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For stable areas (such as nonglacial surfaces), vertical differences were detected between the two point clouds (RMS M3C2 vertical difference of 8.5 m), with the outwash zones adjacent to the assessed glacier termini showing less extensive vertical discrepancies (94% of M3C2 vertical differences between ± 5 m).
This result is attributed to the structural stability and the Coulombic force between the two point defects.
After the appearance of flexural cracks in the maximum moment region, by increasing the load, new flexural cracks were formed between the two point loads.
But the difference between the two point estimates is mostly less than 10 percentage points for M4+, which is small in relation to the width of the confidence set.
We performed six successful demonstrations of this method using a basalt thin section and found a standard deviation of ~0.1 mm for a distance (x 59.9 mm, y 24.2 mm) between the two point sources.
The positioning errors between the two point sets (DR and CT) are found to be approximately ≤0.1 mm, which is consistent with the validation of the derived setup geometry above.
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Mr. Alpert himself wavers between the two points of view.
The length of the geodesic curve defines the distance between the two points in.
That would be misleading; the journey between the two points is rich in surprises.
What we end up doing is inferring what's going on between the two points.
If V G > V A, as shown in this example, information cannot travel between the two points.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com