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	<id>http://wiki.atlasleuven.be/index.php?action=history&amp;feed=atom&amp;title=Physical_Geography_Field_Trip_Abroad</id>
	<title>Physical Geography Field Trip Abroad - Bewerkingsoverzicht</title>
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	<updated>2026-05-05T16:39:31Z</updated>
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		<title>NikkeTamer op 24 jun 2025 om 14:18</title>
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		<updated>2025-06-24T14:18:54Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Oudere versie&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Versie van 24 jun 2025 16:18&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l10&quot;&gt;Regel 10:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Regel 10:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;= 2025: France =&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;= 2025: France =&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;You always got two questions from this set: (sorry, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;they&#039;re &lt;/del&gt;dutch, but i dont have the time or energy to translate them myself; google is your friend)&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;You always got two questions from this set: (sorry, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;some are &lt;/ins&gt;dutch, but i dont have the time or energy to translate them myself; google is your friend) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;There might be some doubles in here depending on who wrote it down and how well they remembered:&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Factoren die &lt;/del&gt;badlands &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;veroorzaken en hoe zou je ze stoppen. &lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;What are factors causing &lt;/ins&gt;badlands &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;formation? How would you stop badlands from eroding further?&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;morfologie van &lt;/del&gt;Ardèche &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;en welke processen&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;hoe geologie een invloed heeft based &lt;/del&gt;on &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;plan view / DEM en teken daar wat profielen bij&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Morphology of the &lt;/ins&gt;Ardèche&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&#039;s course: what processes&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;lithologies influence it? What types of valley forms do you encounter in different regions?&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flashfloods verschil &lt;/del&gt;in &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Ardèche en Allier en die dateren &lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;# Why is the Ardèche so susceptible to flash floods when compared to, for example, the Allier? How would you reconstruct historical floods &lt;/ins&gt;on &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;centennial and millennial timescales?&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;wat zich onder de vulkanische gesteenten bevind en hoe en van wanneer die daar komen&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;What type of material can you find under the volcanic rocks &lt;/ins&gt;in &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the different formations we saw?&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Name three different knickpoints we saw or whose influence we saw (doesnt need to exist anymore), discuss their formation and how you would estimate their retreat rate.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# What were the three monogenetic morphology types we saw and compre them in terms of composition, eruption type, and hazard&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# What were the three monogenetic morphology types we saw and compre them in terms of composition, eruption type, and hazard&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# You are a hazard risk manager on the ardeche what types of hazards are there and how would you assess the risk and how would you minimize it&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# You are a hazard risk manager on the ardeche what types of hazards are there and how would you assess the risk and how would you minimize it&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# 3 ways of lake forming a lake and where you can find them&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# 3 ways of lake forming a lake and where you can find them&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# different types of erutions &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ja en leg gwn basicly alles uit wa ge er van weet&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# different types of erutions &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;explain everything you know&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# Explain the meandering flow of the Ardèche, and the presence of its deep gorges around the Saint-Remeze plateau. Link this with the formation of caves.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# Explain the meandering flow of the Ardèche, and the presence of its deep gorges around the Saint-Remeze plateau. Link this with the formation of caves.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# Some deposits observed in the field were interpreted to result from phreato-magmatic eruptions. Describe what are the main characteristics of the deposit and the volcano morphology that can lead to that interpretation. Highlight how deposits from a phreato-magmatic eruption can vary within a single volcano and relate it to the evolution of the eruption dynamics.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# Some deposits observed in the field were interpreted to result from phreato-magmatic eruptions. Describe what are the main characteristics of the deposit and the volcano morphology that can lead to that interpretation. Highlight how deposits from a phreato-magmatic eruption can vary within a single volcano and relate it to the evolution of the eruption dynamics.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l28&quot;&gt;Regel 28:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Regel 29:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# bespreek op verschillende ruimtelijke schalen de typische vorm van het kalksteenplateau in saint remèze&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# bespreek op verschillende ruimtelijke schalen de typische vorm van het kalksteenplateau in saint remèze&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# Alle knickpoints die we hebben gezien (beke een curveball) - noem er 4&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;# Alle knickpoints die we hebben gezien (beke een curveball) - noem er 4&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;# De vulkanen in de Chaîne des Puys komen voort uit dezelfde magmaserie. Verklaar hoe deze serie is geëvolueerd om te zorgen voor de grote variëteit aan vulkanen in het gebied. Geef ook aan hoe deze evolutie mogelijk is. Leg vervolgens uit hoe het mogelijk is dat de verschillende types vulkanen net langs elkaar kunnen gevormd worden. Leg ook het verband uit tussen de invloed van de magmatische serie op het type uitbarsting. &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;# ... there&#039;s more but you get the idea right&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>NikkeTamer</name></author>
	</entry>
	<entry>
		<id>http://wiki.atlasleuven.be/index.php?title=Physical_Geography_Field_Trip_Abroad&amp;diff=849&amp;oldid=prev</id>
		<title>NikkeTamer: enkele vragen toegevoegd for future reference; het zouden er in totaal iets van 40 moeten zijn ma geen goesting mee</title>
		<link rel="alternate" type="text/html" href="http://wiki.atlasleuven.be/index.php?title=Physical_Geography_Field_Trip_Abroad&amp;diff=849&amp;oldid=prev"/>
		<updated>2025-06-20T09:59:40Z</updated>

		<summary type="html">&lt;p&gt;enkele vragen toegevoegd for future reference; het zouden er in totaal iets van 40 moeten zijn ma geen goesting mee&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Nieuwe pagina&lt;/b&gt;&lt;/p&gt;&lt;div&gt;The field trip has a three-yearly rotation, so different field trips take place to different regions with different professors. &lt;br /&gt;
&lt;br /&gt;
2025: prof. Kervyn, Massif Central/Chaine des Puys/Ardeche&lt;br /&gt;
&lt;br /&gt;
2024: prof. Vanmaercke, Moldavian Plateau / Eastern Romania&lt;br /&gt;
&lt;br /&gt;
2023: prof. Verstraeten, Spain&lt;br /&gt;
&lt;br /&gt;
The exam is oral; you get some preparation time for random questions. It is open book, so you get to take the excursion guide and the compiled notes.&lt;br /&gt;
&lt;br /&gt;
= 2025: France =&lt;br /&gt;
You always got two questions from this set: (sorry, they&amp;#039;re dutch, but i dont have the time or energy to translate them myself; google is your friend)&lt;br /&gt;
&lt;br /&gt;
# Factoren die badlands veroorzaken en hoe zou je ze stoppen. &lt;br /&gt;
# morfologie van Ardèche en welke processen/hoe geologie een invloed heeft based on plan view / DEM en teken daar wat profielen bij&lt;br /&gt;
# flashfloods verschil in Ardèche en Allier en die dateren &lt;br /&gt;
# wat zich onder de vulkanische gesteenten bevind en hoe en van wanneer die daar komen&lt;br /&gt;
# What were the three monogenetic morphology types we saw and compre them in terms of composition, eruption type, and hazard&lt;br /&gt;
# You are a hazard risk manager on the ardeche what types of hazards are there and how would you assess the risk and how would you minimize it&lt;br /&gt;
# 3 ways of lake forming a lake and where you can find them&lt;br /&gt;
# different types of erutions ja en leg gwn basicly alles uit wa ge er van weet&lt;br /&gt;
# Explain the meandering flow of the Ardèche, and the presence of its deep gorges around the Saint-Remeze plateau. Link this with the formation of caves.&lt;br /&gt;
# Some deposits observed in the field were interpreted to result from phreato-magmatic eruptions. Describe what are the main characteristics of the deposit and the volcano morphology that can lead to that interpretation. Highlight how deposits from a phreato-magmatic eruption can vary within a single volcano and relate it to the evolution of the eruption dynamics.&lt;br /&gt;
# Zet de volgende evenementen in chronologische volgorde. Geef voor elk aan wat de ruimtelijke omvang ervan is en hoe men deze kan dateren. &lt;br /&gt;
# The Chaîne des Puys and the Limagne fault became a UNESCO World heritage site in 2018, and the Chauvet cave in 2014. Explain what this means and what are the arguments that were put forward in these applications. Explain what challenges these sites are facing for their preservation and their touristic valorization. &lt;br /&gt;
# Waarom zijn de gorges in het Saint-Remeze plateau zo diep, hoe zijn ze gevormd en wanneer? Bespreek de verschillende fases.&lt;br /&gt;
# 2 stops bespreken die bewijs vormen voor uplift plioceen-pleistoceen en hoe we de rate van uplift daar konden bepalen&lt;br /&gt;
# bespreek op verschillende ruimtelijke schalen de typische vorm van het kalksteenplateau in saint remèze&lt;br /&gt;
# Alle knickpoints die we hebben gezien (beke een curveball) - noem er 4&lt;/div&gt;</summary>
		<author><name>NikkeTamer</name></author>
	</entry>
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