<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-561941599923340931</id><updated>2012-02-16T17:47:39.752-05:00</updated><title type='text'>The Marcellus Clay Experiment</title><subtitle type='html'>a quest to make ceramic clay from Marcellus Shale</subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://marcellusclay.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/561941599923340931/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://marcellusclay.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>JS</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>2</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-561941599923340931.post-5113800200067401911</id><published>2011-09-26T19:24:00.001-04:00</published><updated>2011-10-21T22:51:09.755-04:00</updated><title type='text'>Intro: Why?</title><content type='html'>&lt;span class="Apple-style-span" style="font-family: Arial, Helvetica, sans-serif;"&gt;Though I'm a resident of Pennsylvania, it wasn't until I started working on &lt;a href="http://www.catskillcenterpieces.blogspot.com/"&gt;a project in the Catskills&lt;/a&gt;&amp;nbsp;that the practice of&amp;nbsp;fracking became a common topic. &amp;nbsp;The part of the Catskills where we are working is full of shale. It wasn't clear what type it was, leaving me to wonder: is &lt;i&gt;that&lt;/i&gt;&amp;nbsp;the Marcellus? What is this stuff? Is it safe? What makes Marcellus so different from other rock formations?&amp;nbsp;&lt;/span&gt;&lt;br /&gt;&lt;div&gt;&lt;span class="Apple-style-span" style="font-family: Arial, Helvetica, sans-serif;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span class="Apple-style-span" style="font-family: Arial, Helvetica, sans-serif;"&gt;Dusty red and pink shale-bed roads and driveways are common in that part of Sullivan County. Outcroppings line the highways. &amp;nbsp;After one particularly wet week, I recognized that the fine creamy silt settling in puddles and along the roadside was clay. Shale, I learned, makes excellent clay.&amp;nbsp;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span class="Apple-style-span" style="font-family: Arial, Helvetica, sans-serif;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span class="Apple-style-span" style="font-family: Arial, Helvetica, sans-serif;"&gt;Questions resurfaced and I still had no answers. &amp;nbsp;Is this Marcellus? Is it hazardous to use? How do you made into a usable ceramic clay? Would the final product be foodsafe? What could I make with it?&amp;nbsp;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span class="Apple-style-span" style="font-family: Arial, Helvetica, sans-serif;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span class="Apple-style-span" style="font-family: Arial, Helvetica, sans-serif;"&gt;This site documents the experiments, information, stories and lessons I've learned through this ongoing investigation into the use of Marcellus Shale as a material.&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/561941599923340931-5113800200067401911?l=marcellusclay.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://marcellusclay.blogspot.com/feeds/5113800200067401911/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://marcellusclay.blogspot.com/2011/09/why.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/561941599923340931/posts/default/5113800200067401911'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/561941599923340931/posts/default/5113800200067401911'/><link rel='alternate' type='text/html' href='http://marcellusclay.blogspot.com/2011/09/why.html' title='Intro: Why?'/><author><name>JS</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-561941599923340931.post-7293601914398594410</id><published>2011-09-25T20:04:00.001-04:00</published><updated>2011-09-26T16:32:40.351-04:00</updated><title type='text'>Chapter 1: Catskill Red Shale</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: justify;"&gt;This is typical of the part of Fallsburg I've been working in for the past year.&amp;nbsp;Roads and driveways often sit directly on top of the bedrock stone.&amp;nbsp;&lt;/div&gt;&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/-DnXiLCowN6c/Tn-qNBN6xGI/AAAAAAAADNE/8Zoe1vMVXUc/s1600/Untitled-1.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="640" src="http://3.bp.blogspot.com/-DnXiLCowN6c/Tn-qNBN6xGI/AAAAAAAADNE/8Zoe1vMVXUc/s640/Untitled-1.jpg" width="535" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;/div&gt;&lt;br /&gt;&lt;div style="text-align: center;"&gt;The most common rock types in the area are bluestone and a reddish shale. &amp;nbsp;&lt;/div&gt;&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/-UdfqmroLEfU/Tn-sw_9-FeI/AAAAAAAADNg/Ov-Ho1US2kA/s1600/IMG_7724.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="640" src="http://2.bp.blogspot.com/-UdfqmroLEfU/Tn-sw_9-FeI/AAAAAAAADNg/Ov-Ho1US2kA/s640/IMG_7724.jpg" width="478" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;When side-by-side, the blue sandstone takes on a bright green.&lt;br /&gt;&lt;br /&gt;&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/-9_bBUt-KfMo/Tn-9qIVBGlI/AAAAAAAADNw/XvYcFS-OyMw/s1600/Untitled-2.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="246" src="http://3.bp.blogspot.com/-9_bBUt-KfMo/Tn-9qIVBGlI/AAAAAAAADNw/XvYcFS-OyMw/s400/Untitled-2.jpg" width="400" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;The shale - it's violet, pink, maroon, brick, brown and orange.&lt;br /&gt;&lt;a href="http://3.bp.blogspot.com/-BDDSiDGfob0/Tn-qd0nieBI/AAAAAAAADNQ/DWI54n-_Z1A/s1600/shale.jpg" imageanchor="1" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="451" src="http://3.bp.blogspot.com/-BDDSiDGfob0/Tn-qd0nieBI/AAAAAAAADNQ/DWI54n-_Z1A/s640/shale.jpg" width="640" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;div class="separator" style="clear: both; text-align: center;"&gt;Puddles after a storm are blood red. As they evaporate, a dark red clay silt remains.&lt;/div&gt;&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/-7XZGpFU7X68/Tn-qaC5spkI/AAAAAAAADNM/nA5WgBKIMAQ/s1600/IMG_7721a.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="300" src="http://4.bp.blogspot.com/-7XZGpFU7X68/Tn-qaC5spkI/AAAAAAAADNM/nA5WgBKIMAQ/s400/IMG_7721a.jpg" width="400" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div class="separator" style="clear: both; text-align: justify;"&gt;Shale = silt stone. These puddles were the prime places to hunt for clay. It was a frustrating process - there just were too few puddles. Instead,&amp;nbsp;I decided to try to refine&amp;nbsp;mud collected by red shale outcrops . Three 5-gallon buckets of mud traveled back to Philly with me.&amp;nbsp;&lt;/div&gt;&lt;div class="separator" style="clear: both; text-align: left;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div class="separator" style="clear: both; text-align: left;"&gt;This was the beginning. The next step: refining. &amp;nbsp;&lt;/div&gt;&lt;div&gt;&lt;br /&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/561941599923340931-7293601914398594410?l=marcellusclay.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://marcellusclay.blogspot.com/feeds/7293601914398594410/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://marcellusclay.blogspot.com/2011/09/chapter-1-catskill-red-shale_25.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/561941599923340931/posts/default/7293601914398594410'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/561941599923340931/posts/default/7293601914398594410'/><link rel='alternate' type='text/html' href='http://marcellusclay.blogspot.com/2011/09/chapter-1-catskill-red-shale_25.html' title='Chapter 1: Catskill Red Shale'/><author><name>JS</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/-DnXiLCowN6c/Tn-qNBN6xGI/AAAAAAAADNE/8Zoe1vMVXUc/s72-c/Untitled-1.jpg' height='72' width='72'/><thr:total>0</thr:total></entry></feed>
