======Gelatin Volcano Model====== **Materials: **{{$demo.materials_description}}\\ **Difficulty: **{{$demo.difficulty_description}}\\ **Safety: **{{$demo.safety_description}}\\ \\ **Categories:** {{$demo.categories}} \\ **Alternative titles:** Edible Magma Injection, Single-Serving Volcanism ====Summary==== {{$demo.summary}} ====Procedure==== - Refrigerate gelatin cups until cool and firm. - Use a pushpin and small knife to create a hole in the bottom of the cup, just wide enough for the syringe tip. - Fill a plastic syringe with pudding, yogurt, or chocolate sauce, removing excess air. - Insert the syringe into the hole at the base of the cup. - Put on goggles and remove the gelatin cup’s cover. - Slowly inject the “magma” into the gelatin, observing as it intrudes and spreads inside. - Continue injecting until the magma breaks through the surface, simulating a volcanic eruption. - Remove the syringe, place the cup on a plate, and excavate with a spoon while eating, noting “sills,” “dikes,” and inclusions. ====Links==== Gelatin Volcano—classroom demonstration [educational] - IRIS Earthquake Science: {{youtube>EmGl5fakHoY?}}\\ STEAM Fun: Gelatin Volcano - Wood Dale Public Library District: {{youtube>wWp0-uwTBi8?}}\\ 📄 Single-Serving Volcanism - Exploratorium: [[https://www.exploratorium.edu/snacks/single-serving-volcanism]]\\ ====Variations==== * Use layered gelatin to simulate rock strata. * Inject multiple types of sauces to model successive magma intrusions. * Chill or warm the sauce to see how viscosity affects intrusion and eruption. ====Safety Precautions==== * Wear goggles to protect eyes from splashes. * Use caution with sharp tools when piercing the gelatin cup. * Keep tools and utensils clean, since the activity ends with edible food. ====Questions to Consider==== * How is the gelatin like country rock and the sauce like magma? (The gelatin is pre-existing rock, and the sauce represents molten rock intruding into it.) * What geological features do the blobs, layers, and cracks of sauce represent? (Plutons, sills, dikes, xenoliths.) * What changes when the “magma” erupts at the surface? (It transitions from magma to lava, modeling extrusive volcanism.) * In what ways is this model similar to real volcanism, and in what ways is it different? (Similar in showing intrusion and eruption; different in scale, time, pressure, and material behavior.)