(Table 1) Magnetozone boundaries, age and sedimentation rate at DSDP Hole 93-605

Natural Remanent Magnetization (NRM) was measured for regularly spaced samples from the 620-m-thick, lower middle Eocene to upper Maestrichtian section of DSDP Site 605. The total NRM of the Eocene chalks was too low (5-50 µA/m) to establish a reliable magnetic polarity stratigraphy. However, the results from the somewhat more clayrich Paleocene-upper Maestrichtian section are useful. A fourfold quality classification of the results of progressive demagnetization studies aided in determining the polarity of the original remanence. Two types (1 and 2a) showed a Characteristic Remanent Magnetization (ChRM) direction with reversed and normal polarity, respectively; the third type (2b) can be interpreted as having a reversed ChRM, which could not be cleaned, whereas the fourth type (3) is considered to be unreliable. The Site 605 magnetic polarity stratigraphy compares well with published sections, adding important detail to the correlation with planktonic microfossil zones and, hence, to the resolution of this portion of the time scale (C24-C32 on the Berggren et al., 1985, scale). The Cretaceous/Tertiary boundary occurs in a reversed polarity zone that has been correlated with Subchron C29r. We suspect the presence of an unconformity at the boundary between lithostratigraphic Units Va and IV a location which is also the level of Reflection Horizon A*.

Polarity chron boundaries and interval sedimentation rates of ODP Leg 162 sites

Magnetic polarity stratigraphies for Sites 980-984 are based on shipboard measurements from the pass-through magnetometer after alternating field (AF) demagnetization at a peak field of 25 mT and shore-based stepwise AF demagnetization of discrete samples. The characteristic magnetization component was determined after AF demagnetization removed the steep downward drill-string-related magnetic overprint. Peak AF fields in the 20-30 mT range were required to resolve the component, carried by magnetite, that was used to produce unambiguous Pliocene-Pleistocene magnetic stratigraphies at all five sites. At Sites 980 and 983, magnetic stratigraphies were resolved to the base of the recovered advanced hydraulic piston corer (APC) section, which lies in the Matuyama Chron (1r.2r) and Olduvai Subchron (2n), respectively. At Sites 981 and 982, magnetization intensities decrease sharply in the normal polarity zone corresponding to the Gauss Chron (2An), and magnetic stratigraphies below this level could not be resolved. At Site 984, the resolution of magnetic stratigraphy was curtailed at ~250 meters below seafloor (Olduvai Subchron) by core deformation at the base of the APC section and in the underlying extended core barrel section. As the magnetic stratigraphies at all four sites are unequivocal, polarity chron interpretations can be made without aid from the biostratigraphy. Mean sedimentation rates within polarity chrons have been calculated and Pliocene-Pleistocene biomagnetostratigraphic correlations tested.

The effects of restraining boundaries on the passive resistance of sand; results of a series of tests with a medium-scale testing apparatus. Report submitted to the Office of Naval Research, Dept. of the Navy,

"Project No. Nr-081-117. Contract No. Nonr-100 9(00)"

Shore and sea boundaries : with special reference to the interpretation and use of Coast and Geodetic Survey data.

Vol. 3 by: Michael W. Reed.

Drainage basins of streams entering the Hudson River in Orange, Ulster, Dutchess and Putnam Counties, except Rondout Creek below Rondout Reservoir, Esopus Creek below Ashokan Reservoir, Wappinger Creek, and waters contained within boundaries of State-owned forest preserve lands; official classifications.

Cover title.

Boundaries of the United States and of the several states and territories,

Mode of access: Internet.

FCC record : a comprehensive compilation of decisions, reports, public notices, and other documents of the Federal Communications Commission of the United States.

Latest issue consulted: Vol. 22, no. 28 (Dec. 10-Dec. 31, 2007).

How to use your VHF marine radio : FCC rules for recreational boaters /

Mode of access: Internet.

Methods for estimating peak discharge and flood boundaries of streams in Utah /

624-B

Estimation of natural streamflow in the Jemez River at the boundaries of Indian lands, central New Mexico /

Bibliography: p. 24-25.

Successful preparation for FCC radio operator license examinations

Previously published under title: Answers to radio operating questions.

Parliamentary representation; further return to an address to His Majesty, dated 12 December, 1831; for copies of instructions given by the Secretary of State for the Home department with reference to Parliamentary representation; likewise copies of letters of reports received by the Secretary of state for the Home department in answer to such instructions. Reports from Commissioners on proposed division of counties and boundaries of boroughs ...

At bottom of t.p.: 141.

Boundaries, areas, geographic centers and altitudes of the United States and their several states, with a brief record of important changes in their territory and government,

"A revision and enlargement of Bulletin 226...was...issued in 1923 as Bulletin 689. The present bulletin is a revision and enlargement of the 1923 edition"--Foreword, p. vii.

Travels in the United States of America and Canada, containing some account of their scientific institutions, and a few notices of the geology and mineralogy of those countries. To which is added, an essay on the natural boundaries of empires.

Errata slip inserted.