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Bendeleben Mountains

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Journal Article
Published: 13 June 2003
Canadian Journal of Earth Sciences (2003) 40 (6): 865–886.
... relations and 40 Ar/ 39 Ar geochronology bracket the dike ages between 90 and 84 Ma. Diabase dikes in the York Mountains are associated with normal faults that strike east–west to east-northeast. Dikes in the Bendeleben Mountains are both mafic and felsic, but their orientations are unknown. Alkalic dikes...
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Simplified geologic map of Seward Peninsula, showing location of the York Mountains (YM), Kigluaik Mountains (KM), Bendeleben Mountains (BM), Darby Mountains (DM), and Cape Nome (CN). The analyzed samples are also shown; see Table 1 for sample list. Geology is after Beikman (1980), Till et al. (1986), and Amato et al. (2004). See Figure 1 for map location.
Published: 01 September 2009
Figure 2 Simplified geologic map of Seward Peninsula, showing location of the York Mountains (YM), Kigluaik Mountains (KM), Bendeleben Mountains (BM), Darby Mountains (DM), and Cape Nome (CN). The analyzed samples are also shown; see Table 1 for sample list. Geology is after Beikman (1980
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Summary of data pertaining to Cretaceous to Recent extension directions in the Bering Strait region. BM, Bendeleben Mountains; DM, Darby Mountains; KD, Koolen dome; KM, Kigluaik Mountains; NU, Neshkan uplift; STL, St. Lawrence Island; SU, Senyavin uplift; YM, York Mountains. Sources include Miller and Hudson (1991), Plafker et al. (1994), BSGFP (1997), Miller et al. (2002b), and Klemperer et al. (2002). See text for details.
Published: 13 June 2003
Fig. 13. Summary of data pertaining to Cretaceous to Recent extension directions in the Bering Strait region. BM, Bendeleben Mountains; DM, Darby Mountains; KD, Koolen dome; KM, Kigluaik Mountains; NU, Neshkan uplift; STL, St. Lawrence Island; SU, Senyavin uplift; YM, York Mountains. Sources
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Model for Cretaceous tectonic evolution of Seward Peninsula. Large arrows indicate direction of tectonic transport. Pre-120 Ma: north-south convergence produces blueschist-facies assemblages in the Nome Group. 110–90 Ma: east–west lineations may have formed during extension at deeper crustal levels, coeval with north–south extension recorded by lineations in the Nome Group and possibly coeval with north–south extension recorded by undated east–west normal faults and dikes in the York Mountains. 90–80 Ma: northeast-striking dikes in the Kigluaik and Darby mountains formed during northwest extension. 80 Ma and younger: east-west dikes in the York Mountains and normal faults in the Kigluaik and Bendeleben mountains record north–south extension.
Published: 13 June 2003
northwest extension. 80 Ma and younger: east-west dikes in the York Mountains and normal faults in the Kigluaik and Bendeleben mountains record north–south extension.
Journal Article
Journal: GSA Bulletin
Published: 01 September 2009
GSA Bulletin (2009) 121 (9-10): 1219–1235.
...Figure 2 Simplified geologic map of Seward Peninsula, showing location of the York Mountains (YM), Kigluaik Mountains (KM), Bendeleben Mountains (BM), Darby Mountains (DM), and Cape Nome (CN). The analyzed samples are also shown; see Table 1 for sample list. Geology is after Beikman (1980...
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Index map of the Seward Peninsula, showing the high-grade metamorphic culminations (gneiss domes) flanked by lower grade metamorphic rocks in the Kigluaik, Bendeleben, and Darby mountains. The York Mountains area exposes only low-grade to unmetamorphosed rocks. Cretaceous plutonic rocks in each area are also shown. Dike swarms in each area are displayed in larger scale maps as indicated in the figure.
Published: 13 June 2003
Fig. 2. Index map of the Seward Peninsula, showing the high-grade metamorphic culminations (gneiss domes) flanked by lower grade metamorphic rocks in the Kigluaik, Bendeleben, and Darby mountains. The York Mountains area exposes only low-grade to unmetamorphosed rocks. Cretaceous plutonic rocks
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Simplified geologic map of the Seward Peninsula, modified from Till et al. (2011). Location and orientation of folds of foliation within the Nome Complex are shown. Plutonic rocks, which are most voluminous in the Kigluaik, Bendeleben, and Darby Mountain ranges, are not shown. For location of figure, see Figure 2.
Published: 01 June 2016
Figure 6. Simplified geologic map of the Seward Peninsula, modified from Till et al. (2011) . Location and orientation of folds of foliation within the Nome Complex are shown. Plutonic rocks, which are most voluminous in the Kigluaik, Bendeleben, and Darby Mountain ranges, are not shown
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 June 2016
Lithosphere (2016) 8 (3): 219–237.
...Figure 6. Simplified geologic map of the Seward Peninsula, modified from Till et al. (2011) . Location and orientation of folds of foliation within the Nome Complex are shown. Plutonic rocks, which are most voluminous in the Kigluaik, Bendeleben, and Darby Mountain ranges, are not shown...
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Journal Article
Published: 01 June 1980
Bulletin of the Seismological Society of America (1980) 70 (3): 873–883.
... Mountain, and traverses the epicentral area of the 1950 earthquake (m~ = 6.5). About 75 to 100 km to the west of this zone, a second trend in seismicity (I-I) cuts across the Bendeleben-Kigluaik mountain 173 ° 165 o 69 ° 69 ° '~ ANTICLINE SYNCLINE THRUST FAULT NORMAL FAULT FAULT TRACE RIDGE AND BASIN AXIS...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1974
AAPG Bulletin (1974) 58 (8): 1506–1517.
... field studies. Multipurpose geologic mapping and field studies were conducted throughout the State, including southeastern Alaska in the Craig, Ketchikan, and Juneau areas; in southern Alaska in the Chugach Mountains and Prince William Sound area; in central Alaska in the Wrangell Mountains, eastern...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1982
AAPG Bulletin (1982) 66 (3): 255–285.
... and then divided by total length of all faults. Circle in each diagram represents 10% of that total length. The most evident high-angle faults on the Seward Peninsula are two major normal faults that strike nearly east and bound the Kigluaik and Bendeleben Mountains ( Fig. 1 ; Hudson and Plafker, 1978...
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Journal Article
Published: 27 January 2016
Canadian Journal of Earth Sciences (2016) 53 (3): 260–280.
... of granitoids from an uplifted fault block in the Bendeleben Mountains that they also ascribe to extensional faulting, offshore basin development, and erosion. Both Dumitru et al. (1995) and McDannell et al. (2014) propose that Paleogene extension, exhumation, and block rotation induced by tectonic...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1970
AAPG Bulletin (1970) 54 (6): 1070–1083.
... geologic mapping to provide a basis for the interpretation of geochemical anomalies. Continuing metal resource investigations that functioned in 1969 included the Hogatza trend, Seward Peninsula, southwest Alaska, central, southern and eastern Alaska Range, Talkeetna Mountains, Yukon-Tanana, Livengood...
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Journal Article
Journal: GSA Bulletin
Published: 03 July 2024
GSA Bulletin (2025) 137 (1-2): 241–258.
...., 2014 ). Traverses, geologic mapping, and sampling were carried out in the Mount Distin area ( Fig. 3 ), southwest of upper Salmon Lake ( Fig. 4 ), and the Anvil Mountain–Newton Peak area just north of Nome ( Fig. 5 ). We found similar lithologic units, structural relations, and lithologic interlayering...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1973
AAPG Bulletin (1973) 57 (8): 1406–1420.
... these beds on the continental slope north of Barrow. Field studies were continued in the several mineralized districts of Alaska, including geologic mapping at a scale of 1:63,360 in the Prince of Wales Island region, Talkeetna Mountains, Western Chugach Mountains, Wrangell Mountains, eastern Alaska...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1974
AAPG Bulletin (1974) 58 (1): 79–105.
... the subject of extensive discussion and speculation for many years. Since the early work of Mertie (1930c) the structural grain as delineated by major faults, axes of mountain ranges, and trends of outcrops has been used as a basis for conjecture ( Payne, 1955 ; Gates and Gryc, 1963 ; Grantz, 1966...
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Journal Article
Published: 10 January 2025
Canadian Journal of Earth Sciences (2025) 62 (4): 725–757.
... . Geological Society of America . doi: 10.1130/2022.1220(30) . McDannell , K.T. 2011 . Exhumation in the Bendeleben Mountains (Seward Peninsula, Alaska) constrained by (U–Th)/He thermochronology. M.S. Thesis , University of West Virginia , Morgantown, WV . McElhinny , M.W. 1964...
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Journal Article
Journal: Economic Geology
Published: 01 November 2009
Economic Geology (2009) 104 (7): 945–960.
..., and fine-grained clastic sedimentary strata of Ordovician through Mississippian age that deposited in a shallow-water platform environment. The York section bears similarities in lithofacies and biofacies to the metacarbonate sequence of the Baird Mountains in the western Brooks Range 300 km...
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Journal Article
Published: 01 December 2016
Russ. Geol. Geophys. (2016) 57 (12): 1668–1687.
... constraints on Late Cretaceous to Cenozoic exhumation of the Bendeleben Mountains, Seward Peninsula, Alaska . Geochem. Geophys. Geosyst. 15 , 4009 – 4023 , doi: https://doi.org/10.1002/2014GC005424 . McWhae , J.R. , 1986 . Tectonic history...
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Journal Article
Journal: Geosphere
Published: 25 July 2022
Geosphere (2022) 18 (5): 1492–1523.
... Mountains allochthon, which is characterized by thick siliciclastic strata of Devonian–Mississippian age ( Mayfield et al., 1988 ; Moore et al., 1994 ; Dumoulin et al., 2004 ). The next highest sheet is the Picnic Creek allochthon, which includes Carboniferous rocks representative of deep-water facies...
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