{"id":3629,"date":"2010-06-02T07:15:00","date_gmt":"2010-06-02T07:15:00","guid":{"rendered":"http:\/\/all-geo.org\/highlyallochthonous\/2010\/06\/accretionary-wedge-25-an-illustrated-glossary-of-cool-geological-things\/"},"modified":"2010-07-11T09:58:19","modified_gmt":"2010-07-11T09:58:19","slug":"accretionary-wedge-25-an-illustrated-glossary-of-cool-geological-things","status":"publish","type":"post","link":"https:\/\/all-geo.org\/highlyallochthonous\/2010\/06\/accretionary-wedge-25-an-illustrated-glossary-of-cool-geological-things\/","title":{"rendered":"Accretionary Wedge #25: An Illustrated Glossary of Cool Geological Things"},"content":{"rendered":"<p><span style=\"float: left; padding: 5px;\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/chrisicon2.jpg\" alt=\"A post by Chris Rowan\" width=\"49\" height=\"50\" \/><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/anneicon.jpg\" alt=\"A post by Anne Jefferson\" width=\"49\" height=\"50\" \/><\/span>Welcome to the latest edition of the <a href=\"http:\/\/theaccretionarywedge.wordpress.com\"><\/a>Accretionary Wedge geoblogging carnival. We&#8217;ve been delighted by the response to our call for your favourite geological imagery, and the number of nominations we&#8217;ve received has been matched by their diversity &#8211; images have ranged from the microscopic to continental scales, from the depths of geological time to the present day, from the igneous to the sedimentary. The only way we could think of to do this smorgasboard of earth science justice was in the form of a visual dictionary, matching the images you&#8217;ve provided to the feature or process that they exemplify. Clicking on each image will allow you to see it in all its full-resolution glory at the original post, which in many cases also provides some more background on the geological feature or process depicted. Fun, pretty and at least a little bit educational &#8211; we hope you&#8217;ll have as much fun looking through our little glossary as we had putting it together.<\/p>\n<div style=\"width: 600px;\">\n<div>\n<h2>A<\/h2>\n<\/div>\n<p><a name=\"arch\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Arch, natural<\/strong> &#8211; Formed by differential erosion at the base of a narrow ridge.<\/p>\n<p>Photo: Arch, Arches National Park from <a href=\"http:\/\/geotripper.blogspot.com\/2010\/05\/my-favorite-geology-foto-mays.html\">Geotripper<\/a><\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/geotripper.blogspot.com\/2010\/05\/my-favorite-geology-foto-mays.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Geotripper.jpg\" alt=\"Geotripper.jpg\" width=\"250\" height=\"187\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>B<\/h2>\n<\/div>\n<p><a name=\"beach\"><\/a><\/p>\n<div style=\"height: 220px; width: 330px; float: left;\"><strong>Beach<\/strong> &#8211; deposit of unconsolidated sediment (sand, gravel, or shell fragments) at the land-water interface. One of many coastal zone morphologies.<\/p>\n<p>Photo: Unknown beach with channel deposits. From <a href=\"http:\/\/throughthesandglass.typepad.com\/through_the_sandglass\/2010\/05\/beach-patterns-accretionary-wedge-geoimage-bonanza.html\">Michael Welland<\/a>.<\/p>\n<\/div>\n<div style=\"height: 220px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/throughthesandglass.typepad.com\/through_the_sandglass\/2010\/05\/beach-patterns-accretionary-wedge-geoimage-bonanza.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Sandglass.jpg\" alt=\"Sandglass.jpg\" width=\"250\" height=\"209\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"breccia\"><\/a><\/p>\n<div style=\"height: 170px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/geosciblog.blogspot.com\/2010\/05\/favorite-geophotos-for-accretionary.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/GeoSciBlog-breccia.jpg\" alt=\"GeoSciBlog breccia.jpg\" width=\"250\" height=\"157\" \/><\/a><\/div>\n<div style=\"height: 170px; width: 330px; float: right;\"><strong>Breccia<\/strong> &#8211; coarse sedimentary or volcanic rock with angular clasts<\/p>\n<p>Photo:  Pyroclastic breccia, Eagle Mtns, west Texas. From <a href=\"http:\/\/geosciblog.blogspot.com\/2010\/05\/favorite-geophotos-for-accretionary.html\">geosciblog<\/a>.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"butte\"><\/a><\/p>\n<div style=\"height: 220px; width: 330px; float: left;\"><strong>Butte<\/strong> &#8211; prominent, isolated hill with steep sides and flat top. Smaller than a mesa.<\/p>\n<p>Photo: Monument Valley by <a href=\"http:\/\/jazinator.blogspot.com\/2010\/03\/pretty-cool-picture-of-monument-valley.html\">Dino Jim<\/a>.<\/p>\n<\/div>\n<div style=\"height: 220px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/jazinator.blogspot.com\/2010\/03\/pretty-cool-picture-of-monument-valley.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Dino-Jim-Mon-Valley.jpg\" alt=\"Dino Jim Mon Valley.jpg\" width=\"250\" height=\"177\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>C<\/h2>\n<\/div>\n<p><a name=\"canyon\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Canyon (or gorge)<\/strong> &#8211; a deep, steep-sided valley, often formed by a river incising into a plateau or mountain range.<\/p>\n<p>Photo: Canyonlands National Park  from <a href=\"http:\/\/geologyhappens.blogspot.com\/2010\/05\/geo-image-bonanza-aw-24.html\">Geology Happens<\/a><\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/geologyhappens.blogspot.com\/2010\/05\/geo-image-bonanza-aw-24.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Geology-Happens.jpg\" alt=\"Geology Happens.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"coastal_zone\"><\/a><\/p>\n<div style=\"height: 200px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/geologiamarinha.blogspot.com\/2010\/05\/accretionary-wedge-geo-images.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/ebb-tidal-delta.jpg\" alt=\"ebb tidal delta.jpg\" width=\"250\" height=\"169\" \/><\/a><\/div>\n<div style=\"height: 200px; width: 330px; float: right;\"><strong>Coastal zone<\/strong> &#8211; region where interaction of terrestrial and marine processes occurs. Morphology can take the form of a beach, barrier island, delta, cliff, or wave-cut platform.<\/p>\n<p>Photo: Ebb-tidal delta &#8211; eastern Brazil. From <a href=\"http:\/\/geologiamarinha.blogspot.com\/2010\/05\/accretionary-wedge-geo-images.html\">Geologia Marinha e Costeira<\/a>.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"conglomerate\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Conglomerate <\/strong> &#8211; coarse sedimentary rock with rounded clasts.<\/p>\n<p>Photo: Ogallala\/Arikaree formation near the Pawnee Buttes in north eastern Colorado (conglomerate butte landscape) from <a href=\"http:\/\/www.flickr.com\/photos\/flight0001\/4283129331\/in\/set-72157617689162564\"><\/a>Russ Dale<\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/www.flickr.com\/photos\/flight0001\/4283129331\/in\/set-72157617689162564\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Dale%20Cong.jpg\" alt=\"Dale Cong.jpg\" width=\"250\" height=\"188\" \/><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>D<\/h2>\n<\/div>\n<p><a name=\"debris_flow\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Debris flow<\/strong> &#8211; type of mass wasting where large clasts are carried in a mud-water mixture.<\/p>\n<p>Photo: Debris flows, Pacific NW. From <a href=\"https:\/\/all-geo.org\/highlyallochthonous\/2010\/05\/when-it-rains-a-lot-and-the-mountains-fall-down\"><\/a>Anne Jefferson<\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"https:\/\/all-geo.org\/highlyallochthonous\/2010\/05\/when-it-rains-a-lot-and-the-mountains-fall-down\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Debris%20flow.jpg\" alt=\"Debris flow.jpg\" width=\"250\" height=\"188\" \/><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"dessication_cracks\"><\/a><\/p>\n<div style=\"height: 200px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/poolsandriffles.blogspot.com\/2010\/05\/riviere-de-terre.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/PoolsRiffles.jpg\" alt=\"PoolsRiffles.jpg\" width=\"250\" height=\"117\" \/><\/a><\/div>\n<div style=\"height: 200px; width: 330px; float: right;\"><strong>Dessication cracks<\/strong> &#8211; fractures formed by the shrinkage of clay, silt, or mud as it dries out from subaerial exposure.<\/p>\n<p>Photo: Riviere de Terre &#8211; natural &#8216;artwork&#8217; featuring dried, cracked clay. From <a href=\"http:\/\/poolsandriffles.blogspot.com\/2010\/05\/riviere-de-terre.html\">Pools and Riffles<\/a>.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"diagenesis\"><\/a><\/p>\n<div style=\"height: 250px; width: 330px; float: left;\"><strong>Diagenesis<\/strong> &#8211; post-depositional alteration of sediments at low temperatures and pressures, often leading to the growth of new minerals in response to changing geochemical conditions.<\/p>\n<p>Photo: pendant calcite crystals precipitated within meteoric aquifers during late Ordovician sea-level fall, Appalachians. From <a href=\"http:\/\/suvratk.blogspot.com\/2010\/05\/accretionary-wedge-geo-images-calcite.html\">Suvrat<\/a>.<\/p>\n<\/div>\n<div style=\"height: 250px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/suvratk.blogspot.com\/2010\/05\/accretionary-wedge-geo-images-calcite.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Suvrat.jpg\" alt=\"Suvrat.jpg\" width=\"250\" height=\"224\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"diff_weathering\"><\/a><\/p>\n<div style=\"height: 280px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/gmcgeology.blogspot.com\/2010\/05\/geology-paintings-works-of-levi-wells.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Taconic.jpg\" alt=\"Taconic.jpg\" width=\"250\" height=\"181\" \/><\/a><\/div>\n<div style=\"height: 280px; width: 330px; float: right;\"><strong>Differential weathering<\/strong> &#8211; divergence in the degree of weathering and erosion of different lithologies exposed to the same environment. Differential weathering is a factor in the formation of arches, buttes, and mesas, as well as steep slopes where some layers form vertical cliffs and other rock layers have subvertical exposures.<\/p>\n<p>Picture:  Letchworth State Park in Castille, NY, painted by Levi Wells. From <a href=\"http:\/\/gmcgeology.blogspot.com\/2010\/05\/geology-paintings-works-of-levi-wells.html\">John van Hoesen.<\/a><\/p>\n<\/div>\n<\/div>\n<p><!--more--><\/p>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>E<\/h2>\n<\/div>\n<p><a name=\"exposure\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Exposure<\/strong> &#8211;  the amount of geology that is exposed on the surface, and not hidden by pesky vegetation, soils, etc.<\/p>\n<p>Photo: Cerro Divisadero, Patagonia, from <a href=\"http:\/\/clasticdetritus.com\/2010\/05\/28\/geo-image-extravaganza-my-header-photograph\"><\/a>Brian Romans<\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/clasticdetritus.com\/2010\/05\/28\/geo-image-extravaganza-my-header-photograph\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/BrianR%20Patagonia.jpg\" alt=\"BrianR Patagonia.jpg\" width=\"250\" height=\"169\" \/><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"extinction\"><\/a><\/p>\n<div style=\"height: 340px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/my.opera.com\/nielsol\/blog\/accretionary-wedge-geo-image\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Olelog%20KT.jpg\" alt=\"Olelog KT.jpg\" width=\"250\" height=\"87\" \/><\/a><a href=\"http:\/\/geologyblues.blogspot.com\/2010\/05\/accretionary-wedge.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Geology%20Blues%20KT.jpg\" alt=\"Geology Blues KT.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<div style=\"height: 340px; width: 330px; float: right;\"><strong>Extinction event<\/strong> &#8211; abrupt disappearance of species, often as a result of extreme environmental changes, which can also result in a prominent lithological boundary. Significant (mass) extinction events include:<\/p>\n<p>&#8211; <strong>K\/T (or K\/Pg) boundary<\/strong>, 65 million years ago<\/p>\n<p>Photos: (top) KT boundary at Stevns Klint in Denmark.  From <a href=\"http:\/\/my.opera.com\/nielsol\/blog\/accretionary-wedge-geo-image\">olelog<\/a>.<\/p>\n<p>(bottom) KT boundary, Makoshika State Park, Montana.  From <a href=\"http:\/\/geologyblues.blogspot.com\/2010\/05\/accretionary-wedge.html\">Geology Blues<\/a><\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\">\n<p>&#8211; <strong>Permo-Triassic boundary<\/strong>, 250 million years ago.<\/p>\n<p>Photo: Permo-Triassic transition, Dolomites, N Italy. From <a href=\"http:\/\/schmunda.blogspot.com\/2010\/05\/accretionary-wedge-25-geo-image.html\">Nologic<\/a>.<\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/schmunda.blogspot.com\/2010\/05\/accretionary-wedge-25-geo-image.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Nologic.jpg\" alt=\"Nologic.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>F<\/h2>\n<\/div>\n<p><a name=\"folding\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Folding<\/strong> &#8211; deformation of formerly horizontal layers of rock, usually due to compression.<\/p>\n<p>Photo: Kings Canyon National Park. From <a href=\"http:\/\/helenaheliotrope.blogspot.com\/2010\/06\/kings-canyon-national-park.html\">Helena Heilotrope<\/a><\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/helenaheliotrope.blogspot.com\/2010\/06\/kings-canyon-national-park.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Folding.jpg\" alt=\"Folding.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a><\/a><\/p>\n<div style=\"height: 200px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/failedrift.wordpress.com\/2010\/05\/13\/accretionary-wedge-geo-images-wish-list\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Failed%20Rift%20Lamurde.jpg\" alt=\"Failed Rift Lamurde.jpg\" width=\"250\" height=\"192\" \/><\/div>\n<div style=\"height: 200px; width: 330px; float: right;\"><strong>_, plunging <\/strong> &#8211; non-horizontal fold axes, due to later deformation events.<\/p>\n<p>Photo: Lamurde Anticline, from <a href=\"http:\/\/failedrift.wordpress.com\/2010\/05\/13\/accretionary-wedge-geo-images-wish-list\"><\/a>Failed Rift.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a><\/a><\/p>\n<div style=\"height: 260px; width: 400px; float: left;\"><strong>_,  ptygmatic <\/strong> &#8211; occurs in sequences with high viscosity contrasts between layers.<\/p>\n<p>Photo: ptygmatic folding in metagraywacke, from <a href=\"http:\/\/mountainbeltway.wordpress.com\/2010\/04\/03\/ptyggie\"><\/a>Callan Bentley.<\/p>\n<\/div>\n<div style=\"height: 260px; width: 180px; float: right; padding: 5px;\"><a href=\"http:\/\/mountainbeltway.wordpress.com\/2010\/04\/03\/ptyggie\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Callan.jpg\" alt=\"Callan.jpg\" width=\"153\" height=\"250\" \/><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a><\/a><\/p>\n<div style=\"height: 200px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/img25.imageshack.us\/img25\/1356\/dscn1940h.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Overturn.jpg\" alt=\"Overturn.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<div style=\"height: 200px; width: 330px; float: right;\"><strong>_, overturned, recumbant<\/strong> &#8211; where high deformation leads to inversion of stratigraphy in fold limbs.<\/p>\n<p>Photo: overturned syncline at Dog Canyon, Big Bend National Park.  From <a href=\"http:\/\/img25.imageshack.us\/img25\/1356\/dscn1940h.jpg\">Antonio<\/a><\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>G<\/h2>\n<\/div>\n<p><a name=\"gooseneck\"><\/a><\/p>\n<div style=\"height: 160px; width: 330px; float: left;\"><strong>Gooseneck<\/strong> &#8211; the pinched bit of land in an extremely bowed stream meander.<\/p>\n<p>Photo: Goosenecks, Utah. From <a href=\"http:\/\/failedrift.wordpress.com\/2010\/05\/13\/accretionary-wedge-geo-images-wish-list\"><\/a>Failed Rift.<\/p>\n<\/div>\n<div style=\"height: 160px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/failedrift.wordpress.com\/2010\/05\/13\/accretionary-wedge-geo-images-wish-list\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Failed%20Rift%20Goosenecks.jpg\" alt=\"Failed Rift Goosenecks.jpg\" width=\"250\" height=\"150\" \/><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"gulleywasher\"><\/a><\/p>\n<div style=\"height: 260px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/geofroth.posterous.com\/some-memorable-geo-events-in-photo-form\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/GeoFroth%20GCanyon%20Rain.jpg\" alt=\"GeoFroth GCanyon Rain.jpg\" width=\"188\" height=\"250\" \/><\/a><\/div>\n<div style=\"height: 260px; width: 330px; float: right;\"><strong>Gullywasher<\/strong> &#8211; an intense rainstorm that activates ephemeral channels.<\/p>\n<p>Photo: the most epic rainstorm of <a href=\"http:\/\/geofroth.posterous.com\/some-memorable-geo-events-in-photo-form\">Kyle House&#8217;s<\/a> life.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>H<\/h2>\n<\/div>\n<p><a name=\"hematite\"><\/a><\/p>\n<div style=\"height: 240px; width: 330px; float: left;\"><strong>Hematite<\/strong> &#8211;  iron oxide (Fe2O3), a common product of weathering and other low temperature alteration.<\/p>\n<p>Photo: Hematite sheets, Red River Gorge, Kentucky. From <a href=\"http:\/\/stubotics.com\/geoalbum\/hematite-R.jpg\">Stubotics<\/a><\/p>\n<\/div>\n<div style=\"height: 240px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/stubotics.com\/geoalbum\/hematite-R.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/stubonics.jpg\" alt=\"stubonics.jpg\" width=\"250\" height=\"231\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>J<\/h2>\n<\/div>\n<p><a name=\"jointing\"><\/a><\/p>\n<div style=\"height: 310px; width: 330px; float: left;\"><strong>Jointing<\/strong> &#8211; rock fractures with no displacement across the fracture. Can be the result of regional stresses or cooling of volcanic rock.<\/p>\n<p>Photo: Long&#8217;s Peak, from <a href=\"http:\/\/pascals-puppy.blogspot.com\/2010\/05\/longs-peak-album.html\">Pascal<\/a><\/p>\n<\/div>\n<div style=\"height: 310px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/pascals-puppy.blogspot.com\/2010\/05\/longs-peak-album.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Pascal%20Longs%20Peak.jpg\" alt=\"Pascal Longs Peak.jpg\" width=\"250\" height=\"307\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>K<\/h2>\n<\/div>\n<p><a name=\"kyanite\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Kyanite<\/strong> &#8211; an aluminum-rich silica mineral (Al2SiO5), commonly deep blue in color, that generally forms during high pressure metamorphism.<\/p>\n<p>Photo: Metamorphic kyanite, Scotland. From <a href=\"http:\/\/a-life-long-scholar.blogspot.com\/2010\/05\/barrows-kyanite-zone.html\">Life-Long Scholar<\/a><\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/LLScholar%20Kyanite.jpg\" alt=\"LLScholar Kyanite.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>L<\/h2>\n<\/div>\n<p><a name=\"landslide_dam\"><\/a><\/p>\n<div style=\"height: 250px; width: 330px; float: left;\"><strong>Landslide dam<\/strong> &#8211; formed when a landslide blocks a river valley, these natural dams impound water upstream. Such dams can create hazards if the upstream impounded water floods property or if they suddenly overtop or breach releasing a flood wave downstream.<\/p>\n<p>Photo: Attabad landslide, Hunza, N. Pakistan   from <a href=\"http:\/\/daveslandslideblog.blogspot.com\/2010\/05\/retrogressive-erosion-at-attabad.html\">Dave&#8217;s Landslide Blog<\/a><\/p>\n<\/div>\n<div style=\"height: 250px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/daveslandslideblog.blogspot.com\/2010\/05\/retrogressive-erosion-at-attabad.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Landslide%20dam.jpg\" alt=\"Landslide dam.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"lava_lake\"><\/a><\/p>\n<div style=\"height: 200px; width: 260px; float: left; padding: 5px;\"><a href=\"https:\/\/all-geo.org\/highlyallochthonous\/2010\/05\/lava-lake-tectonics\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Erte_Ale_1.jpg\" alt=\"Erte_Ale_1.jpg\" width=\"250\" height=\"181\" \/><\/div>\n<div style=\"height: 200px; width: 330px; float: right;\"><strong>Lava Lake<\/strong> &#8211; body of mostly molten lava contained within a depression over a volcanic vent.<\/p>\n<p>Photo: Erta Ale, Afar, Ethiopia from <a href=\"https:\/\/all-geo.org\/highlyallochthonous\/2010\/05\/lava-lake-tectonics\"><\/a>Chris Rowan<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>M<\/h2>\n<\/div>\n<p><a name=\"mesa\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Mesa<\/strong> &#8211; tableland with steep sides and flat top of uplifted, erosion-resistant rock. A mesa is generally larger than a butte.<\/p>\n<p>Photo: North Caineville Mesa, just east of Capitol Reef National Park in southern Utah. From <a href=\"http:\/\/jrepka.blogspot.com\/2010\/05\/accretionary-wedge-geo-image-bonanza.html\">Jim Repka<\/a>.<\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/jrepka.blogspot.com\/2010\/05\/accretionary-wedge-geo-image-bonanza.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Repka%20Mesa.jpg\" alt=\"Repka Mesa.jpg\" width=\"250\" height=\"167\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"mountain\"><\/a><\/p>\n<div style=\"height: 200px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/outsidetheinterzone.blogspot.com\/2010\/05\/accretionary-wedge-geo-images.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Lockwood.jpg\" alt=\"Lockwood.jpg\" width=\"250\" height=\"184\" \/><\/a><\/div>\n<div style=\"height: 200px; width: 330px; float: right;\"><strong>Mountain<\/strong> &#8211; the natural habitat of the geologist.<\/p>\n<p>Photo: Ansel Adams, Winter Sunrise, Sierra Nevada. From <a href=\"http:\/\/outsidetheinterzone.blogspot.com\/2010\/05\/accretionary-wedge-geo-images.html\">Lockwood<\/a>.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>O<\/h2>\n<\/div>\n<p><a name=\"ooid\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Ooids<\/strong> &#8211; round, concentrically layered sedimentary grains, usually of calcium carbonate.<\/p>\n<p>Photo: Photomicrograph of ooids in a Jurassic carbonate, from <a href=\"http:\/\/lostgeologist.blogspot.com\/2010\/05\/accretionary-wedge-geo-image-bonanza.html\">Lost Geologist<\/a><\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/lostgeologist.blogspot.com\/2010\/05\/accretionary-wedge-geo-image-bonanza.html\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/LostGeo.jpg\" alt=\"LostGeo.jpg\" width=\"250\" height=\"188\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"ore\"><\/a><\/p>\n<div style=\"height: 260px; width: 330px; float: left; padding: 5px;\"><a href=\"http:\/\/highway8a.blogspot.com\/2010\/05\/accretionary-wedge-geo-images-gold-with.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/LfDetach%20Gold.jpg\" alt=\"LfDetach Gold.jpg\" width=\"200\" height=\"250\" \/><\/a><\/div>\n<div style=\"height: 260px; width: 260px; float: right;\"><strong>Ore<\/strong> &#8211; rocks containing high concentrations of economically useful minerals.<\/p>\n<p>Photo: Gold with naumannite (Ag2Se), Northern Nevada. From <a href=\"http:\/\/highway8a.blogspot.com\/2010\/05\/accretionary-wedge-geo-images-gold-with.html\">Silver Fox<\/a>.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>P<\/h2>\n<\/div>\n<p><a name=\"pioneer_sp\"><\/a><\/p>\n<div style=\"height: 260px; width: 390px; float: left;\"><strong>Pioneer Species<\/strong> &#8211; the first organisms to colonise bare land, either newly created or swept clean by fire or flood.<\/p>\n<p>Photo: First colonisation of lava flow by plant  from <a href=\"http:\/\/magmacumlaude.blogspot.com\/2010\/05\/geo-image-accretionary-wedge.html\">Magma Cum Laude<\/a>.<\/p>\n<\/div>\n<div style=\"height: 260px; width: 200px; float: right; padding: 5px;\"><a href=\"http:\/\/magmacumlaude.blogspot.com\/2010\/05\/geo-image-accretionary-wedge.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Magma%20Cum%20Laude.jpg\" alt=\"Magma Cum Laude.jpg\" width=\"188\" height=\"250\" \/><\/a>.<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"power_law_creep\"><\/a><\/p>\n<div style=\"height: 250px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/news.discovery.com\/earth\/zooms\/earth-mentle-crust-alaska.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/mantle-zoom.jpg\" alt=\"mantle-zoom.jpg\" width=\"250\" height=\"152\" \/><\/a><\/div>\n<div style=\"height: 250px; width: 330px; float: right;\"><strong>Power Law Creep<\/strong> &#8211; a type of deformation where small increases in applied stress leads to greatly increased strain rates. Thought to control deformation in the mantle explaining how you can get extremely rapid mantle flow around subducting slabs.<\/p>\n<p>Picture: model of mantle flow around subducting Alaskan slab, from <a href=\"http:\/\/news.discovery.com\/earth\/zooms\/earth-mentle-crust-alaska.html\">Discovery News<\/a>.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"precipice\"><\/a><\/p>\n<div style=\"height: 240px; width: 330px; float: left;\"><strong>Precipice<\/strong> &#8211; often encountered by single minded geologists in search of the perfect outcrop.<\/p>\n<p>Photo: from <a href=\"http:\/\/geofroth.posterous.com\/some-memorable-geo-events-in-photo-form\">Kyle House<\/a>.<\/p>\n<\/div>\n<div style=\"height: 240px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/geofroth.posterous.com\/some-memorable-geo-events-in-photo-form\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/GeoForth%20Snake%20Cliff.jpg\" alt=\"GeoForth Snake Cliff.jpg\" width=\"250\" height=\"229\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>S<\/h2>\n<\/div>\n<p><a name=\"ref_seismic\"><\/a><\/p>\n<div style=\"height: 260px; width: 390px; float: left;\"><strong>Seismic Reflection Survey<\/strong> &#8211; controlled release of sound waves to examine the subsurface structure of the Earth. Modern computer processing provides extremely high spatial resolution.<\/p>\n<p>Photo: Buried paleo-channels in Gulf of Mexico. From <a href=\"http:\/\/zsylvester.blogspot.com\/2010\/05\/deep-sea-landscapes-from-ice-age.html\">Hindered Settling<\/a>.<\/p>\n<\/div>\n<div style=\"height: 260px; width: 200px; float: right; padding: 5px;\"><a href=\"http:\/\/zsylvester.blogspot.com\/2010\/05\/deep-sea-landscapes-from-ice-age.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/HindSett%20Sesimic1.jpg\" alt=\"HindSett Sesimic1.jpg\" width=\"188\" height=\"250\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"seismogram\"><\/a><\/p>\n<div style=\"height: 160px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/hypocentral.com\/blog\/2010\/06\/01\/accretionary-wedge-25-images\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/seismogram.jpg\" alt=\"seismogram.jpg\" width=\"250\" height=\"119\" \/><\/div>\n<div style=\"height: 160px; width: 330px; float: right;\"><strong>Seismogram<\/strong> &#8211; a visual record of ground motions due to an earthquake.<\/p>\n<p>Photo: Seismograph for Mb 6.0 earthquake beneath the Kermadec Islands on Sept 21, 1981, recorded at Adelaide, Australia. From <a href=\"http:\/\/hypocentral.com\/blog\/2010\/06\/01\/accretionary-wedge-25-images\"><\/a>Hypocentre.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>T<\/h2>\n<\/div>\n<p><a name=\"tilting\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Tilting<\/strong> &#8211; regional deviation of beds away from the horizontal, usually in response to regional tectonic uplift.<\/p>\n<p>Photo: Tilted sandstones, Fountain Valley, Roxborough State Park near Denver, Colorado. From <a href=\"http:\/\/www.flickr.com\/photos\/flight0001\/3965140613\/in\/set-72157623946574927\"><\/a>Russ Dale<\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/www.flickr.com\/photos\/flight0001\/3965140613\/in\/set-72157623946574927\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Dale%20sst.jpg\" alt=\"Dale sst.jpg\" width=\"250\" height=\"196\" \/><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<p><a name=\"twinning\"><\/a><\/p>\n<div style=\"height: 260px; width: 180px; float: left; padding: 5px;\"><a><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Geoberg.jpg\" alt=\"Geoberg.jpg\" width=\"167\" height=\"250\" \/><\/a><\/div>\n<div style=\"height: 260px; width: 400px; float: right;\"><strong>Twinning<\/strong> &#8211; where a crystal is subdivided into regions with different lattice alignments.<\/p>\n<p>Photo: twinned selenite (sparry gypsum), from <a href=\"http:\/\/www.geoberg.de\/blog\/geoblogosphaere-web-2-0\/mein-beitrag-zum-aktuellen-accretionary-wedge-geo-image-bonanza\">Lutz<\/a>.<\/p>\n<\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div>\n<h2>V<\/h2>\n<\/div>\n<p><a name=\"volcano\"><\/a><\/p>\n<div style=\"height: 200px; width: 330px; float: left;\"><strong>Volcano<\/strong> &#8211; an opening in the Earth&#8217;s surface through which lava, ash, or gases are erupted. Volcanoes chiefly occur in regions where rifting, subduction, or hot spots have triggered melting of the mantle.<\/p>\n<p>Photo: Mt St Helens &#8211; volcano above a subduction zone. From <a href=\"http:\/\/shortgeologist.blogspot.com\/2010\/05\/accretionary-wedge.html\">Short Geologist<\/a>.<\/p>\n<\/div>\n<div style=\"height: 200px; width: 260px; float: right; padding: 5px;\"><a href=\"http:\/\/shortgeologist.blogspot.com\/2010\/05\/accretionary-wedge.html\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/scienceblogs.com\/highlyallochthonous\/upload\/2010\/06\/Short%20Geologist%20Mt%20St%20Helens.jpg\" alt=\"Short Geologist Mt St Helens.jpg\" width=\"250\" height=\"144\" \/><\/a><\/div>\n<\/div>\n<div style=\"clear: both; width: 600px;\">\n<div style=\"height: 200px; width: 260px; float: left; padding: 5px;\"><a href=\"http:\/\/scienceblogs.com\/eruptions\/2010\/05\/a_closer_look_at_the_eyjafjall.php\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2010\/07\/Eyjafjallajokul.jpg\" alt=\"Eyjafjallajokul.jpg\" width=\"250\" height=\"195\" \/><\/a><\/div>\n<div style=\"height: 200px; width: 330px; float: right;\">Photo: Eyjafjallajokull, Iceland &#8211; volcano at a rift zone from <a href=\"http:\/\/scienceblogs.com\/eruptions\/2010\/05\/a_closer_look_at_the_eyjafjall.php\">Eruptions<\/a>.<\/p>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>A smorgasboard of earth science imagery, in visual dictionary form.<br \/>\n <a href=\"https:\/\/all-geo.org\/highlyallochthonous\/2010\/06\/accretionary-wedge-25-an-illustrated-glossary-of-cool-geological-things\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[4,26],"tags":[206],"class_list":["post-3629","post","type-post","status-publish","format-standard","hentry","category-geology","category-photos","tag-geology-images-accretionary-wedge"],"_links":{"self":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/3629","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\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/comments?post=3629"}],"version-history":[{"count":10,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/3629\/revisions"}],"predecessor-version":[{"id":3642,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/3629\/revisions\/3642"}],"wp:attachment":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/media?parent=3629"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/categories?post=3629"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/tags?post=3629"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}