1-6 OF 6 RESULTS FOR

Third Watchung Mountain

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Journal: GSA Bulletin
Published: 01 January 1980
GSA Bulletin (1980) 91 (1_Part_II): 156–191.
... cut into the relatively soft mudstones. Stratigraphically from bottom to top, the three ridges are known as the First, Second, and Third Watchung Mountains and average 183, 229, and 91 m thick, respectively (Faust, 1975). A fourth basalt ridge located west of the Third Watchung was recognized by Black...
Journal Article
Journal: Geology
Published: 01 September 2000
Geology (2000) 28 (9): 859–862.
...) . Incremental-heating data for sample 6J from the Orange Mountain flow (Watchung flow I) follow a pattern suggestive of radiogenic Ar loss to eight contiguous steps that define a plateau age of 201.0 ± 2.1 Ma (the complete intralaboratory uncertainties are stated at the 2 σ confidence level). Sample 7B...
FIGURES
Journal Article
Published: 01 September 2001
The Journal of Geology (2001) 109 (5): 585–601.
...John H. Puffer; Richard A. Volkert Abstract Coarse-grained segregations are found in several subaerial flows of Jurassic flood basalts in the Watchung Mountains, New Jersey. They are particularly common within a 140–180-m-thick quartz-tholeiitic Preakness flow, the thickest of the Watchung flows...
FIGURES | View All (9)
Journal Article
Published: 01 March 2009
The Journal of Geology (2009) 117 (2): 139–155.
....  Stratigraphy of the Triassic and Jurassic rocks of the Newark Basin, New Jersey and New York. The Orange Mountain, Preakness, and Hook Mountain basalts are referred to by Olsen ( 1980 ) as the basalt formations of the Newark Basin but are informally known as the Watchung basalts. Bulk analyses...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1977
AAPG Bulletin (1977) 61 (1): 79–99.
... of the basins varies slightly, apparently controlled by local grain of the Variscan basement. The northeasterly trend continues southwestward onto the African platform where a long trough parallels the Mauritanide mountain chain. Westernmost Moroccan basins lie within 150 km of the outer edge of the continental...
FIGURES | View All (5)
Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.256.01.13
EISBN: 9781862395046
...) came to the attention of the Museum's third president Morris Ketchum Jesup (1830–1908) in the early 1890s. Jesup (Fig. 4 ) served from 1881 to 1908, and formed the Peary Arctic Club to finance and publicize Lieutenant, later Commander, Peary's expeditions. Jesup facilitated Peary's leave from the Navy...
FIGURES | View All (11)