Wild Ride No More

Contributed by John Bergman-McCool

Cups and Coaster
The collections environment before and after rehousing in archival boxes

Back in March I wrote a blog post summarizing efforts to rid collections objects of mold and salt uncovered during inventory and rehousing. We identified and isolated affected objects and cleaned them by dry brushing and vacuuming. The cleaned objects were rehoused in archival boxes that included a sachet of silica gel. The purpose of the gel is to reduce relative humidity (RH), thereby robbing mold and salt of the environmental conditions necessary for their growth. To better understand what the environment is like inside the boxes, we are monitoring their temperature and relative humidity with two data loggers. One is placed inside a box without silica gel and one is placed inside a box with silica gel. These conditions will be compared against a data logger that is recording general conditions in the basement not far from where these test boxes are located. We will be watching these data loggers over the coming year, but we already have some interesting results.

Temp and RH graph for John August 2019
Environmental Stats for April

First, the boxes are working well as a buffer against relative humidity cycles. The graph above shows RH and temperature for the month of April; the basement is shown in red and the boxes with and without silica are blue and yellow, respectively. In April the RH in the basement was quite volatile. However, the RH inside the boxes is remarkably tranquil in comparison. The boxes are exhibiting small daily shifts of 1 or 2%, which is acceptable. Keeping RH from shifting dramatically is an important factor in collections care. Organic materials such as basketry, bone, and wood are hygroscopic, meaning that they can absorb and release moisture in the air. Rapid and large changes in RH can cause organic materials to swell and contract leading to damage such as cracking or delamination. It is best to keep collections from experiencing RH shifts exceeding 10% over a given month and on that count the boxes are doing a great job. As they are found, the most sensitive organic collections are being moved to another part of the museum that has a better environment.

Layerd Storage
Layered Storage

The National Park Service recommends creating a layered approach to collections storage. Every enclosure within museum storage can act as an environmental buffer. The first enclosure is the building itself. It may seem pretty obvious, but keeping collections inside a building greatly reduces the effects of environmental factors. The same is true of every subsequent layer of enclosed storage. Here at the Peabody Institute we have wooden storage bays that, when closed, serve as another layer. The archival boxes act as a final layer.

 

Interestingly, the basement seems to be effective at buffering daily temperature cycles. The temperature in the basement has been hovering around 70 between February and June leaving little for the boxes to mediate.

Sachet
Silica Gel Sachets

The second finding of note is that the sachets of silica gel were spent faster than anticipated. As mentioned above sachets of silica gel were placed in the boxes with cleaned objects. The gel, in solid pebble-like form, starts out orange and as it absorbs water it changes to a deep blue. The expectation was that the gel would keep the RH at a reduced and steady level. The graph above shows that the silica gel was keeping relative humidity lower than that of the box without gel, but it is only a matter of a few percentage points. Most likely the boxes are not well enough sealed for the silica gel to more significantly moderate RH levels. The silica was active from mid-February until mid-April (see star on graph) when RH graphs inside both boxes started to match almost perfectly. A visual inspection in June indicated that the gel was spent. We replaced the silica in mid-June and it was spent within two weeks given the higher RH levels generally in the basement.

 

Our data shows that the boxes are acting as a significant buffer against potentially damaging cycles of increasing and decreasing RH levels. For now, we are forgoing replacing spent silica gel. Later in the fall we’ll see how the archival boxes work with our dehumidifiers at keeping mold and salt inducing RH at bay.

Halfway there…and funding for the finish!

Contributed by Marla Taylor

I am thrilled to share that we have officially inventoried half of the collection!

As of mid-June, the collections team has inventoried 1,079 artifact drawers – half of the 2,159 that hold our collection.  Those drawers translate to 243,967 individual artifacts that have been counted and rehoused in the process!

A massive “thank you” goes out to all of the staff and volunteers who have contributed to the inventory so far: Rachel Manning, John Bergman-McCool, Emma Cook, Annie Greco, Alex Hagler, Quinn Rosefsky, and dozens of work duty students.

With excitement and deep gratitude, we also announce that funding has been secured to complete the inventory by our target deadline of December 31, 2020.

The Oak River Foundation of Peoria, Illinois has renewed its support for a temporary inventory specialist for another two years.  Our deepest appreciation goes to the Oak River Foundation for its continued generosity and commitment to the Peabody’s goal of improving the intellectual and physical control of the museum’s collections.

But that is not all!

Barbara and Les Callahan have agreed to provide critical funding to extend the appointment of our current inventory specialist – John Bergman-McCool.  Les graduated from Phillips Academy in 1968 and is an active volunteer on campus. Barbara has served on the Peabody Advisory Committee since 2013.  Both have been steadfast advocates and supporters of our mission and we cannot thank them enough for providing this deeply meaningful gift.

We hope these acts will inspire others to support our work to better catalog, document, and make accessible the Peabody’s world-class collections of objects, photographs and archival materials. If you would like information on how you can help, please contact Peabody director Ryan Wheeler at rwheeler@andover.edu or 978 749 4493.

Calling All Volunteers!

Have you ever wondered what it would be like to work in a museum? The Peabody, like many museums, has a small force of volunteers who dedicate a few hours each week to helping our staff further our work. We are currently looking to expand this group of volunteers.

Our volunteers have assisted us with a huge number of projects. We currently have one volunteer who works with our textile collection. In a museum setting, it is very important to protect artifacts from pests that can occasionally work their way into the building. Our textile artifacts are particularly susceptible to the damage from carpet beetle and clothes moth larvae. An infestation of these pests can completely destroy a textile collection without proper intervention and pest management. In order to stay on top of any potential pest problems, one of our volunteers systematically goes through our textiles and inspects them for evidence of damage, insect excrement, and live specimens. This involves vacuuming the textiles, inspecting them, and putting them through a freezing process designed to kill living pests. Once this two week process is completed, the textiles are removed from the freezer, isolated, and then inspected again for any signs of life. Once we are satisfied that pests are not present, the objects are returned to the collections storage space. Our volunteer has done an excellent job with this, and has made significant process on this project.

Our other current volunteer is a P.A. alumnus who works on a wide variety of projects. One of the most important projects is our complete inventory of the collection. We hope to renovate the Peabody in the next few years and before we do that, we need to have a completed inventory of our collections. This involves inventory of our storage drawers and recording information about collections, including objects present, count, geographic origin, and current storage location.  Volunteers can help with this most important project.

In addition to helping out with the inventory, volunteers help out as needed across the Peabody. Other projects include organizing portions of the archives for researchers, pulling out and putting away objects for classes, creating labels for our artifact boxes, and transcribing catalog cards into a digital system. There is never a shortage of work to be done at the Peabody!

If this sounds like an opportunity that you would be interested in, feel free to contact me with for more information at rmanning@andover.edu. I would be glad to speak to anyone about potentially volunteering for us!

Fowled in Collection

Contributed by Marla Taylor

This skeleton is from a site near Glorieta, New Mexico – just southeast of Santa Fe – and collected by Alfred Kidder during his work at Pecos Pueblo.

As discussed in a previous blog, The Macaw Factor, the presence of macaws in the southwest is certainly note-worthy.  These birds have a natural habitat approximately 1000 miles to the south and were clearly transported to the region as status symbols.  They may have been kept for their feathers or displayed as a sign of wealth and connections.

Two scarlet macaws
Scarlet macaws

As we continue to move through the collection, who knows what we will find next!

Further reading:

Hill, Erica. “The Contextual Analysis of Animal Interments and Ritual Practice in Southwestern North America.” Kiva 65, no. 4 (2000): 361-98. http://www.jstor.org/stable/30246334.

Wu, Katherine J. “A Macaw Breeding Center Supplied Prehistoric Americans With Prized Plumage.” Smithsonian.com, August 13, 2018.

 

Half-Life: Radiocarbon Dating Tehuacán Carbon Samples

Contributed by Emma Cook

In my last blog I discussed soil analysis and its importance in dating and understanding a site. Another form of analysis used in the Tehuacán Archaeological-Botanical Project by Richard “Scotty” MacNeish was a process called radiocarbon dating, a technique developed by University of Chicago physicist Willard Libby. Carbon samples were collected during excavation and sent for carbon dating to be used for the Tehuacán Chronology Project.

There are two techniques for dating in archaeological sites: relative and absolute dating. Relative dating, in a stratigraphic context, is the idea that objects closer to the surface are more recent in time relative to objects found deeper in the ground. This relates to the law of superposition, which in its plainest form, states soil layers in undisturbed sequences will have the oldest materials at the bottom of the sequence and the newest material closer to the surface. Although this form of dating can work well in certain cases, it does not work for all.

Jars of Carbon Samples from various sites in the Tehuacán Valley.
Jars of Carbon Samples from various sites in the Tehuacán Valley.

Many sites include soil layers that have been disturbed and this can happen several ways. Natural disasters, such as floods, can erase top layers of sites. Rodents can move around layers in a site as they burrow underground, sometimes moving items from one context to another. Even current human activity can change the stratigraphy of a site through construction, post holes, and pits.

This takes us to our second dating technique. Absolute dating represents the absolute age of a sample before the present. Examples of objects that can be used to find absolute dates are historical documents and calendars. However, when working in an archaeological site without documents, it is hard to determine an absolute date. If a site has organic material present, radiocarbon dating can be used to determine an absolute date. Radiocarbon dating is a universal dating technique that is used around the world and can be used to date materials ranging from about 400 to 50,000 years old. Radiocarbon dating may even work on very recent materials.

Part of this carbon sample sent to Isotopes lab for radiocarbon dating.
Part of this carbon sample sent to Isotopes lab for radiocarbon dating.

Organisms such as plants and animals all contain radiocarbon (14C). When these organisms die, they stop exchanging carbon with the environment. When this occurs, they begin to lose amounts of 14C overtime through a process called radioactive decay. The half-life of 14C is about 5,730 years. Radiocarbon dating measures the amount of stable and unstable carbon in a sample to determine its absolute date. As a result, the older the organic material, the less 14C it has relative to stable versions of the isotope.

The carbon samples recovered from the Tehuacán Valley were collected specifically with this in mind. Many of these samples had labels or notes stating that some of each sample was sent to labs for radiocarbon testing. The carbon samples are organic material and their properties of radiocarbon were used to determine the age of the material, which in turn, helped date each site.

Map of the Tehuacán Valley and some of the sites the carbon samples came from.
Map of the Tehuacán Valley and some of the sites the carbon samples came from.

The following sites are represented in some of the jars of carbon samples I catalogued from the Tehuacán Archaeological-Botanical Project.

Site Number                        Site Name                     Radiocarbon years

Tc 35                                         El Riego                                 6800 to 5000 B.C.

Tc 50                                         Coxcatlan Cave                  5000 to 3400 B.C.

Tc 307                                      Abejas                                     3400 to 2300 B.C.

Tc 272                                      Purron Cave                          2300 to 1500 B.C.

Ts 204                                     Ajalpan                                     1500 to 800 B.C.

These results were published in Volume Four of MacNeish’s Prehistory of the Tehuacan Valley: Chronology and Irrigation and can be found on Page 5. MacNeish and Tehuacán Chronology Project director, Frederick Johnson, selected carbon samples to be sent for testing, which resulted in the determination of 218 radiocarbon dates. Johnson played a prominent role in radiocarbon dating, serving as the chair of the Committee on Radioactive Carbon 14 set up by the American Anthropological Association. This project not only produced a chronology for the Tehuacán sequence of excavated sites, but later contributed (along with 400 additional radiocarbon dates) to the chronology for all of Mesoamerica. The dates, however, were made within the first two decades of radiocarbon dating and lack the accuracy and precision now available with newer techniques, especially with the older dates.

To read more about the Tehuacán Archaeological-Botanical Project and the Tehuacán Chronology Project visit Internet Archive.

Further Reading

Libby, Willard F. Radiocarbon Dating, 2nd ed., University of Chicago Press, Chicago, IL, 1955. Print.

MacNeish, Richard S. et al., The Prehistory of the Tehuacan Valley: Chronology and Irrigation. Vol. 4. University of Texas Press, Austin, TX, 1972. Print.

Stromberg, Joseph. “A New Leap Forward for Radiocarbon Dating.” Smithsonian.com, October 18, 2012. Web. https://www.smithsonianmag.com/science-nature/a-new-leap-forward-for-radiocarbon-dating-81047335/

Taylor, R.E. and Ofer Bar-Yosef. Radiocarbon Dating: An Archaeological Perspective. 2nd ed., Routledge, New York, NY, 2016. Print.

The Dirt on Soil Analysis

Contributed by Emma Cook

My latest work for the Peabody Inventory and Rehousing Project has led me to Tehuacán, where I have been cataloguing glass jars that contain soil samples. These jars are a part of the Tehuacán Archaeological-Botanical Project by Richard “Scotty” MacNeish during the early 1960s. The samples were collected for testing and analysis purposes from the project area. When archaeologists excavate a site, they dig through soil layers formed by the activities of past people. What archaeologists recover from these layers provides clues about what happened at that site from features or artifacts. However, the actual soil is another very important clue for archaeologists, as it can help date sites and tell a lot about the environment of the site during the time the soil layers were formed.

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Jars of Soil Samples from the Tehuacán Archaeological-Botanical Project, 1960s

Giving an accurate description of soils help archaeologists better understand what happened in the past at a site. The color and texture of soil can reveal the age of an archaeological site, as well as how the site was used. For example, a circular stain in the soil may reveal a post-hole deposit, indicating that there was once a wooden post that had decayed, leaving a soil discoloration in the ground. Depending on the site, these post-holes could represent a structure or palisade. In addition, studying soil fertility can help archaeologists understand ancient agricultural systems.

Soil blog_pic3
MacNeish (left) and a field assistant analyzing stratigraphy at the Gladstone site on Kluane Lake in the Yukon.

Archaeologists use the Munsell Color Chart to help them describe the colors of the soil layers in a standardized way. This system was developed by Albert H. Munsell at what is now MassArt in 1905. Archaeologists compare the soil color in their excavation units to the color chips of the Munsell Chart – similar to the color squares found in hardware stores for paint. Where a color may be brown to one person, it may be gray to another – so it is important that archaeologists use this chart so they can standardize their descriptions.

Munsell Color Chart
Munsell Color Chart

To describe soil textures, archaeologists and geomorphologists use a soil triangle to help them determine what type of soil they are examining in the field. There are three types of soil components: sand, silt, and clay. Most soils have a combination of these three components and each of these components vary in sizes – sand particles being the largest and clay particles being the smallest. Similar to how the Munsell Color Chart describes soil color the same way, the soil triangle helps archaeologists describe soil texture consistently.

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Soil Triangle – Courtesy of the United States Department of Agriculture

Another way archaeologists analyze their site is through soil stratigraphy. This is the different types of strata, or layers of soil that archaeologists examine to map out the archaeological site over time. Stratigraphy can be used to determine which soil was associated with human occupation and which layers are sterile, meaning the soil is not associated with human occupation and does not contain any archaeological material. Layers that include artifacts and features represent a place where people lived and worked, as archaeologists can see the objects left behind by human activity. Sterile layers such as subsoil, flood sediment, and bedrock are not as distinct, but provide information on a site’s activity or inactivity.

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Archaeologists mapping out the stratigraphy at Purron Cave, TC 272, in the Tehuacán Valley.

The jars of soil samples were most likely examined after excavation and retained for further analysis. Presently, these soil samples have been rehoused and cataloguing for each of these jars is complete. To learn more about Richard “Scotty” MacNeish and the Tehuacán Archaeological-Botanical Project, visit the Peabody’s online archival collections. The MacNeish archives are available for research, separated into two collections – the Richard S. MacNeish Papers and the Richard S. MacNeish Records.

 

Further Readings

Birkeland, Peter W. 1974. Pedology, Weathering, and Geomorphological Research, New York: Oxford University Press.

Limbrey, Susan. 1975. Soil Science and Archaeology. London and New York: Academic Press.

Solecki, R. 1951. Notes on Soil Analysis and Archaeology. American Antiquity, 16(3), 254-256.

Uninvited Guests

Contributed by John Bergman-McCool

Mold_Salt 1
Meet Mold and Salt

In early February we wrapped up inventorying and rehousing collections that originated in Missouri. The work was followed by two weeks of cleaning, and as a result we’ve completed one of the regions held in the collection. So you may be wondering what we were cleaning. During the inventory, we encountered bone and antler objects covered with salt crystals and patchy dormant mold. The objects were cleaned before they were stored inside their new boxes to remove salt and minimize the risk of mold spreading to unaffected objects.

Where did the mold and salt come from and why are they a problem?

Mold spores are found everywhere in the environment. When the humidity is high, those spores germinate resulting in mold. Because it is a living organism, mold is classified in the museum world as an agent of biological deterioration. It eats organic matter, in this case the dust resting on the outer surface of bone or the bone itself, and secretes waste that can stain or damage the surface that it is growing on. Mold can appear to be dormant, but when the conditions are right mold will generate spores that are easily borne on the wind, allowing it to spread quickly.

Mold_Salt 2
Agents of deterioration

Salts on the other hand are considered chemical agents of deterioration. They are brought into museum collections on the objects themselves.  Dissolved salts present in groundwater can be absorbed by porous objects, such as bone, while they are buried underground. After the water evaporates the salts are left behind. Excessively humid conditions can dissolve soluble salts, allowing them to move through porous objects. When they arrive at the surface they form crystals. If the crystals form below the surface they can exert enough force to cause damaging cracks and spalling.

Mold and salt thrive in damp environments where the Relative Humidity (RH) is above 65%. The institute’s storage area is located in the basement, which does not have a controlled climate, so mold and salt are an unfortunate reality. Currently, the RH in the basement is somewhere below 15% (15% is as low as our monitoring equipment can read). RH levels this low shouldn’t support active mold and salt growth, so what we found is inactive, but it is hard to say when and for how long the growth of mold and salt was last active.

At the Peabody we are committed to maintaining the longevity of this very important research collection and salt and mold pose a risk to its scientific viability. Damage to the surface of artifacts caused by mold and salt can negatively impact the research value of the collection.

How do we prevent mold and salt?

While we don’t have an HVAC system maintaining the environment in basement storage, we have adopted a few practices that will mitigate and prevent future growth of mold and salt. First, we use dehumidifiers during times of high humidity that typically arise during the summer. Second, we are moving the artifacts currently stored in open drawers and rehousing them in closed archival boxes. The enclosed space of a box helps create a buffer that protects the contents from rapid shifts in RH that lead to mold and salt growth. The boxes will also keep future mold growth from spreading; something that was not possible with open-drawer storage.

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Vacuum defeats Mold and Salt

In addition to the rehousing, we have implemented a cleaning program. When mold and salt are identified we isolate the effected object to keep spores from spreading. We clean the affected artifacts with a dry brush and vacuum. After we clean we use sachets of silica gel to absorb excess moisture, thereby providing another buffer against cycles of RH increases and decreases. In six months we’ll check on the status of the bone to see if the mold and salt are staying away.

More Than a Number: Cataloguing the Peabody Collection

Contributed by Emma Cook

My name is Emma Cook, I am the Administrative Assistant at the Robert S. Peabody Institute of Archaeology. I have a background in archaeology, history, and museum studies with undergraduate and graduate degrees from the University of Georgia and Tufts University. Aside from my administration duties, I work with the Peabody’s collections. Recently I’ve been involved in the Inventory and Rehousing Project and I am working with collections on the first floor South Alcove, located in one of our gallery/classroom spaces.

The Robert S. Peabody Institute of Archaeology collection comprises nearly 600,000 artifacts, photographs, and archives. Some of these materials are displayed and used for teaching, while many reside in our collection storage. What is unique about much of our collection space is its original storage. The bays and drawers in which many of these artifacts inhabit are almost as old as the Peabody itself, the bays being first built in the early 1920s. However, below the surface of these pine wood bays and drawers are a collection of uncatalogued objects that have hardly come to light (literally), with some still stored in the tin foil and paper bags they were placed in upon archaeological excavation many years ago.

The antiquated charm of these wooden bays is not enough to meet the need of accessible storage for our collections and the goal is to replace them with new custom-built shelves. In preparation of this storage renovation, objects need to be identified, catalogued, and rehoused. This work is completed through our Inventory and Rehousing Project.

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First Floor, South Alcove – where my cataloguing work began

I began my work simply inventorying the objects in each drawer of each bay in the alcove. Some of these objects were already identified, numbered, and recorded in Past Perfect – a museum software that is the standard for cataloguing museum collections. Through this software, the Peabody collection is documented and made accessible online. My job was to make sure these objects were accounted for and in the right place, as well as properly rehoused and organized within the drawers. Sounds pretty easy right? Well, eventually things changed as I came across several drawers and bays containing objects with old numbers or no numbers at all. This is where my cataloguing efforts began.

Cataloguing is the process of recording details about an object into a collection catalog or database that documents the information of each object as well as its location in storage. Through this process each object receives a unique number. This number is physically attached to the object and appears in records related to the object in Past Perfect. In museums and archives, objects or materials in a collection are normally catalogued in what is called a collection catalog. In the past, this was traditionally done using a card index, but in the present-day it is normally implemented using a computerized database – for the Peabody this is Past Perfect. Some of the objects I came across with “old numbers” were either connected to the Peabody’s past card index cataloguing system or the Peabody’s original numbering system (i.e. 1,2,3,…. 78,049).

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Lithic objects with affixed labels and old numbers

Each object was given a new number associated with the Peabody’s present catalog numbering sequence (i.e. 2019.1.123). This numbering sequence is a three-part number, making it both simple and expandable. The first part of the sequence is the year in which the object was accessioned or catalogued (i.e. 2019). The second part of the sequence is given to objects in chronological order based on when they were first accessioned (i.e. 2019.1). The third part of the sequence gives a single object a number in chronological order (i.e. 2019.1.1). Objects that had an affixed label had the new number written on the label. Objects without labels had their numbers painted on with ink. A solution called B72 is applied to the object before the ink in order to protect the original surface of each object. This solution is not harmful to the object and can be easily removed if a mistake is made or the object needs a different number.

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Lithic objects with new numbers painted on their surface using ink and the B72 solution

The cataloguing process is not an easy one, nor is inventorying and rehousing a collection. The process may be slow and tedious, but it does have its rewards. By using a great deal of care, time, and effort, rehoused and identified objects can be used for teaching and research. Not only can collection staff have full access to the collection, they can provide a safe and accessible place for these materials in storage. The cataloguing process may seem like a trivial task, but it just goes to show – it’s more than a number.

For more information and reading on the Inventory and Rehousing Project, see the following blogs below:

Transcribing the Collection – January 2019

A New Face in the Basement – January 2019

Ceramic Inventory Complete – December 2018

Collections Reboxing Project Update – April 2018

A Day in the Life of Boxing Boxes – November 2017

Shelving to the Rescue – September 2016

Boxes and Boxes and Boxes – August 2016

Summer Work Duty Students Begin Rehousing Inventory – August 2016

A New Face in the Basement

Contributed by John Bergman-McCool

Hi there! My name is John and I am the new Inventory Specialist at the Robert S. Peabody Institute. As Inventory Specialist my primary task is to work on the ongoing inventory and rehousing project. The project’s goals are to fully understand the collections that are held at the Institute and move them from their old wooden drawers into archival boxes. Armed with the more precise knowledge of what is in the Peabody, the institute can ensure their continued care and share them with students and the public for years to come.

This position is a dream job for me. It brings together my interest in archaeology, museums and collections care, and who doesn’t love spending time underground!

John inside a pit during excavations
Yep, this is me in a bell pit during an excavation in Arizona!

Before moving to Massachusetts in 2013, I worked for almost a decade as an archaeologist in the Pacific Northwest and Arizona. After relocating to New England I enrolled in the MFA program at Tufts and the School of the Museum of Fine Arts. During my time as a graduate student I found that I kept coming back to archaeology and the history of museum collections as a subject for my artwork.

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Artwork from my thesis project

While I was in graduate school I also pursued a certificate in Museum Studies. I gravitated towards collections care and since graduating I’ve worked in collections at the Fitchburg Art Museum and Historic New England. ­

In a round-about way I’ve come back to archaeology, though it’s been following me for the past 5 years. During my time here I’ve been inventorying objects from Missouri. There have been some surprising finds, which has been great. You never know what you’re going to find here at the Peabody.

Party’s not over – volunteering at the Peabody

Contributed by Quinn Rosefsky ’59

No one invited us to the party but we’ve stayed for over nine years. And the desserts keep getting better. Not that what we do would come under the category of party. What should be obvious to readers of this blog is that I am talking about what it is like to volunteer at the Peabody Institute. First of all, who can volunteer? Being a graduate of Phillips Academy helps in passing the rigorous entrance examination but there are exceptions, such as my wife, Susan, whose qualifications, while many, started with marriage. This automatically reduces the interview process (but does not eliminate the background check.) And what do volunteers do?

Some of you might get the wrong impression that all we do is what the staff shy away from. Far from it. There have been plenty of occasions where it was all we could do to pry staff apart from a project to allow us to either dig into the unknown (such as categorizing about one hundred yards of unclassified photos) or finish it off (such as one hundred yards of labels.)

Of course, I am exaggerating. (No point in frightening you.) I have handled (and often read) documents from the nineteenth and twentieth centuries; paleolithic artifacts from 10,000 B.C.E; ledgers with tens of thousands of entries. I can picture specific bifaces, sherds and feathers.

What my wife, Susan, and I have been doing has varied considerably over the years as staff have come and gone, priorities have shifted, and time frames have expanded. I like to think that volunteering has allowed the Peabody to think in terms of decades, not centuries. This might come as a surprise until you consider that the Peabody is home to somewhere in the vicinity of 600,000 artifacts.

For quite a number of the past nine years, Susan and Leah (another spectacular volunteer) have been inspecting, vacuuming and protecting textiles from Guatemala. Although the end of the project has been in their sights for the past year, Einstein’s theory of special relativity keeps getting in the way (time slowing, distances shortening…easy stuff.) Eager to try my own hand at a multitude of projects, my time has been slowed as well. Despite Einstein’s slowing of time as we operate at the speed of light, sadly, all of us working as an extended family inside the Peabody’s walls have grown somewhat older (but not by much and not at the same rate.)

Most recently, I had the task of filling out labels to put on a few of the 1,500 drawers containing a variety of artifacts. It was a matter of necessity, not just my dexterity and eye coordination. When I completed that task, it was my honor to look for the “absence” of items. It all started with the discovery that an item had been “mislabeled.” That’s akin to looking through a haystack and saying you didn’t find the needle. And winning means you did not find the needle.

Sometimes I write blogs. I’ll stop here because my limit is 500 words. (Only staff can do more!)

Yoda_Quinn
Quinn after volunteering for 9 years