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<!DOCTYPE html><html><head><title>Fjord Systems and Archives - Google Books</title><link rel="stylesheet" href="/books/css/_a33f2a89320471e58c940b9287b9d4eb/kl_viewport_kennedy_full_bundle.css" type="text/css" /><link rel="stylesheet"href="https://fonts.googleapis.com/css2?family=Product+Sans:wght@400"><script src="/books/javascript/v2_a33f2a89320471e58c940b9287b9d4eb__en.js"></script><script>_OC_Hooks = ["_OC_Page", "_OC_SearchReload", "_OC_TocReload", "_OC_EmptyFunc", "_OC_SearchPage", "_OC_QuotePage" ];for (var _OC_i = 0; _OC_i < _OC_Hooks.length; _OC_i++) {eval("var " + _OC_Hooks[_OC_i] + ";");}function _OC_InitHooks () {for (var i = 0; i < _OC_Hooks.length; i++) {var func = arguments[i];eval( _OC_Hooks[i] + " = func;");}}</script><link rel="canonical" href="https://books.google.com/books/about/Fjord_Systems_and_Archives.html?id=rTOvGGUYNokC"/><meta property="og:url" content="https://books.google.com/books/about/Fjord_Systems_and_Archives.html?id=rTOvGGUYNokC"/><meta name="title" content="Fjord Systems and Archives"/><meta name="description" content="Fjords are glacially over-deepened, semi-enclosed marine basins, but are often neglected as a sedimentary realm. They represent the transition from the terrestrial to the marine environment and as such have the potential to preserve evidence of environmental change. Typically most fjords have been glaciated a number of times and some high-latitude fjords still possess a resident glacier. The stratigraphic record in fjords largely preserves a glacialdeglacial cycle of deposition. Sheltered water and high sedimentation rates potentially make fjords ideal depositional environments for preserving continuous records of climate and environmental change with high temporal resolution. Fjords are also referred to as miniature oceans providing the unique opportunity to study marine processes in great detail. With predictions of warming climates, changing ocean circulation and rising sea levels, this volume is a timely look at these environmentally sensitive coastlines."/><meta property="og:title" content="Fjord Systems and Archives"/><meta property="og:type" content="book"/><meta property="og:site_name" content="Google Books"/><meta property="og:image" content="https://books.google.com.sg/books/content?id=rTOvGGUYNokC&printsec=frontcover&img=1&zoom=1&edge=curl&imgtk=AFLRE73KkjnVuxIJ0YSnF4sphJrZXIPVzUh9g_IHS89-lPcRzFXtqnirAyzMx_dXyStPNjvQpWzZSmHeJekiIcedGBQAgllHJ4Yez4tGvY8VylitbdicULY8DiYf13pJIEBmB5TOU0hA"/><link rel="image_src" href="https://books.google.com.sg/books/content?id=rTOvGGUYNokC&printsec=frontcover&img=1&zoom=1&edge=curl&imgtk=AFLRE73KkjnVuxIJ0YSnF4sphJrZXIPVzUh9g_IHS89-lPcRzFXtqnirAyzMx_dXyStPNjvQpWzZSmHeJekiIcedGBQAgllHJ4Yez4tGvY8VylitbdicULY8DiYf13pJIEBmB5TOU0hA"/><script></script><style>#gbar,#guser{font-size:13px;padding-top:1px !important;}#gbar{height:22px}#guser{padding-bottom:7px !important;text-align:right}.gbh,.gbd{border-top:1px solid #c9d7f1;font-size:1px}.gbh{height:0;position:absolute;top:24px;width:100%}@media all{.gb1{height:22px;margin-right:.5em;vertical-align:top}#gbar{float:left}}a.gb1,a.gb4{text-decoration:underline !important}a.gb1,a.gb4{color:#00c !important}.gbi .gb4{color:#dd8e27 !important}.gbf .gb4{color:#900 !important} #gbar { padding:.3em .6em !important;}</style></head><body class=""><div id=gbar><nobr><a target=_blank class=gb1 href="https://www.google.com.sg/search?tab=pw">Search</a> <a target=_blank class=gb1 href="https://www.google.com.sg/imghp?hl=en&tab=pi">Images</a> <a target=_blank class=gb1 href="https://maps.google.com.sg/maps?hl=en&tab=pl">Maps</a> <a target=_blank class=gb1 href="https://play.google.com/?hl=en&tab=p8">Play</a> <a target=_blank class=gb1 href="https://www.youtube.com/?tab=p1">YouTube</a> <a target=_blank class=gb1 href="https://news.google.com/?tab=pn">News</a> <a target=_blank class=gb1 href="https://mail.google.com/mail/?tab=pm">Gmail</a> <a target=_blank class=gb1 href="https://drive.google.com/?tab=po">Drive</a> <a target=_blank class=gb1 style="text-decoration:none" href="https://www.google.com.sg/intl/en/about/products?tab=ph"><u>More</u> »</a></nobr></div><div id=guser width=100%><nobr><span id=gbn class=gbi></span><span id=gbf class=gbf></span><span id=gbe></span><a target=_top id=gb_70 href="https://www.google.com/accounts/Login?service=print&continue=https://books.google.com.sg/books%3Fid%3DrTOvGGUYNokC%26q%3Ddebris%2Blobe%26source%3Dgbs_word_cloud_r%26hl%3Den&hl=en&ec=GAZACg" class=gb4>Sign in</a></nobr></div><div class=gbh style=left:0></div><div class=gbh style=right:0></div><div role="alert" style="position: absolute; left: 0; right: 0;"><a href="https://books.google.com.sg/books?id=rTOvGGUYNokC&q=debris+lobe&source=gbs_word_cloud_r&hl=en&output=html_text" title="Screen reader users: click this link for accessible mode. 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They represent the transition from the terrestrial to the marine environment and as such have the potential to preserve evidence of environmental change. Typically most fjords have been glaciated a number of times and some high-latitude fjords still possess a resident glacier. The stratigraphic record in fjords largely preserves a glacialdeglacial cycle of deposition. Sheltered water and high sedimentation rates potentially make fjords ideal depositional environments for preserving continuous records of climate and environmental change with high temporal resolution. Fjords are also referred to as miniature oceans providing the unique opportunity to study marine processes in great detail. With predictions of warming climates, changing ocean circulation and rising sea levels, this volume is a timely look at these environmentally sensitive coastlines.","my_library_url":"https://www.google.com/accounts/Login?service=print\u0026continue=https://books.google.com.sg/books%3Fop%3Dlibrary\u0026hl=en","is_magazine":false,"is_public_domain":false},{"enableUserFeedbackUI":true,"pseudocontinuous":true,"is_cobrand":false,"sign_in_url":"https://www.google.com/accounts/Login?service=print\u0026continue=https://books.google.com.sg/books%3Fid%3DrTOvGGUYNokC%26q%3Ddebris%2Blobe%26source%3Dgbs_word_cloud_r%26hl%3Den\u0026hl=en","isEntityPageViewport":false,"showViewportOnboarding":false,"showViewportPlainTextOnboarding":false},{"page":[{"pid":"PA235","highlights":[{"X":72,"Y":208,"W":27,"H":12},{"X":44,"Y":221,"W":27,"H":11},{"X":78,"Y":221,"W":19,"H":11},{"X":78,"Y":704,"W":27,"H":10},{"X":109,"Y":704,"W":20,"H":10},{"X":140,"Y":741,"W":28,"H":11},{"X":172,"Y":741,"W":20,"H":11},{"X":72,"Y":804,"W":27,"H":11},{"X":335,"Y":105,"W":28,"H":12},{"X":369,"Y":105,"W":20,"H":12},{"X":322,"Y":170,"W":28,"H":12},{"X":342,"Y":262,"W":31,"H":9},{"X":377,"Y":262,"W":22,"H":9},{"X":359,"Y":284,"W":28,"H":9},{"X":390,"Y":284,"W":20,"H":9},{"X":306,"Y":360,"W":28,"H":11},{"X":338,"Y":360,"W":19,"H":11},{"X":334,"Y":463,"W":28,"H":11},{"X":368,"Y":463,"W":20,"H":11},{"X":499,"Y":475,"W":19,"H":12},{"X":295,"Y":526,"W":28,"H":11},{"X":327,"Y":526,"W":20,"H":11},{"X":295,"Y":577,"W":27,"H":11},{"X":326,"Y":577,"W":19,"H":11},{"X":334,"Y":615,"W":27,"H":11},{"X":365,"Y":615,"W":19,"H":11},{"X":458,"Y":691,"W":28,"H":11},{"X":489,"Y":691,"W":19,"H":11}],"flags":8,"order":246,"vq":"debris lobe"}]},null,{"number_of_results":12,"search_results":[{"page_id":"PA179","page_number":"179","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e that was deposited beyond the limit of a surge of Paulabreen in AD 1870. This lobe has a \u0026#39; fresh \u0026#39; appearance with clearly defined limits and more subtle surface morphology ( e.g. creep and block - like features ; Fig . 7 )\u0026nbsp;..."},{"page_id":"PA190","page_number":"190","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e was deposited in relation to this surge . Apart from advances related to surges ( Hagen et al . 1993 ) , the glacier fronts have retreated since c . AD 1900 ( De Geer in Plassen et al . 2004 ) . Characteristics of the modern\u0026nbsp;..."},{"page_id":"PA219","page_number":"219","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e ( Plassen et al . 2004 ; Forwick et al . 2009 ) are indicated . deposited during the rapid deglaciation of the fjord suggested by. 1 \u0026gt; 11,230 cal . BP + Glacier 5 5470-3230 cal . BP Ice Linear features + + + + BFZ + 2 11,230\u0026nbsp;..."},{"page_id":"PA225","page_number":"225","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e and a discrete intact slide block preserved within the postglacial basinal deposits . The former is a localized accumulation linked to a fluvial catch- ment on the adjacent An Teallach massif . These mass - transport\u0026nbsp;..."},{"page_id":"PA226","page_number":"226","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e ; B : Badcaul Slide ; C : Cadail Slide ; LB : rotational slumping in Loch Broom ; LLB : Little Loch Broom Slide Complex ; GI , Gruinard Island . 5 cm Silty clay Sand Silty clay Sandy , silty. 226 M. STOKER ET AL ."},{"page_id":"PA227","page_number":"227","snippet_text":"... debris flows Annat Bay Formation c . 14 ka c . 15 ka c . 25 ka NEOTECTONIC EVENTS Instigation of Little Loch Broom Slide Complex \u0026amp; Badcaul Slide Faulting \u0026amp; folding , Loch Broom Cadail Slide , North Annat Basin Ardessie \u003cb\u003edebris lobe\u003c/b\u003e\u0026nbsp;..."},{"page_id":"PA235","page_number":"235","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e and a discrete slide deposit in core GC088 . These latter two deposits are both associ- ated with the ... \u003cb\u003edebris lobe\u003c/b\u003e that has accumulated at the base of the slope and which becomes progressively buried beneath younger\u0026nbsp;..."},{"page_id":"PA240","page_number":"240","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e appears to be a localized anomalous Holocene sea- floor sediment accumulation linked via a series of ... debris flow lithogenetic unit . Elsewhere in the inner loch , localized sliding and mass - flow deposition\u0026nbsp;..."},{"page_id":"PA322","page_number":"322","snippet_text":"... \u003cb\u003elobe\u003c/b\u003e , which becomes isolated from its upvalley source and thus stagnates in situ , and an inner \u003cb\u003elobe\u003c/b\u003e which remains ... \u003cb\u003edebris\u003c/b\u003e flows in most basins during the late to 322 K. L. MCINTYRE \u0026amp; J. A. HOWE."},{"page_id":"PA371","page_number":"371","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e 225 , 226 , 228 , 232 , 235 , 238 Arisaig Formation 365 , 366 arm , defined 17 Armorella sp . 174 Assynt Glaciogenic Formation 227 , 228 , 229 , 231 , 234 , 235 , 236 Astacolus hyalacrulus 175 Asterigerinata mamilla 85 , 86\u0026nbsp;...","page_url":"https://books.google.com.sg/books?id=rTOvGGUYNokC\u0026pg=PA371\u0026vq=debris+lobe"},{"page_id":"PA372","page_number":"372","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e 235 Badcaul Slide 235 seismic profile 229 Slide Complex 231 , 232 , 233-234 stratigraphy 231 , 235-236 swath bathymetry 230 results discussed mass failure timing 239 mass failure triggering 239-240 mass transport 236-239\u0026nbsp;...","page_url":"https://books.google.com.sg/books?id=rTOvGGUYNokC\u0026pg=PA372\u0026vq=debris+lobe"},{"page_id":"PA378","page_number":"378","snippet_text":"... \u003cb\u003edebris lobe\u003c/b\u003e 235 Badcaul Slide 235 seismic profile 229 Slide Complex 231 , 232 , 233-234 stratigraphy 231 , 235-236 swath bathymetry 230 results discussed mass failure timing 239 mass failure triggering 239-240 Sogndalsfjord ( Norway )\u0026nbsp;...","page_url":"https://books.google.com.sg/books?id=rTOvGGUYNokC\u0026pg=PA378\u0026vq=debris+lobe"}],"search_query_escaped":"debris lobe"},{});</script></div></div></div><script>(function() {var href = window.location.href;if (href.indexOf('?') !== -1) {var parameters = href.split('?')[1].split('&');for (var i = 0; i < parameters.length; i++) {var param = parameters[i].split('=');if (param[0] == 'focus') {var elem = document.getElementById(param[1]);if (elem) {elem.focus();}}}}})();</script>