Map of the Huron River Valley from Surveys made in 1908-1909 by G. S. Williams. 5118 [Hudson Mills]

Hudson Mills, 1908: Map of the Huron River Valley [Scanned in two parts and combined using PhotoShop CS6 PhotoMerge command]

Map of the Huron River Valley from Surveys made in 1908-1909 by G. S. Williams. 5117 [Between Dexter and Hudson Mills]

Between Dexter and Hudson Mills, 1908: Map of the Huron River Valley [Scanned in two parts and combined using PhotoShop CS6 PhotoMerge command]

Map of the Huron River Valley from Surveys made in 1908-1909 by G. S. Williams. 5116 [Between Dexter and Hudson Mills]

Between Dexter and Hudson Mills, 1908: Map of the Huron River Valley [Scanned in two parts and combined using PhotoShop CS6 PhotoMerge command]

Henry Hudson; captain of ice-bound seas.

Mode of access: Internet.

Amended act of incorporation of the Hudson River railroad company, by-laws and extracts from revised statutes, &c., &c.

Mode of access: Internet.

Annual report of the Delaware and Hudson Company ...

Report year ends Dec. 31.

Henry Hudson the navigator : the original documents in which his career is recorded, collected, partly translated, and annotated with an introduction /

Mode of access: Internet.

History of the captivity of Napoleon at St. Helena; from the letters and journals of the late Lieut.-Gen. Sir Hudson Lowe, and official documents not before made public.

Mode of access: Internet.

Report on the Dominion of Canada government expedition to the Arctic islands and Hudson strait on board the D. G. S. 'Arctic' [1908-1909]

Mode of access: Internet.

Origin of the Archean Sask craton and its extent within the Trans-Hudson orogen: evidence from Pb and Nd isotopic compositions of basement rocks and post-orogenic intrusions

U-Pb zircon ages from the exposed Sask craton are 2450-3100 Ma, from the Peter Lake Domain 2575-2640 Ma, and from rocks of the Trans-Hudson orogen 1840-1880 Ma. U-Pb monazite and zircon ages of post-orogenic pegmatites and aplites are 1770-1800 Ma. Common Pb and Sm-Nd isotopic compositions of post-orogenic intrusions, as probes of crust beneath the orogen, were compared to Sask craton rocks and ca. 1850 Ma orogenic rocks to infer the origin and subsurface distribution of the Sask craton within the internides of the Trans-Hudson orogen. Results show that post-orogenic intrusions within most of the Glennie Domain and Hanson Lake block were derived, at least in part, from Archean source materials, demonstrating that the Sask craton lies beneath Paleoproterozoic orogenic rocks present at the surface. In contrast, common Pb and Sm-Nd isotopic compositions from pegmatites and aplites of the La Ronge Domain are essentially identical with those of the Paleoproterozoic orogenic rocks into which they are intruded, indicating derivation by partial melting of similar rocks. Thus, if the Sask craton extended to the west beneath the La Ronge Domain, it was beneath the zone of melting that produced the post-orogenic intrusions, making it unlikely that the Sask craton is a detached part of the Hearne craton. Many samples from the Sask craton have elevated Pb-208/Pb-204 ratios, unlike Superior craton or Hearne craton rocks, suggesting that the Sask craton was derived from an exotic source, such as the Wyoming craton, which shares similar elevated Pb-208/Pb-204 ratios.

Hudson v DWP 2012

Case law report - online

Annotated record of the detailed examination of Mn deposits from C.S.S. Hudson Cruise 19 (1967) stations

The Bedford Institute of Oceanography provided ship time on the C.S.S. Hudson during the B.I.0. 1967 Metrology and IODAL Cruise for surveying two separate bottom features in the North Atlantic; the Flemish Cap and the San Pablo Seamount one of the Kelvin Seamounts (also known as the New England Seamounts) about 400 miles SSE of Halifax, Nova Scotia. Underwater photography, dredging, and drilling showed San Pablo seamount to have a very considerable covering of manganese deposit, which may be recoverable by mining. San Pablo Seamount was surveyed and sampled; good hauls were made both on the top and on the slopes, at various depths from 500-1000 fathoms; in all cases samples of an unusual stratified manganese-iron ore were recovered. In the hope of gaining additional information in the immediate sample area, one of the dredges had been previously modified to accommodate underwater photographic equipment. X-ray chemical analyses indicate that the ore contains 20 to 25 per cent MnO2, with similar amounts of Fe2O3. Since bottom photographs indicate that these deposits form a continuous cover 1 foot to 3 feet thick over most of the seamount, it is estimated that there are ore reserves in the order of 10 to 30 M tons above 1,000 fathoms.