Naomi nodded.
"I won't."
Claire continued.
"Also, your measurements are useful. Keep recording from safe locations."
Naomi smiled faintly.
"That's the one thing I know how to do."
Claire arrived with a field technician and a survey specialist.
They didn't walk directly to the water.
Instead, they reviewed the available records, inspected the broader landscape, and established safe locations from which to observe the pond.
Naomi watched them work.
For the first time since returning to the farm, she felt as though someone was approaching the problem with the same seriousness she had.
Claire examined the shoreline data.
Then compared it with rainfall information and the visible subsidence.
The pattern troubled her.
She explained that the pond's expansion could result from more than one interacting process.
Additional groundwater input might increase the water level.
Erosion beneath the bank could allow the ground to settle.
And a damaged underground structure could alter both water movement and soil stability.
Those processes weren't mutually exclusive.
In fact, they sometimes made one another worse.
Claire looked toward the cracked crescent.
Then toward the pond.
"Something is changing below the surface."
Naomi nodded.
"That's what I've been trying to tell everybody."
The engineer smiled slightly.
"I believe your observations. We still need to establish the mechanism."
She pointed toward the bank.
"The dangerous part is that the visible crack may not show the full extent of unstable ground."
Naomi looked toward the water.
For a moment, she remembered Otis's boot sinking into the mud.
Claire continued.
"The safest approach is to keep that area isolated until the underlying conditions are evaluated."
Naomi agreed.
Then the engineer asked whether the old waterworks had a connection to the quarry.
Naomi showed her the historic map.
Claire studied it for several minutes.
Then looked toward the distant northern ridge.
For a moment, she seemed concerned.
"That corridor needs to be investigated."
The initial sampling results arrived several days later.
Claire's team found that the pond's water chemistry differed from what they would have expected if it were receiving only its historically documented spring flow and ordinary surface runoff.
The differences weren't enough to identify a single source conclusively.
Groundwater chemistry could vary.
Sediment could affect certain measurements.
And older drainage structures could introduce complications.
But the results justified further examination.