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Smithsonian at the Poles: Contributions to International Polar

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<strong>the</strong> description and cur<strong>at</strong>ion of Antarctic meteorites fell<br />

<strong>to</strong> Roy S. Clarke Jr., whose specialty in <strong>the</strong> metallography<br />

of iron meteorites and oversight of <strong>the</strong> non-Antarctic<br />

collection made him an ideal choice. While all meteorites<br />

are classifi ed, <strong>the</strong> <strong>Smithsonian</strong>’s major task is identifying<br />

those specimens th<strong>at</strong> are of particular interest <strong>to</strong> scientists<br />

and th<strong>at</strong> would be worthy of fur<strong>the</strong>r study. Figure 3<br />

illustr<strong>at</strong>es <strong>the</strong> results of <strong>the</strong>se efforts, indic<strong>at</strong>ing <strong>the</strong> number<br />

of samples recovered, <strong>the</strong> <strong>to</strong>tal number of meteorites,<br />

and <strong>the</strong> subset of meteorites th<strong>at</strong> are not equilibr<strong>at</strong>ed ordinary<br />

chondrites. The number of meteorites recovered<br />

increased steadily from an average of �300 (1977– 1984)<br />

<strong>to</strong> gre<strong>at</strong>er than 1,000 per year (2002– 2006) as collecting<br />

techniques improved and fi eld parties grew in size and<br />

number. The number of samples was sometimes gre<strong>at</strong>er<br />

than <strong>the</strong> number of meteorites due <strong>to</strong> <strong>the</strong> collection of<br />

a small number of terrestrial rocks mistaken for meteorites.<br />

The number of <strong>the</strong> most scientifi cally interesting<br />

specimens, those o<strong>the</strong>r than equilibr<strong>at</strong>ed ordinary chondrites<br />

(e.g., unequilibr<strong>at</strong>ed ordinary chondrites, carbona-<br />

U.S. ANTARCTIC METEORITE PROGRAM 391<br />

ceous and enst<strong>at</strong>ite chondrites, achondrites, and irons),<br />

remained constant <strong>at</strong> �50/year. (The sharp dip in 1989<br />

was due <strong>to</strong> a cancelled fi eld season.) The apparent disconnect<br />

between <strong>the</strong> number collected and those of gre<strong>at</strong>est<br />

scientifi c interest is due <strong>to</strong> <strong>the</strong> occurrence of meteorites<br />

th<strong>at</strong> break up in <strong>the</strong> <strong>at</strong>mosphere and possibly shower local<br />

areas with thousands of individual fragments. While<br />

most scientifi c studies focus on <strong>the</strong> small subset of <strong>the</strong><br />

most interesting specimens, <strong>the</strong> collection as a whole still<br />

offers clues <strong>to</strong> ice movements rel<strong>at</strong>ed <strong>to</strong> concentr<strong>at</strong>ion<br />

mechanism and <strong>the</strong> infl ux of meteoritic m<strong>at</strong>erial <strong>to</strong> Earth<br />

over time (Harvey, 2003). Only through system<strong>at</strong>ic collection<br />

and classifi c<strong>at</strong>ion of all <strong>the</strong> meteorites can <strong>the</strong>se<br />

l<strong>at</strong>ter studies be undertaken.<br />

The o<strong>the</strong>r major oblig<strong>at</strong>ion of <strong>the</strong> SI in <strong>the</strong> U.S. Antarctic<br />

Meteorite Program was serving as <strong>the</strong> long-term cur<strong>at</strong>orial<br />

facility for specimens (Figure 4). In 1983, <strong>the</strong> SI<br />

opened its Museum Support Center in Suitland, Maryland.<br />

This st<strong>at</strong>e-of-<strong>the</strong>-art collections facility is centered on four<br />

pods (football-fi eld-sized buildings �50 feet (�15 m) high)<br />

FIGURE 3. The number of samples and recovered meteorites and those meteorites th<strong>at</strong> are not equilibr<strong>at</strong>ed ordinary chondrites (EOCs) from<br />

1977 <strong>to</strong> 2007.

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