Settlement of chambers, 1741-1764

The book is comprised of folio-sized pages conserved in a modern soft-cover binding. The volume consists of yearly handwritten lists of dormitory room assignments for the years 1741-1753 and 1761-1764. Students are listed by last name and building names are often abbreviated as "M" for Massachusetts Hall, "S" for Stoughton Hall, and "O" for Old College or Harvard Hall. The organizational pattern varies by list, some are alphabetical, others arranged by building and room number. The lists for 1743, 1748, 1749, 1761-1764 also note students living outside of the College and their locations. The lists for 1761-1764 also include the waiters and monitors for the academic year.

Process of Expropriation of Buildings for the Construction of the New Dock of the Port of Cartagena (Spain) in the 18th Century

The need of the Bourbon monarchy to build a Naval Base in the Bay of Cartagena (Spain) during the eighteenth century, implied performing various actions on the environment which allowed the construction of the new dock. One of the priority actions was the transformation of the watershed of the streams that flowed into Mandaraches´s sea. For this reason, a dike was designed and constructed in the northern part of the city. The design of this great work, which was designed as a fortification of the city, was subject to considerable uncertainties. Its proximity to the city involved the demolition of several buildings in the San Roque´s neighborhood. The greater or lesser number of affected buildings and the value of the just indemnification for the expropriation of them, become decisive factors to determine if the work was viable for the Royal Estate or not.

Plan of College buildings and lot from Mr. Bulfinch, [ca. 1814]

Known as the Bulfinch view, this proposed site plan of the College grounds by Charles Bulfinch depicts University Hall at the center of the drawing surrounded by Massachusetts, Harvard, Hollis, Stoughton, and Holworthy Halls. Several unlabeled buildings are displayed in the plan.

Description of a College Chamber (manuscript copy), ca. 1744

This humorous, rhyming poem appears to have been co-authored by Thomas Handcock of Massachusetts and Richard Waterman of Warwick, Rhode Island. The document is also signed by Catharine Waterman. Neither of the authors attended Harvard College, and the circumstances of this poem's creation are not known. The poem suggests that they composed the poem while visiting - uninvited - the room of "honest Bob." The poem describes the contents of this college chamber, including the following items: an oak table with a broken leg; paper, a pen, and sand for writing; books, including "Scotch songs," philosophy, Euclid, a book of prayer, Tillotson, and French romances; pipes and tobacco; mugs; a broken violin; copperplate and mezzotint prints; a cat; clothes; two globes; a pair of bellows; a broom; a chamber pot; a candle in a bottle; tea; cups and saucers; a letter to Chloe, to whom the room's inhabitant apparently owed money; a powder horn; a fishing net; a rusty gun; a battledore; a shuttlecock; a cannister; a pair of shoes; and a coffee mill. The poem references events related to the War of Austrian Succession (1740-1748); British Vice Admiral Edward Vernon's siege of Portobello (in present-day Panama) in 1739; the "Rushian War" (perhaps the Russo-Swedish War of 1741-1743); and the War of Jenkins' Ear (the cat in the college chamber, like British Captain Robert Jenkins, has lost an ear).

Valedictory poem delivered in the Chapel of Harvard University on the 21 June 1796: in the presence of the President Proffers & Tutors & the four classes of understudents at the request of the class who completed their college studies on that day

Handwritten draft of the Charles P. Sumner’s valedictory poem to the Harvard class of 1796, in a 19th century hardcover binding beginning “The youth by adverse fortune forced to roam…”. The poem mentions John Russell, a member of the Class of 1796 who died in November 1795. The copy includes edits and struck-out words.

A poem delivered at Harvard College, September 29th, 1789

Eight-page untitled handwritten poem attributed to Harvard student Benjamin Whitwell (Harvard AB 1790). The poem begins “The brow of age is soften’d into smiles” and contains classical and militaristic allusions. An annotation indicates that a set of stanzas beginning, “On thee, our common parent! Guardian! Friend! His mildest warmth, his brightest beams descend….” refers to Harvard President Joseph Willard. The text includes edits and annotations.

Letter from Samuel Willard, Harvard College, Cambridge, Massachusetts, to Sophronia Willard, Lancaster, Massachusetts, October 18, 1805

Willard describes his current job working at Harvard, where he is paid “to keep order in one of the buildings.” He mentions that he can attend medical lectures free of charge, and refers to a preacher, Mr. Parker, a former classmate of Willard’s. He explains that he is currently with his brother Solomon, who is ill, and that he is living in the College House, where he resided his first year of school.

Collection of Harvard College bills sent to George Wingate, 1792-1796

This collection of bills, sent to George Wingate while he was an undergraduate at Harvard College from 1792 to 1796, includes quarter bills, butler's bills, and bills and receipts of payment from two women, Mary Hilliard and Mary Kidder, who provided Wingate room and board ("board and chamber"). The butlers bills were created by the two men who held that position during Wingate's time as a student, John Pipon and Timothy Alden. Caleb Gannett was the steward the entire time, and thus creator of all the quarter bills. Some of the bills indicate charges for sizings and fines for punishments, and a bill from Mary Hilliard indicates that Wingate purchased candles, blank books and sheets of paper from her.

Collection of Harvard College quarter bill and butler's bills sent to Charles Davis, 1793-1796

This collection consists of one quarter bill and three butler's bills, all sent to Charles Davis while he was an undergraduate at Harvard College. The quarter bill is from August 1795 and the butler's bills are from February and November 1793 and July 1796. John Pipon and Timothy Alden were the butlers at this time, and Caleb Gannett was the steward (responsible for the quarter bill).

Reconstructions of past climates from documentary and natural sources in Finland since the 18th century

In this paper both documentary and natural proxy data have been used to improve the accuracy of palaeoclimatic knowledge in Finland since the 18th century. Early meteorological observations from Turku (1748-1800) were analyzed first as a potential source of climate variability. The reliability of the calculated mean temperatures was evaluated by comparing them with those of contemporary temperature records from Stockholm, St. Petersburg and Uppsala. The resulting monthly, seasonal and yearly mean temperatures from 1748 to 1800 were compared with the present day mean values (1961-1990): the comparison suggests that the winters of the period 1749-1800 were 0.8 ºC colder than today, while the summers were 0.4 ºC warmer. Over the same period, springs were 0.9 ºC and autumns 0.1 ºC colder than today. Despite their uncertainties when compared with modern meteorological data, early temperature measurements offer direct and daily information about the weather for all months of the year, in contrast with other proxies. Secondly, early meteorological observations from Tornio (1737-1749) and Ylitornio (1792-1838) were used to study the temporal behaviour of the climate-tree growth relationship during the past three centuries in northern Finland. Analyses showed that the correlations between ring widths and mid-summer (July) temperatures did not vary significantly as a function of time. Early (June) and late summer (August) mean temperatures were secondary to mid-summer temperatures in controlling the radial growth. According the dataset used, there was no clear signature of temporally reduced sensitivity of Scots pine ring widths to mid-summer temperatures over the periods of early and modern meteorological observations. Thirdly, plant phenological data with tree-rings from south-west Finland since 1750 were examined as a palaeoclimate indicator. The information from the fragmentary, partly overlapping, partly nonsystematically biased plant phenological records of 14 different phenomena were combined into one continuous time series of phenological indices. The indices were found to be reliable indicators of the February to June temperature variations. In contrast, there was no correlation between the phenological indices and the precipitation data. Moreover, the correlations between the studied tree-rings and spring temperatures varied as a function of time and hence, their use in palaeoclimate reconstruction is questionable. The use of present tree-ring datasets for palaeoclimate purposes may become possible after the application of more sophisticated calibration methods. Climate variability since the 18th century is perhaps best seen in the fourth paper study of the multiproxy spring temperature reconstruction of south-west Finland. With the help of transfer functions, an attempt has been made to utilize both documentary and natural proxies. The reconstruction was verified with statistics showing a high degree of validity between the reconstructed and observed temperatures. According to the proxies and modern meteorological observations from Turku, springs have become warmer and have featured a warming trend since around the 1850s. Over the period of 1750 to around 1850, springs featured larger multidecadal low-frequency variability, as well as a smaller range of annual temperature variations. The coldest springtimes occurred around the 1840s and 1850s and the first decade of the 19th century. Particularly warm periods occurred in the 1760s, 1790s, 1820s, 1930s, 1970s and from 1987 onwards, although in this period cold springs occurred, such as the springs of 1994 and 1996. On the basis of the available material, long-term temperature changes have been related to changes in the atmospheric circulation, such as the North Atlantic Oscillation (February-June).