Lava is molten rock that erupts from a volcano or fissure in the Earth'scrust. It is a type of magma that reaches the surface and flows out as a liquid before solidifying.
Basaltic Lava: This type of lava is low in viscosity and flows easily. It often forms extensive lava flows and can travel long distances from the volcanic vent.
Andesitic Lava: Andesitic lava has higher viscosity than basaltic lava and may form domes and short, thick flows.
Rhyolitic Lava: Rhyolitic lava is the most viscous type and tends to form thick, short flows and lava domes.
How does the composition of lava vary among different types, such as basaltic, andesitic, and rhyolitic lava?
What are the primary factors that influence the viscosity of lava?
What are the potential hazards associated with lava flows?
How do lava tubes form, and what are their significance?
Additionally, it can be helpful to study specific examples of volcanic eruptions and their associated lava flows, as well as the geological features formed by lava, such as volcanic cones and lava plateaus.
Earth/Space Science: Students will use scientific skills and processes to explain the chemical and physical interactions (i.e., natural forces and cycles, transfer of energy) of the environment, Earth, and the universe that occur over time.
Earth History: Explain how sedimentary rock is formed periodically, embedding plant and animal remains and leaving a record of the sequence in which the plants and animals appeared and disappeared.
Explain how sedimentary rock buried deep enough may be reformed by pressure and heat and these reformed rock layers may be forced up again to become land surface and even mountains.
Explain why some fossils found in the top layers of sedimentary rock are older then those found beneath in lower layers: Folding; Breaking; Uplift; Faulting; Tilting.