this area was submersed under a vast shallow ocean (see Figure 2 below).<\/p>\n<figure id=\"attachment_2001\" aria-describedby=\"caption-attachment-2001\" style=\"width: 235px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-2.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2001 \" title=\"devonian 2\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-2.jpg\" alt=\"\" width=\"235\" height=\"308\" srcset=\"https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-2.jpg 235w, https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-2-228x300.jpg 228w\" sizes=\"auto, (max-width: 235px) 100vw, 235px\" \/><\/a><figcaption id=\"caption-attachment-2001\" class=\"wp-caption-text\">Figure 2: North American then and now &#8211; Current position indicated by blue Long. and Lat. lines &#8211; Former position indicated by diagonal Equator<\/figcaption><\/figure>\n<p>A continental collision with Baltica (proto Europe) starting 410 million years ago (mya) pushed up the Acadian Mountains that once stood mightily along North America&#8217;s east coast.\u00a0 Forces of nature then slowly eroded these huge mountains and the fine particulates flowed deep out onto the Catskill Delta that then covered much of the Southern Tier of New York State, Pennsylvania, Ohio, West Virginia, and eastern Kentucky (Figure 3).<\/p>\n<figure id=\"attachment_1999\" aria-describedby=\"caption-attachment-1999\" style=\"width: 306px\" class=\"wp-caption alignright\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/catskill-delta.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-1999 \" title=\"Catskill Delta\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/catskill-delta.jpg\" alt=\"\" width=\"306\" height=\"114\" srcset=\"https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/catskill-delta.jpg 306w, https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/catskill-delta-300x111.jpg 300w\" sizes=\"auto, (max-width: 306px) 100vw, 306px\" \/><\/a><figcaption id=\"caption-attachment-1999\" class=\"wp-caption-text\">Figure 3: Example of a Delta<\/figcaption><\/figure>\n<p>Over vast periods of time those particulates settled to the bottom of the ocean creating layer upon layer of sediment that eventually lithified: the clay sediments became the shale, the silt became siltstone, and the sand became sandstone (see Figure 4).<\/p>\n<figure id=\"attachment_2002\" aria-describedby=\"caption-attachment-2002\" style=\"width: 288px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-3.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2002\" title=\"devonian 3\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/devonian-3.jpg\" alt=\"\" width=\"288\" height=\"283\" \/><\/a><figcaption id=\"caption-attachment-2002\" class=\"wp-caption-text\">Figure 4: Northeastern US Devonian Deposition Pattern<\/figcaption><\/figure>\n<figure id=\"attachment_2003\" aria-describedby=\"caption-attachment-2003\" style=\"width: 207px\" class=\"wp-caption alignright\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/key-devonian.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2003\" title=\"key devonian\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/key-devonian.jpg\" alt=\"\" width=\"207\" height=\"85\" \/><\/a><figcaption id=\"caption-attachment-2003\" class=\"wp-caption-text\">Devonian Deposition Key for Figure 4<\/figcaption><\/figure>\n<p>Standing in this region 380 mya would have necessitated a boat.\u00a0 There were no rolling hills of green &#8211; just rolling waves of salty water.<\/p>\n<p>It was likely quite hot (average temp 80\u00b0 F) with no appreciable winter and certainly no snow.\u00a0 At the bottom of the ocean lived brachiopods, crinoids, coral, placoderm fish, eurypterids, and trilobites.\u00a0 No mammals yet, not even dinosaurs.<\/p>\n<p>As the mountain sediment inflow slowly filled our sea and worldwide oceanic water levels trended downward, this area slowly approached the shoreline of that shrinking ocean. Today&#8217;s sandstone remains are evidence of beachfront long ago.\u00a0 The Acadians continued to shed contents but, larger material was laid down.\u00a0 The top surface of the current mountain top rock city formations of Cattauraugus and Chautauqua Counties were once the bottom of a shallow sea (see Image 1).\u00a0 The pebbles (see Image 2) in those mighty rock city quartz conglomerate rocks were flushed into this shallow sea by torrential floods.<\/p>\n<figure id=\"attachment_2005\" aria-describedby=\"caption-attachment-2005\" style=\"width: 315px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/rock-city.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2005\" title=\"rock city\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/rock-city.jpg\" alt=\"\" width=\"315\" height=\"236\" srcset=\"https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/rock-city.jpg 315w, https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/rock-city-300x224.jpg 300w\" sizes=\"auto, (max-width: 315px) 100vw, 315px\" \/><\/a><figcaption id=\"caption-attachment-2005\" class=\"wp-caption-text\">Image 1: Rock City Formation, Olean, New York<\/figcaption><\/figure>\n<figure id=\"attachment_2007\" aria-describedby=\"caption-attachment-2007\" style=\"width: 224px\" class=\"wp-caption alignright\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/quartz-conglom.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-2007\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/quartz-conglom-224x300.jpg\" alt=\"Image 2: Quartz Conglomerate, Rock City Formation, Western New York\" width=\"224\" height=\"300\" srcset=\"https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/quartz-conglom-224x300.jpg 224w, https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/quartz-conglom.jpg 246w\" sizes=\"auto, (max-width: 224px) 100vw, 224px\" \/><\/a><figcaption id=\"caption-attachment-2007\" class=\"wp-caption-text\">Image 2: Quartz Conglomerate, Rock City Formation, Western New York<\/figcaption><\/figure>\n<p>It&#8217;s hard to imagine their former lowland status today when standing upon these high points gazing down below at the rolling hills and whittled valleys.<\/p>\n<p><!-- @font-face {   font-family: \"Cambria\"; }p.MsoNormal, li.MsoNormal, div.MsoNormal { margin: 0in 0in 0.0001pt; font-size: 12pt; font-family: \"Times New Roman\"; }div.Section1 { page: Section1; } -->Over yet another immensely vast period of time, the earth remained tectonically active and another continental collision, this time with Africa, pushed up the Allegheny Mountains between 360 and 245 mya.\u00a0 Pangaea, the last super-continent, existed 330 to 220 mya and the dinosaurs reigned supreme on land. \u00a0About 190 mya the Atlantic Ocean opened and began it\u2019s ongoing expanse.\u00a0 Concurrently our continent was propelled north-by-north-west by plate tectonics, slowly bringing it closer to its current northern hemisphere location.\u00a0 During this gradual transition, a mighty asteroid struck near the Yucatan Peninsula (65 mya) causing a cataclysmic global disaster that is believed to have wiped out the dinosaurs (except for those that evolved into our current birds).\u00a0 Small rodent like mammals did survive and thereafter thrived \u2013 ultimately giving rise to us and our fellow mammals.<\/p>\n<p>Until about 1.8 mya the geology of this region remained relatively stable.\u00a0 Things again got exciting as the most recent ice-age commenced.\u00a0 Huge and powerful glaciers slowly carved their way through our landscape gouging out deep valleys and Finger Lake crevasses (see Image 3). \u00a0They slowly plowed through those long accumulated and lithified deposits creating new lower grounds and thus substantial opportunities for erosion.\u00a0 The surviving rock city formations constitute the few locations in NY that were not scoured by those powerful glaciers. Regardless, the near misses that exposed the under layers of more delicate sedimentary rock beds (e.g., shale), led to the erosion of this base material and thus the characteristic breakage and shifting of those conglomerate structures that make them city like today.<\/p>\n<figure id=\"attachment_2004\" aria-describedby=\"caption-attachment-2004\" style=\"width: 252px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/finger-lakes.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2004\" title=\"finger lakes\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/finger-lakes.jpg\" alt=\"\" width=\"252\" height=\"206\" \/><\/a><figcaption id=\"caption-attachment-2004\" class=\"wp-caption-text\">Image 3: New York Finger Lakes &#8211; NASA Image<\/figcaption><\/figure>\n<p>The deep Finger Lake gouges left by the glaciers also left hanging-falls that slowly eroded to form the incredible formations at Watkins Glen, NY (see Image 4), Buttermilk Falls, and Taughannock Falls (in Ithaca, NY).<\/p>\n<figure id=\"attachment_2006\" aria-describedby=\"caption-attachment-2006\" style=\"width: 314px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/watkins-glen.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2006\" title=\"watkins glen\" src=\"http:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/watkins-glen.jpg\" alt=\"\" width=\"314\" height=\"236\" srcset=\"https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/watkins-glen.jpg 314w, https:\/\/geraldguild.com\/blog\/wp-content\/uploads\/2011\/05\/watkins-glen-300x225.jpg 300w\" sizes=\"auto, (max-width: 314px) 100vw, 314px\" \/><\/a><figcaption id=\"caption-attachment-2006\" class=\"wp-caption-text\">Image 4: Watkins Glen State Park, New York<\/figcaption><\/figure>\n<p>About that same time, the high peaks of the Adirondacks were just beginning to rise from the north country plains being uplifted by a magma hotspot. \u00a0\u00a0The Adirondacks are actually composed of bedrock much older than the bedrock exposed in Central and Western New York.<\/p>\n<p>All of these remnant features are unique and incredibly beautiful landmarks that speak volumes about the vast amounts of time and power that played out in this story.\u00a0\u00a0 Whenever you pass a roadside cut, think back to when each layer was once the floor of a warm ocean.\u00a0 Make time to get to Rock City in Olean, Panama Rocks in Panama, NY or Thunder Rocks in Allegany State Park.\u00a0 Think about how the top of those rocks, the relative top of the world in Western New York now, were once the bottom of this world.\u00a0 Then picture mountainous walls of snow and ice halting just in time to spare your ground.\u00a0\u00a0 Finally, imagine their sculpting retreat.\u00a0 What a beautiful and powerful story our wondrous land tells.<\/p>\n<p><strong>References:<\/strong><\/p>\n<p>Allman, W., &amp; Ross, R. (2008). <span style=\"text-decoration: underline;\">Ithaca is Gorges: A Guide to the Geology of the Ithaca Area. 4<sup>th<\/sup> Ed<\/span>. Ithaca: Museum of the Earth.<\/p>\n<p>Ansley, J. (2000). <span style=\"text-decoration: underline;\">The Teacher Friendly Guide to the Geology of the Northeastern U.S.<\/span> Ithaca: Paleontological Research Institute.<\/p>\n<p>Van Diver, B. (1985). <span style=\"text-decoration: underline;\">Roadside Geology of New York<\/span>.\u00a0 Missoula: Mountain Press Publishing Company.<\/p>\n<p>Whiteley, T., Kloc, G., &amp; Brett, C. (2002). <span style=\"text-decoration: underline;\">Trilobites of New York: An Illustrated Guide<\/span>. Ithaca: Cornell University Press.<\/p>\n<p>Figures 1-4: John Wiley and Sons &#8211; used with permission. <a href=\"http:\/\/higheredbcs.wiley.com\/legacy\/college\/levin\/0471697435\/chap_tut\/chaps\/chapter11-03.html\">http:\/\/higheredbcs.wiley.com\/legacy\/college\/levin\/0471697435\/chap_tut\/chaps\/chapter11-03.html<\/a><\/p>\n<p>Images 1, 2, &amp; 4: Photographs by Gerald Guild<\/p>\n<p>Image 3: NASA Image: <a href=\"http:\/\/rst.gsfc.nasa.gov\/Sect6\/Sect6_2.html\">http:\/\/rst.gsfc.nasa.gov\/Sect6\/Sect6_2.html<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>The geology of Western and Central New York tells an incredible story, the words of which, are laid out in the rolling hills, picturesque valleys, and the seemingly banal roadside cuts throughout this region.\u00a0 The stunningly beautiful cascading waterfalls of Watkins Glen and Ithaca along with the equally dramatic rock city formations of Cattauraugus and &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/geraldguild.com\/blog\/2011\/05\/08\/geology-western-central-new-york\/\" class=\"more-link\">Read more<span class=\"screen-reader-text\"> &#8220;The Grand Story of Time Told in the Beauty of Today: The Geology of Western and Central New York&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"jetpack_post_was_ever_published":false,"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_publicize_message":"","jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":false,"jetpack_social_options":{"image_generator_settings":{"template":"highway","default_image_id":0,"font":"","enabled":false},"version":2}},"categories":[66],"tags":[95],"class_list":["post-1599","post","type-post","status-publish","format-standard","hentry","category-geology","tag-science-geology-physics-astronomy-evolutionary-biology-astrobiology"],"jetpack_publicize_connections":[],"jetpack_featured_media_url":"","jetpack_shortlink":"https:\/\/wp.me\/p3mcUm-pN","jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/posts\/1599","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/comments?post=1599"}],"version-history":[{"count":44,"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/posts\/1599\/revisions"}],"predecessor-version":[{"id":3797,"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/posts\/1599\/revisions\/3797"}],"wp:attachment":[{"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/media?parent=1599"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/categories?post=1599"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/geraldguild.com\/blog\/wp-json\/wp\/v2\/tags?post=1599"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}