Learning target: I can use cross-cutting relationships in a trench log to decide whether a fault has moved recently, evaluate three building plans against criteria and constraints, and justify a recommendation.
Read the problem, the criteria and constraints, and the trench log. Part A asks you to decide, from the trench, whether the fault counts as active. Part B asks you to evaluate three site plans with a scoring matrix and choose one. Part C asks for a site plan sketch and a justification written for the school board, who are not scientists. Everything you need is on this sheet; the school, the lot and the trench are invented, but the law and the method are real.
You will need: This worksheet, Pencil, Ruler, Colored pencil for the setback band
Alder Creek Middle School (invented) wants to build a new gym on an empty lot east of the main building. The lot is 120 m long from west to east and 60 m wide from north to south; the main building stands along the lot's west edge. A state map shows a fault trace crossing the lot from north to south, about 45 m from the west edge, but the map is only accurate to about 10 m either way. California's Alquist-Priolo Earthquake Fault Zoning Act does not allow a building for people to sit on top of an active fault, meaning one that has moved in roughly the last 11,700 years. The usual rule is a setback of 15 m (50 feet) on each side of an active fault trace. To find out whether the fault is active and exactly where it runs, the district dug a trench across the lot and logged the layers in its wall.
| Layer | Depth below surface (m) | Material | Age of charcoal in the layer | Broken by the fault? |
|---|---|---|---|---|
| 1 | 0 to 0.4 | Dark topsoil | none found | No; runs across unbroken |
| 2 | 0.4 to 1.2 | Tan silt | about 2,500 years | No; runs across unbroken |
| 3 | 1.2 to 2.0 | Gravel | about 9,000 years | Yes; offset 0.3 m |
| 4 | 2.0 to 3.5 | Gray clay | about 18,000 years | Yes; offset 0.9 m |
| 5 | 3.5 to 5.0 | Brown sand | none found | Yes; offset 0.9 m |
| Plan | Gym position and orientation | Nearest gym wall to the fault (at 52 m) | Walk from main building | Estimated cost | Notes |
|---|---|---|---|---|---|
| 1 | Centered on the lot, long side west-east: 40 m to 80 m | 0 m (the fault runs under the gym) | 40 m | 5.1 million dollars | Flat ground; shortest utility lines |
| 2 | East side, long side west-east: 70 m to 110 m | 18 m | 70 m | 5.3 million dollars | Flat ground; needs a longer path and utility line |
| 3 | West side, turned so the short side faces west-east: 5 m to 30 m | 22 m | 5 m | 5.9 million dollars | Ground slopes; needs cutting and filling before building |
| Criterion | Plan 1 | Plan 2 | Plan 3 |
|---|---|---|---|
| 1. At least 15 m from the fault on every side | |||
| 2. Walk under 100 m | |||
| 3. Lowest cost | |||
| Any constraint broken? (X) | |||
| Total |
The trench wall is a tiny version of the road cuts in this chapter. The rule is the same: a fault is younger than every layer it breaks and older than every layer that lies across it unbroken. Mark each row of the log with B (broken) or U (unbroken). The last movement happened after the youngest B layer formed and before the oldest U layer formed. For the matrix, do criterion 1 first; any plan that fails it is out, whatever its other scores.
The trench shows the fault last moved between about 9,000 and 2,500 years ago, a window of 6,500 years. Describe what a geologist could look for in a deeper or longer trench to narrow that window (think about finding and dating a layer between layers 2 and 3, or a thin layer that is broken by only a tiny amount). Then explain why the district would care whether the last movement was 8,900 years ago or 2,600 years ago, even though both count as active.