History of the early settlement and progress of Cumberland County, New Jersey : and of the currency of this and adjoining colonies /

Includes index.

An exposition of the character and management of the New Jersey joint monopolies : the Camden and Amboy railroad and transportation company, the Delaware and Raritan canal company, and their appendages /

Mode of access: Internet.

Mayflower Pilgrim descendants in Cape May County, New Jersey; memorial of the three hundredth anniversary of the landing of the Pilgrims at Plymouth, 1620-1920; a record of the Pilgrim descendants who early in its history settled in Cape May County, and some of their children throughout the several states of the union at the present time,

Lettered on cover: Mayflower descendants in Cape May County, 1620-1920.

The Daily union history of Atlantic City and County, New Jersey. Containing sketches of the past and present of Atlantic City and County ...

"Biographies": p. 443-517.

Address of the directors of the Camden and Amboy Rail Road and Delaware and Raritan Canal companies to the people of New Jersey.

Original has call no. : ARCHIVES/O/J900/M2/no. 54

Geologic and water-supply reports and maps : Pennsylvania-New Jersey.

Mode of access: Internet.

Opinion of Gov. Williamson and Gen. Wall, on the rights vested in the Delaware and Raritan Canal and Camden and Amboy Railroad companies, by the acts of the state of New Jersey passed in relation to them.

Signed (page 20): I.H. Williamson, Elizabethtown, Dec. 8th, 1834 ... Garret D. Wall, Burlington, Dec. 19th, 1834.

Memorial of the united Delaware and Raritan Canal Co., Camden and Amboy Railroad and Transportation Company and New Jersey Railroad and Transportation Co., to the Legislature of New Jersey.

Petition for reduced transit duty of heavy products carried.

Shall the extension or recreating of the Camden & Amboy Railroad monopoly be permitted by the people of New Jersey, and made perpetual?

Cover title.

Cape May County Board of Taxation, Cape May Court House, New Jersey.

"September 1995"--P. iii.

Extent and frequency of inundation of Millstone River flood plain in Somerset County, New Jersey,

Open-file report [no. 4]

Impact of Rapid Transit on the Residential Market in Hudson County, New Jersey

The New York Metropolitan region is one of the most populous urban agglomerations in the world, and the single largest in North America.[1] It is also one of the most prominent economic centers, with New York City at the epicenter of its growth. With the entire region growing rapidly over the last decade, it is essential to analyze the socio-economic changes in order to understand the impact it has on commercial real estate. With its focus on housing rentals, this study aims to highlight housing costs as a function of rapid transit over time.

Fluorescent Chrysotile From Sterling Hill, New Jersey

Minerals of the serpentine group, notably chrysotile and to a lesser extent lizardite, are widely present at both Franklin and Sterling Hill. They are late-stage hydrous magnesium silicate minerals that formed by hydrothermal alteration of earlier species, among them willemite and tephroite, and are also common components of hydrothermal veins cutting the ore bodies and the enclosing marble (Dunn, 1995). Although long recognized in the area (Fowler, 1825), local serpentine was not documented as a fluorescent mineral until 2004, when a brief description of a fluorescent serpentine from Franklin appeared in The Picking Table (Cianciulli, 2004). In the present paper, we describe additional examples of fluorescent serpentine, most from Sterling Hill.

Chemical composition of hydrothermal sulfide minerals from the Rainbow, Logachev-1, and Logachev-2 hydrothermal fields

Composition of ore minerals in MAR sulflde occurrences related to ultramaflc rocks was studied using methods of mineragraphy, electron microscopy, microprobe analysis, and X-ray analysis. Objects are located at various levels of maturity of sulflde mounds owing to differences in age, duration and degree of activity of the following hydrothermal systems: generally inactive Logatchev-1 field (up to 66.5 ka old), inactive Logatchev-2 field (3.9 ka), and generally active Rainbow field (up to 23 ka). Relative to MAR submarine ore occurrences in the basalt substrate, mineralization in the hydrothermal fields mentioned above is characterized by high contents of Au, Cd, Co, and Ni, along with presence of accessory minerals of Co and Ni. The studied mounds differ in quantitative ratios of major minerals and structural-textural features of ores that suggest their transformation. Ores in the Logatchev-1 field are characterized by the highest Cu content and development of a wide range of multistage contrast exsolution structures of isocubanite and bornite. In the Logatchev-2 field, sphalerite-chalcopyrite and gold-arsenic exsolution structures are present, but isocubanite exsolution structures are less diverse and contrast. The Rainbow field is marked by presence of homogenous isocubanite and the subordinate development of exsolution structures. The authors have identified four new phases in the Cu-Fe-S system. Phases X and Y (close to chalcopyrite and isocubanite, respectively) make up lamellae among isocubanite exsolution products in the Logatchev-1 and Logatchev-2 fields. Phase Y includes homogenous zones in zonal chimneys of the Rainbow field. Phases A and B formed in the orange bornite domain at low-temperature alteration of chalcopyrite in the Logatchev-1 field. Mineral assemblages of the Cu-S system are most abundant and diverse in the Logatchev-1 field, but their development is minimal in the Logatchev-2 field where mainly Cu-poor sulfides of the geerite-covellite series have been identified. Specific features of mineral assemblages mentioned above reflect the maturity grade of sulfide mounds and can serve as indicators of maturity.

Stable isotope geochemistry of pore waters and marine sediments from the New Jersey shelf: Methane formation and fluid origin

Interstitial water and sediment samples of the Integrated Ocean Drilling Program (IODP) expedition 313 "New Jersey Shallow Shelf" were analyzed for chemical composition and stable isotope ratios. A total of 222 water samples were collected from the cores by Rhizon samplers and squeezing of fresh core material. Water was analyzed for its stable oxygen and hydrogen isotope geochemistry (d2H and d18O) at sites M0027A and M0029A, and the carbon isotope composition of the dissolved inorganic carbon (d13CDIC) (all sites). In addition, organic material (Corg) and inorganic carbonates from sediments were analyzed for their carbon ratios (d13Corg and d13Ccarb), and in case of the carbonates also for oxygen (d18Ocarb). Carbon isotopes were also analyzed in samples containing enough methane gas (d13Cmeth). Pore fluids from site M0027A were analyzed for the sulfur isotope composition of dissolved sulfate (d34S). The combination of isotope analyses of all phases (interstitial water, sediment, and gas) with pore water chemistry is expected to enable a better understanding of processes in the sediment and will help to identify the origin of fluids under the New Jersey shelf.