In Stock
Fault Model (Diastrophism)
Multi-Part Segmented Block Design: Enables student-led manipulation of crustal blocks to simulate horizontal and vertical displacement, supporting the "Analyze" level of structural geology curricula.
High-Contrast Color-Coded Stratigraphy: Provides clear visual markers for measuring stratigraphic throw and heave, facilitating quantitative assessment in fault-geometry modules.
$5.08
Quick answer: This five-part Fault Model demonstrates normal, reverse, and transcurrent faulting, helping students visualize how tectonic displacement shifts rock layers along a fault line. Fault Model (Diastrophism) is priced at approximately ₹450 (indicative market benchmark, incl. GST, August 2026).
This five-part fault model set demonstrates different types of tectonic faulting — normal, reverse, and transcurrent (strike-slip) faults — showing how rock layers displace relative to each other along a fault line. Seeing these fault types as physical models helps students interpret crustal deformation and stratigraphic offset more concretely than from diagrams alone. Made from a durable polymer for repeated classroom handling, it’s suited to earth science and structural geology coursework at school and college level.
Technical Specifications
| Parameter | Detail |
|---|---|
| Product Type | 5-part fault (diastrophism) model set |
| Fault Types Covered | Normal, reverse, and transcurrent (strike-slip) |
| Function | Visualizing tectonic displacement and stratigraphic offset |
| Exact piece dimensions | Not independently verified for this listing — confirm with STEMAids before ordering |
| Curriculum/standard alignment | Not independently verified for this listing — confirm any specific standard alignment directly with STEMAids |
| Price | Approx. ₹450 (indicative market benchmark, incl. GST, August 2026) |
| Exact dimensions/technical detail | Not independently verified for this listing — confirm with STEMAids before specifying in a tender |
Applications
- Demonstrating normal, reverse, and transcurrent faulting
- Teaching tectonic displacement and stratigraphic offset concepts
- School and college earth science and structural geology coursework
- General classroom demonstration of crustal deformation
Care & Maintenance
- Handle carefully to protect the model’s structure and any moving parts
- Store the full five-part set together to avoid losing individual pieces
- Dust regularly with a soft brush or cloth
Why Choose STEMAids
STEMAids supplies a wide range of Educational Science Models including Globes, Illuminated for related classroom and laboratory needs. Eduscope Smart Learning Solutions Private Limited is a Udyam-registered micro manufacturing enterprise (UDYAM-DL-06-0069460) and ISO 9001:2015 certified, supplying schools, colleges and vocational institutes across India and for export.
Frequently Asked Questions
What fault types does this model demonstrate?
Normal, reverse, and transcurrent (strike-slip) faulting, shown as a five-part model set illustrating tectonic displacement.
What are the dimensions of each piece?
These have not been independently verified for this listing — confirm with STEMAids before ordering.
Is this set aligned with a specific curriculum standard?
No specific standard alignment has been independently verified for this listing — confirm directly with STEMAids before citing any compliance claim.
Is this suitable for a school earth science classroom?
Yes — fault demonstration models of this kind are standard teaching aids for structural geology coursework.
Does STEMAids supply other structural geology teaching models?
Contact STEMAids to confirm current availability of related earth science teaching aids.
Is STEMAids a registered manufacturer of this product?
Yes. Eduscope Smart Learning Solutions Private Limited is a Udyam-registered micro manufacturing enterprise (UDYAM-DL-06-0069460) and is ISO 9001:2015 certified. See the About page for full registration and certification details — manufacturer-stated, verify before citing in procurement documents.
Last updated: 29 August 2026.
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