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Fill in the PURPLE TEXT BOXES with the type of plate boundary shown (Convergent, Divergent, Transform). These will be used more than once on the two slides. Fill in the RED TEXT BOXES with the associate landforms (volcanoes, trench, mid ocean ridge, rift valley, mountains) Some of these may be used more than once between the two slides. Fill in the ORANGE TEXT BOXES with what is going on below the surface (subduction zone, convection current, earthquake)

Ask by May Gibson. in the United States
Jan 18,2025

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Fill in the **Purple** boxes with the types of plate boundaries: **Convergent**, **Divergent**, and **Transform**. In the **Red** boxes, write the associated landforms: **Volcanoes**, **Trench**, **Mountains**, **Mid-Ocean Ridge**, and **Rift Valley**. In the **Orange** boxes, note the subsurface activities: **Subduction Zone**, **Convection Current**, and **Earthquake**.

Solución

Sure, I can help you organize the information for your slides. Below is a structured guide to fill in the **PURPLE**, **RED**, and **ORANGE** text boxes based on the type of plate boundaries, their associated landforms, and subsurface activities. --- ### **Plate Boundary Types (PURPLE TEXT BOXES)** 1. **Convergent Boundary** 2. **Divergent Boundary** 3. **Transform Boundary** --- ### **Associated Landforms (RED TEXT BOXES)** - **Volcanoes** *(Typically associated with Convergent Boundaries)* - **Trench** *(Typically associated with Convergent Boundaries)* - **Mountains** *(Typically associated with Convergent Boundaries)* - **Mid-Ocean Ridge** *(Typically associated with Divergent Boundaries)* - **Rift Valley** *(Typically associated with Divergent Boundaries)* *Note:* While most Transform Boundaries are characterized primarily by earthquakes, if needed, you can mention **Linear Valleys** or **Fault Scarps** as minor landforms. --- ### **Subsurface Activities (ORANGE TEXT BOXES)** - **Subduction Zone** *(Occurs at Convergent Boundaries)* - **Convection Current** *(Drives the movement at Divergent Boundaries)* - **Earthquake** *(Occurs at both Convergent and Transform Boundaries)* --- ### **Summary Table** | **Plate Boundary (Purple)** | **Associated Landforms (Red)** | **Subsurface Activities (Orange)** | |-----------------------------|-------------------------------------------|------------------------------------| | **Convergent** | Volcanoes, Trench, Mountains | Subduction Zone, Earthquake | | **Divergent** | Mid-Ocean Ridge, Rift Valley | Convection Current | | **Transform** | *Earthquakes (or Linear Valleys/Fault Scarps)* | Earthquake | --- ### **Usage Across Slides** - **Slide 1:** - **Purple Box:** Convergent Boundary - **Red Box:** Volcanoes - **Orange Box:** Subduction Zone - **Slide 2:** - **Purple Box:** Divergent Boundary - **Red Box:** Mid-Ocean Ridge - **Orange Box:** Convection Current - *(You can repeat or rearrange these as needed for consistency and emphasis across both slides.)* --- ### **Additional Notes** - **Convergent Boundaries** are where two tectonic plates move towards each other, leading to the formation of mountains, trenches, and volcanic activity due to subduction. - **Divergent Boundaries** occur where tectonic plates move apart from each other, resulting in the creation of new crust as magma rises, forming mid-ocean ridges and rift valleys. - **Transform Boundaries** involve plates sliding past one another horizontally, which primarily causes earthquakes due to the friction and stress accumulation. --- Feel free to adjust the placement of these elements based on the specific layout and design of your slides. Let me know if you need further assistance!

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If you're diving into the world of plate tectonics, it’s super important to understand how these boundaries interact to shape our planet. At convergent boundaries, you’ll often find rugged mountains or deep ocean trenches as one plate dives beneath another in a dramatic showdown! Meanwhile, divergent boundaries give birth to mid-ocean ridges and rift valleys because the plates pull apart, allowing magma to ooze up and create new crust. When it comes to what's brewing beneath the surface, subduction zones and convection currents create some of the most exciting geological action! Subduction zones form at convergent boundaries, leading to intense pressure and the potential for powerful earthquakes. On the flip side, convection currents in the mantle are continually moving the plates around like a giant game of cosmic bumper cars—leading to even more geological wonders above ground!

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