Some historical remarks concerning the Collegiate school of Connecticut in New Haven, now Yale-college, written in part Nov. 20, 1717.

Mode of access: Internet.

Anti-slavery before Garrison; an address at a meeting of the Connecticut society of the Order of the founders and patriots of America, September 19, A. D. 1902,

Mode of access: Internet.

Annual report - State bar association of Connecticut

Mode of access: Internet.

The law of collateral inheritance, legacy and succession taxes, embracing the American and many English decisions, with forms for New York state, and an appendix giving the statutes of New York, Pennsylvania, Maryland, and Connecticut,

Mode of access: Internet.

The New Haven convention of 1778. The boundary line between Connecticut and New York. The ecclesiastical constitution of Yale college. Three historical papers read before the New Haven colony historical society,

From the advance sheets of vol. III of the Transactions of the society.

Connecticut school document ...

Mode of access: Internet.

The Connecticut school journal.

Title from caption.

Reports of cases determined in the Circuit court of the United States, for the Second circuit, comprising the districts of New-York, Connecticut, and Vermont.

Mode of access: Internet.

Bulletin ... Storrs Agricultural Experiment Station, Storrs, Connecticut.

Imprint varies.

The Thomas Lee House, East Lyme, Connecticut; a history and description,

Mode of access: Internet.

History of maritime Connecticut during the American revolution, 1775-1783, /

Mode of access: Internet.

Family names of the plant kingdom. Sponsors: the New York Botanical Garden ... [and] the Connecticut Agricultural Experiment Station.

Mode of access: Internet.

Connecticut digest of administrative reports to the Governor.

Report year 1956/57-1958/59 ends June 30.

Dominant wave energy and sediment movement on intertidal beaches in Freshwater Bay, Washington, U.S.A.

Freshwater Bay (FWB), Washington did not undergo significant erosion of its shoreline after the construction of the Elwha and Glines Canyon Dams, unlike the shoreline east of Angeles Point (the Elwha River’s lobate delta). In this paper I compare the wave energy density in the western and eastern ends of the Strait of Juan de Fuca with the wave energy density at the Elwha River delta. This indicates seasonal high- and low-energy regimes in the energy density data. I group multi-year surveys of four cross-shore transects in FWB along this seasonal divide and search for seasonal trends in profile on the foreshore. After documenting changes in elevation at specific datums on the foreshore, I compare digital images of one datum to determine the particle sizes that are transported during deposition and scour events on this section of the FWB foreshore. Repeat surveys of four cross-shore transects over a five-year period indicate a highly mobile slope break between the upper foreshore and the low-tide delta. Post-2011, profiles in eastern FWB record deposition in the landward portion of the low-tide terrace and also in the upper intertidal. Western FWB experiences transient deposition on the low-tide terrace and high intra-annual variability in beach profile. Profile elevation at the slope break in western FWB can vary 0.5 m in the course of weeks. Changes in surface sediment that range from sand to cobble are co-incident with these changes in elevation. High sediment mobility and profile variation are inconsistent with shoreline stability and decreased sediment from the presumed source on the Elwha River delta.

A new analytical solution for water table fluctuations in coastal aquifers with sloping beaches

The Boussinesq equation appears as the zeroth-order term in the shallow water flow expansion of the non-linear equation describing the flow of fluid in an unconfined aquifer. One-dimensional models based on the Boussinesq equation have been used to analyse tide-induced water table fluctuations in coastal aquifers. Previous analytical solutions for a sloping beach are based on the perturbation parameter, epsilon(N) = alphaepsilon cot beta (in which beta is the beach slope, alpha is the amplitude parameter and epsilon is the shallow water parameter) and are limited to tan(-1) (alphaepsilon) much less than beta less than or equal to pi/2. In this paper, a new higher-order solution to the non-linear boundary value problem is derived. The results demonstrate the significant influence of the higher-order components and beach slope on the water table fluctuations. The relative difference between the linear solution and the present solution increases as 6 and a increase, and reaches 7% of the linear solution. (C) 2003 Elsevier Ltd. All rights reserved.