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      "body": "@@ -138,17 +138,17 @@\n tigraphy\n-.\n+;\n  All of \n@@ -301,20 +301,8 @@\n for \n-getting and \n shar\n@@ -339,25 +339,20 @@\n ting\n-,\n+ but\n  I have \n-however \n been\n@@ -825,22 +825,16 @@\n ock. The\n-re are\n  three m\n@@ -847,16 +847,20 @@\n ck types\n+ are\n , *igneo\n@@ -900,11 +900,11 @@\n ary*\n-, t\n+. T\n hese\n@@ -1004,19 +1004,19 @@\n ous*\n- are\n  rocks \n+are \n form\n@@ -1180,16 +1180,39 @@\n ediments\n+ such as gravel or sand\n . Metamo\n@@ -1251,17 +1251,16 @@\n teration\n-,\n  without\n@@ -1282,17 +1282,16 @@\n melting)\n-,\n  of pre-\n@@ -1443,24 +1443,16 @@\n us rock \n-sourced \n from Mt.\n@@ -1534,15 +1534,16 @@\n nt l\n-ocation\n+ava flow\n s ar\n@@ -1580,235 +1580,172 @@\n ple \n-could be unique in its chemical signature through having a different magma so\n+will have a unique chemical signature. The chemical signat\n ur\n-c\n e \n-or difference in age of magma bodies. The samples could also show similar to the same chemical signat\n+will tell us if the lava flows come from a homogeneous magma so\n ur\n+c\n e \n-if each sample came from one homogeneous\n+or possibly from multiple isolated\n  mag\n@@ -1753,16 +1753,17 @@\n a source\n+s\n .%0ATo det\n@@ -1771,18 +1771,38 @@\n rmine th\n-is\n+e chemical composition\n  we will\n@@ -1866,66 +1866,38 @@\n s a \n-broad name for what is actually a mineral series, commonly\n+range of chemical compositions\n  kno\n@@ -2059,67 +2059,53 @@\n  or \n-the other or any composition in-between the two end-members\n+some ratio of the two depending on its source\n .%0ATh\n@@ -2174,18 +2174,16 @@\n ium. The\n-ir\n  names r\n@@ -2194,18 +2194,18 @@\n ctively \n-at\n+of\n  those e\n@@ -2361,111 +2361,109 @@\n 8*. \n-There is a solid solution between *anorthite* and *albite* and each unique composition has its\n+When composed of a ratio of the two end-members there are specific names depending\n  o\n-w\n n \n-name\n+percent content\n  as \n@@ -2475,23 +2475,22 @@\n  in the \n-diagram\n+figure\n  at the \n@@ -2603,16 +2603,54 @@\n e their \n+composition through measuring percent \n *anorthi\n@@ -2666,62 +2666,45 @@\n nt. \n-Pictured below is t\n+T\n he micro\n--\n probe \n-and on the screen is\n+is pictured below with\n  one\n@@ -2732,24 +2732,50 @@\n ** crystals \n+on the screen be prepared \n for analysis\n@@ -2949,17 +2949,18 @@\n ponents \n-a\n+we\n re cryst\n@@ -2982,44 +2982,8 @@\n oved\n- which changes the magma composition\n . So\n@@ -3645,20 +3645,16 @@\n haven't \n-yet \n had time\n",
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      "body": "I've been super busy with university this term, 17 credit hours that include physics, integral calculus, petrology, and sediment and stratigraphy. All of which have been keeping me indoors looking at rock samples or plugging and chugging equations in the undergrad lounge. This hasn't left much time for getting and sharing my experiences through posting, I have however been curating a little content each weekend that I will eventually get around to once the backlog is cleared.\nAll that aside last Friday I had the opportunity to use a **electron micro-probe** for a group project for my petrology class. Petrology is the branch of **geology** that is concerned with origin, small-scale structure, and composition of rocks. Basically classifying rocks on their mineral composition or percent compositions of parts that make up the whole rock. There are three main rock types, *igneous*, *metamorphic*, and *sedimentary*, these each have many different sub-groups, but ever rock falls under these three categories. *Igneous* are rocks formed by the cooling and solidification of lava(above ground) or magma(below ground). *Sedimentary* rocks are formed from the deposition and solidification of sediments. Metamorphic rocks are formed by the alteration, without liquification(melting), of pre-existing rocks through temperature, pressure, or chemical leeching or enrichment.\nFor our class project each group is analyzing a sample of igneous rock sourced from Mt. Jefferson in the Oregon Cascade range. The samples were taken from different locations around Mt. Jefferson so each sample could be unique in its chemical signature through having a different magma source or difference in age of magma bodies. The samples could also show similar to the same chemical signature if each sample came from one homogeneous magma source.\nTo determine this we will be analyzing **plagioclase** crystals. **Plagioclase** is a broad name for what is actually a mineral series, commonly known as the **plagioclase** feldspar series. This means there are two different chemical end-members and the **plagioclase** crystal could be composed of one or the other or any composition in-between the two end-members.\nThe end member chemicals for **plagioclase** are calcium and sodium. There names respectively at those end-members are *anorthite* and *albite*. Their chemical formulas are slightly different to stay balanced, *anorthite-CaAl2Si2O8* and *albite-NaAlSi3O8*. There is a solid solution between *anorthite* and *albite* and each unique composition has its own name as shown in the diagram at the bottom of the page.\nOur goal for the project is to analyze different crystals from our samples to determine their *anorthite* content. Pictured below is the micro-probe and on the screen is one of our **plagioclase** crystals for analysis. The photo doesn't show it but there are distinct color bands within the crystal showing a change in the magma composition ranging from *albite* to *anorthite* as components are crystallized and removed which changes the magma composition. So for our crystals we choose a point in the center of the crystal, A. Then we choose a point at the edge of the long axis, A'. The machine then blasts electrons at the sample at various points along the A-A' line. From the data *anorthite* composition can be found through calculating its weight%. \nhttps://steemitimages.com/DQmZ86yJsLnP8PWU2MkCpepr8pggdCxXUxELXwtcHRHDLh1/28161697_10212994741716914_7432386345400509609_o.jpg\n*Photo I took while picking sample points.*\n\nWe just started our projects so there isn't much to report yet other that background information and a little bit about our goals for the project. Our data was just posted today and we haven't yet had time to analyze or look at it but I'll post again as this project moves along through the rest of the term. Thanks for taking the time to read this, I appreciate it! \n**Science is badass!!!!!!**\nB\n\nSolid solution ternary diagram for **plagioclase** feldspar and alkali feldspar. The tips of the triangles signify 100% of that composition, 50% is directly between the triangle tips along the edge. Our project is solely looking at the **plagioclase** which is represented by the bottom of this triangle.\n![ternary diagram.jpg](https://steemitimages.com/DQmQMTfsNrSiUbZpyzYtTpHDwnJgRCwny41kwk4vV67NVBx/ternary%20diagram.jpg)\n*photo sourced from http://www.people.carleton.edu/~bhaileab/IntroductionToGeology/Minerals/Plagioclase/Plagioclase.dwt*",
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