Triple
T8712630
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | George Biddell Airy |
E206813
|
entity |
| Predicate | notableWork |
P4
|
FINISHED |
| Object |
Airy isostasy model in geophysics
The Airy isostasy model in geophysics is a theory proposing that variations in topographic height are supported by corresponding differences in crustal thickness, with higher regions underlain by deeper, less dense “roots” floating in gravitational balance on the denser mantle.
|
E753776
|
NE FINISHED |
Provenance (5 batches)
| Stage | Batch ID | Job type | Status |
|---|---|---|---|
| creating | batch_69ca83572d4881909bef3be2b578d539 |
elicitation | completed |
| NER | batch_69cc5c32aebc8190ba19299ce9a18efd |
ner | completed |
| NED1 | batch_69cf28cd239c81909d1feb98b652eb26 |
ned_source_triple | completed |
| NED2 | batch_69cf2cb3c4308190971fb3d25064f205 |
ned_description | completed |
| NEDg | batch_69cf2bd14c3c8190b43840ee57cca22c |
nedg | completed |
Created at: March 30, 2026, 6:35 p.m.