Impact Feature Types

In general, three different types of impacts can be distinguished for experiment surfaces from A0201 MOS detectors and Germanium witness plates, A0187-1 Gold surfaces, and S1003 Aluminum surfaces:

Impact craters on metal surfaces

These features have elliptic impact craters with raised lips, sometimes accompanied with a small spall zone near the lips. Spallation was seen on on the gold surfaces from A0187-1, due to the manufacturing process which utilized a thin (approximately 2 micrometer) beat to cover the base Au substrate. This resulted in a layered structure.

Central craters were usually near-circular shaped, although some features on the S1003 Aluminum surfaces are clearly elongated Diameter measurements were taken as described in the M & D preliminary report, page 8:
"(...)In practice, the microscope was focused on the top of the feature's rim, and the center of the ridge which was in focus was used to make the estimated diameter measurements(...)."
Be aware that diameter measurements reported in some hypervelocity impact related literature might have been taken as diameter of the central crater at the level of the undisturbed surface.

Impact induced discharges on MOS detectors

These discharge features have a central crater and a larger discharge zone. Note that the term crater might be confusing as the central crater of the discharge feature is related to particle parameters in a different manner than is the case with "standard" hypervelocity impacts. All Particles < 3 micrometers in size that "triggered" the MOS sensors resulted in approximately 10 micrometer "craters" i the senter of the discharge zone. The formation mechanism of these 10 micrometer craters was dominated by the sensor's spark discharge energy. For particles >3 micrometers, the impact crater formation mechanism is dominated be the impactor's energyand resemble "classic" impacts into brittle materials.

(See also the calibration paper, in this archive).

Measurements for these sensors were taken as follows:

Hypervelocity impacts craters with spall and fracture zones

These impacts feature a central crater or central zone of damage, depending on feature size, associated with a large spallation zone.

Measurements for these fetures were taken as follows:

Notes:
Klaus G. Paul, 06-20-94