Ledger for the Classes of 1744-1749, 1733-1750

The volume, bound in a hardcover parchment binding, contains accounts for the Classes of 1744-1749.

Ledger for the Classes of 1795-1804, 1795-1804

The leather bound folio account book kept by Steward Caleb Gannett contains accounts for members of the Classes of 1795-1804, as well as accounts for President Joseph Willard, Tutors, Fellows, and Faculty. The volume also contains the Steward's accounts with the Harvard Treasurer, as well as his "Cash" accounting. The volume does not have the detailed transaction descriptions found in earlier ledgers; both Credit and Debit entries are described as being paid by, or being owed to, cash, balance, sundry accounts, or the Treasury.

Ledger, 1795-1804

The large leather-bound volume contains a final monthly accounting of Steward Gannett's financial transactions from December 1795 through September 1804. The journal records four types of transactions: "Sundry accounts dr to Treasury," "Cash dr to sundry accounts," "Treasury dr to sundry accounts," and Treasury Dr to Treasury orders." The pages are arranged into columns for account numbers, transaction descriptions, and associated amounts. The entries reflect the movement of funds between the Steward's cash and sundry accounts and the Treasury. Transaction descriptions include student names and amounts based on quarterly bills, specific scholarship and salary allocations, and the names of individuals paid for services, from wood suppliers to medical instructors.

Quarter bill book for the Classes of 1689-1723 and ledger, 1687-1720

Parchment hardcover bound volume arranged into two parts: Quarter bill book and the Steward's ledger. The Quarter bill book contains quarter bill tallies for the Classes of 1689-1723 arranged by seniority, and covers the bill period ending on October 21, 1687 through the period ending March 11, 1720.

Ledger book of a court clerk, 1768-1773

Ledger book of Isaac Rindge, chief clerk of the court of common pleas in New Hampshire, listing charges to various individuals for writs and fines.

Fault development and interaction in distributed strike-slip shear zones: an experimental approach

Analogue model experiments using both brittle and viscous materials were performed to investigate the development and interaction of strike-slip faults in zones of distributed shear deformation. At low strain, bulk dextral shear deformation of an initial rectangular model is dominantly accommodated by left-stepping, en echelon strike-slip faults (Riedel shears, R) that form in response to the regional (bulk) stress field. Push-up zones form in the area of interaction between adjacent left-stepping Riedel shears. In cross sections, faults bounding push-up zones have an arcuate shape or merge at depth. Adjacent left-stepping R shears merge by sideways propagation or link by short synthetic shears that strike subparallel to the bulk shear direction. Coalescence of en echelon R shears results in major, through-going faults zones (master faults). Several parallel master faults develop due to the distributed nature of deformation. Spacing between master faults is related to the thickness of the brittle layers overlying the basal viscous layer. Master faults control to a large extent the subsequent fault pattern. With increasing strain, relatively short antithetic and synthetic faults develop mostly between old, but still active master faults. The orientation and evolution of the new faults indicate local modifications of the stress field. In experiments lacking lateral borders, closely spaced parallel antithetic faults (cross faults) define blocks that undergo clockwise rotation about a vertical axis with continuing deformation. Fault development and fault interaction at different stages of shear strain in our models show similarities with natural examples that have undergone distributed shear.

Pliocene-Pleistocene stack of globally distributed benthic stable oxygen isotope records

We present a 5.3-Myr stack (the ''LR04'' stack) of benthic d18O records from 57 globally distributed sites aligned by an automated graphic correlation algorithm. This is the first benthic delta18O stack composed of more than three records to extend beyond 850 ka, and we use its improved signal quality to identify 24 new marine isotope stages in the early Pliocene. We also present a new LR04 age model for the Pliocene-Pleistocene derived from tuning the delta18O stack to a simple ice model based on 21 June insolation at 65 N. Stacked sedimentation rates provide additional age model constraints to prevent overtuning. Despite a conservative tuning strategy, the LR04 benthic stack exhibits significant coherency with insolation in the obliquity band throughout the entire 5.3 Myr and in the precession band for more than half of the record. The LR04 stack contains significantly more variance in benthic delta18O than previously published stacks of the late Pleistocene as the result of higher resolution records, a better alignment technique, and a greater percentage of records from the Atlantic. Finally, the relative phases of the stack's 41- and 23-kyr components suggest that the precession component of delta18O from 2.7-1.6 Ma is primarily a deep-water temperature signal and that the phase of d18O precession response changed suddenly at 1.6 Ma.

Highway taxes and fees - how they are collected and distributed. 1995.

Mode of access: Internet.

The ledger-book of Vale Royal Abbey.

Mode of access: Internet.