1![Fluctuations of GlaciersVol. VIII) Fluctuations of GlaciersVol. VIII)](https://www.pdfsearch.io/img/f0315f3c8e7cc5364d054ce4e46eb196.jpg) | Add to Reading ListSource URL: wgms.chLanguage: English - Date: 2015-07-15 08:56:22
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2![STANDING AT THE SOUTH POLE Detailed Itinerary A JOURNEY BY FLIGHT Experience the ultimate destination - the South STANDING AT THE SOUTH POLE Detailed Itinerary A JOURNEY BY FLIGHT Experience the ultimate destination - the South](https://www.pdfsearch.io/img/85ccbd989887af46d64c92e93fa1e6b3.jpg) | Add to Reading ListSource URL: www.eldertreks.comLanguage: English - Date: 2015-02-23 16:35:21
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3![](https://www.pdfsearch.io/img/af9c67f543a9a06a9c1a6c0c7d0b787d.jpg) | Add to Reading ListSource URL: antarcticanz.govt.nzLanguage: English - Date: 2013-08-06 00:53:12
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4![](https://www.pdfsearch.io/img/3dff63e68fc1330a0e25dce8f17ca3db.jpg) | Add to Reading ListSource URL: antarcticanz.govt.nzLanguage: English - Date: 2013-08-06 00:53:12
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5![Granitic rocks were systematically collected on the traverse down Scott Glacier for later chemical analysis. In the Gothic Mountains a roof pendant of porphyry similar to the Wyatt Formation was visited and the granitic Granitic rocks were systematically collected on the traverse down Scott Glacier for later chemical analysis. In the Gothic Mountains a roof pendant of porphyry similar to the Wyatt Formation was visited and the granitic](https://www.pdfsearch.io/img/c815e6ba81f3b59e3ee1d8e715d40376.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 06:15:19
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6![Figure 1. Exposure of Unit Rg, showing meter-thick black glass layers interleaved with crystalline rhyolite. Lighter colored rock bordering the black glass is composed of devitrified glass. Figure 2. Cliff face exposure Figure 1. Exposure of Unit Rg, showing meter-thick black glass layers interleaved with crystalline rhyolite. Lighter colored rock bordering the black glass is composed of devitrified glass. Figure 2. Cliff face exposure](https://www.pdfsearch.io/img/e17acd27f6aba6da2e3153d64c197d55.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 06:15:09
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7![drilling platform (Kuivinen, Antarctic Journal, this issue). Equipment for ice core processing and analyses was installed in the science trench. Stauffer and Schwander (Antarctic Journal, this issue) describe the core pr drilling platform (Kuivinen, Antarctic Journal, this issue). Equipment for ice core processing and analyses was installed in the science trench. Stauffer and Schwander (Antarctic Journal, this issue) describe the core pr](https://www.pdfsearch.io/img/7384932bb3ea9cd86affe5eb17351cf9.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 05:01:26
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8![much lower levels than the outcrops along Touchdown Glacier. As the survey was extended south of the head of Byrd Glacier into the area of the Sefton and Zeller glaciers, a complex series of low-grade metamorphic rocks w much lower levels than the outcrops along Touchdown Glacier. As the survey was extended south of the head of Byrd Glacier into the area of the Sefton and Zeller glaciers, a complex series of low-grade metamorphic rocks w](https://www.pdfsearch.io/img/0948874ca7da73d9c7fc99ed8a67c21a.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 03:37:40
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9![Study of grounding-line sedimentation processes at the Mackay Glacier tongue using a remotely operated vehicle Observations on the seafloor epibenthic community MICHAEL DAwBER and Ross D. POwELL, Department of Geology, Study of grounding-line sedimentation processes at the Mackay Glacier tongue using a remotely operated vehicle Observations on the seafloor epibenthic community MICHAEL DAwBER and Ross D. POwELL, Department of Geology,](https://www.pdfsearch.io/img/b1854d13ed40d4015e93c7d3e2ac68dd.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 17:41:00
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10![in the late winter or early spring. However, the actual mechanisms of storage and release of saline water are likely to be affected by glaciological and climatic variations which are poorly known. Special thanks are due in the late winter or early spring. However, the actual mechanisms of storage and release of saline water are likely to be affected by glaciological and climatic variations which are poorly known. Special thanks are due](https://www.pdfsearch.io/img/4de2aba5ce35622f77288cec8ef0c626.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 03:40:42
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