This page is dedicated to the memory of Carol Thilenius, Juneau, Alaska, 1935-2008

Carol Thilenius was born in 1935 in La Grande.Oregon. She was a graduate of La Grande High School. She was a science teacher, a professional weaver, and marine biologist of considerable skill.

Carol was a very accomplished weaver, and shared her talents by teaching hand weaving at the University of Alaska Southeast in Juneau for many years. Later she became interested in geology, microfossils, and botany. She audited numerous university Earth and Life Science courses at UAS to expand her knowledge.

She with her husband and USFS researcher John Thilenius, traveled extensively in Africa, South and Central America and Australia, collecting plants, shells, and sand along the way. She was a Juneau resident for 31 years and spent many hours sampling the early Holocene Gastineau Formation in the Auke Bay and greater Juneau area. She screened these collected glaciomarine sediments for shells and microfossils, and next identified and photographed them in her home lab.

With the help of UAS ENVS graduate Daniel Bleidorn, she assembled her results for these web pages. She was an excellent field researcher, meticulous lab worker, and amazing scientist, and is very much missed. (Cathy Connor, Professor of Geology Emerita, UAS, July 23, 2020)

Tapestry in Three Parts of Indian Cove, Auke Bay Alaska Woven by Carol Thilenius 1990’s.

Tapestry in Three Parts of Indian Cove, Auke Bay Alaska Woven by Carol Thilenius 1990’s.

The following is from the original website hosted here at UAS.

The fossils in the Gastineau Channel Formation were deposited in water that was shallow (less than 150 feet), saline to brackish (35 to 27 %) and cold (0° C to 10° C). Miller (1973), Smith (1961) and Todd & Low (1967) came to this conclusion based on the tolerances of the species commonly present. Elphidium clavatum was the most abundant and wide spread foraminifera. It tolerates variations in temperature and salinity but not greater depth. Other commonly occurring forams, while tolerant of greater depth, were less tolerant of greater temperature and salinity variations.

   Isostatic rebound has lifted Gastineau Channel Formation deposits above sea level, in some places as much as 750 feet. The highest sample taken in this study was at 300 feet above current sea level. The radiocarbon age of shell material reported by Miller (1975) was 9,500 yr BP to 12,000 yr BP.

    Sampling this formation was of necessity opportunistic. The material ranged from muddy gravel to muddy sand to sandy clay. Much of it was readily eroded. Banks exposed by road construction were later stabilized by rocks and vegetation. Material dug up to set power poles was often rich in fossils but soon vegetated. Some very solid clay samples were in streams and only available at low water. Ditch cleaning by the road department exposed some sites that would have been missed otherwise.

    Macro fossils were picked from the surface when exposed and from the screens used to process the foraminifera samples. Approximately a cup (200— 300 g. dry weight) of blue—gray sandy mud was dried then rewetted to soften the clods. The material was washed through four screens with sizes and mesh openings of #18 (1.0 mm), #35 (0.5 mm), #70 (0.212. mm) and #140 (0.106 mm).
    The material from each screen was examined under a dissecting microscope. Forams and other microfossils were picked and identified. A sample size of over 200 forams was considered adequate to characterize the site. Some samples had fewer than 200 and many had more.

    The sample sites in this study showed a range of habitats from a high energy site with strong currents to moderate energy sites and low energy sites with deposition instill water. Diversity was greatest in the low energy sites and moderate to low in the moderate energy sites. The single high energy site had species adapted to live in stronger currents.

    Following are sections on the macrofossils, foraminifera and descriptions of the sample sites. The bibliography includes references on the Gastineau Channel Formation and keys used to identify the fossils.

Marine Fossils of the Gastineau Channel Formation

BIVALVIA
   Astarte alaskensis Dall
   Astarte montagul (Dillwyn)
   Chlamys rubida (Hinds)
   Clinocardium ciliata (Fabricius)
   Cyclocardita ventricosa (Gould)
   Hiatella arctica (Linnaeus)
   Macoma brota Dall
   Macoma calcarea(Gmelin)
   Macoma obliqua (Sowerby)
   Mya truncata Linnaeus
   Mytilus edulis

Nucula tenuis (Montagu)
   Nuculana fossa (Baird)
   Nuculana minuta (Fabricius)
   Nuculana pernula (Muller)
   Parvamussium alaskensis (Dall)
   Protothaca staminea (Conrad)
   Saxidomus gigantea (Deshayes)
   Serripes groenlandicus (Bruguiere)
   Tresus capax (Gould)

GASTROPODA
   Acmaea mitra Rathke
   Admete couthouyi (Jay)
   Boreotrophon beringi (Dall)
   Buccinum kadiakense Dall
   Colus halli Dall
   Cryptobranchia concentrica(Middendorff)
   Cylichna alba (Carpenter)
   Fusitriton oregonense (Redfield)
   Natica clausa Broderip & Sowerby
   Neptunea lyrata Gmelin
   Nucella canaliculata (Duclos)
   Nucella lamellosa (Gmelin)
   Ocenebra lurida (Mlddendorff)
   Oenopta harpularia (Couthouy)
   Puncturella galeata (Gould)
   Tectura persona (Rathke)
   Trichotropis borealis Broderip & Sowerby
   Trichotropis cancellata Hinds
CRUSTACEA
   Balanus nubilis Darwin
   Balanus spp.
   Ostracoda
BRACHIOPODA
   Laqueus californianus (Koch)
POLYCHAETA
   Serpula vermicularis Linnaeus
   Sinistrella sp.
   Spirorbissp.
BRYOZOA
   Heteropora alaskensis (Borg
   Bryozoa spp
ECHINODERMATA.
   Urchin fragments
PORIFERA
   Spicules
   Spicula matrix

Foraminifera

FAMILY
Saccamminidae
Saccamina difflugiformis (Brady)
Reophacidae
Reopax insectus (Goes)

Lituolidae
Recurvoides turbinatus (Brady)
Valvulinidae
Eggerella advena (Cushman)
Miliolidae
Quinqueloculina agglutina Cushman
Quinqueloculina akneriana d’Orbigny
Quinqueloculina arctica Cushman
Quinqueloculina stalkerl Loebflch & Tappan
triloculina trihedra Loeblich & Tappan
Pyrgo lucernula (Schwager)
Opthalmidiidae
Cornuspira involvens (Reuss)
Lagenidae
Dentaliria baggi Galloway & Wissler
Laevidentalina californica (Cushman & Gray)
Lagena distoma Parker & Jones
Lagena gracillima (Seguenza)
Lagena laevis (Montagu)
Lagena meridionalis Wiesner
Lagena mollis (Cushman)
Lageria parri Loeblich & Tappan
Lagena semilineata Wright
Lagena setigera Wright
Lagena striata (d’Orbigny)
Lagena tenuis (Bornemann) var. Ornata Reuss
Procerolagena complurecosta (Patterson)
Pollymorphinidea
Laryngosigma hyalascida Loeblich & TappanBuliminidae
Buliminella subfusiformis Cushman
Globobulimina aurculata ssp arctica (Bailey)
Virgulina fusiformis (Williamson)
Bolivina decussata Brady
Bolivina pacifica Cushman & McCulloch
Fissurina cucurbitasema Loeblich & Tappan
Fissurina lucida (Williamson)
Fissurina marginata (Montagu)
Oolina apiopleura (Loeblich & Tappan)
Oolmna laevigata d’Orbigny
Oolina melo d’Orbigny
Oolina striatopunctata (Parker & Johnson)
Angulogerina fluens Todd
Spirillinidae
Patellina corrugata Williamson
Rotalidae
Buccella frigida (Cushman)
Buccella tenerrima (Brady)
Epistominella pacifica (Cushman)
Epistominella vitrea Parker
Elphidiidae
Elphidiella nitida Gushman
Elphidium clavatum Cushman
Elphidium frigidum Cushman
Elphidium oregonense Cushman&Grant Anomalinidae
Cibicides lobatulus (Walker&Jacob)
Nonionidae
Nonion labradoricum (Dawson)



Bibliographic Reference

Knopf, Adolph, 1912, The Eagle River region, southeastern Alaska: U.S. Geological Survey Bulletin 502, 61 p., 3 sheets. PDF and MAP

Buddington, A.F., and Chapin, Theodore, 1929, Geology and mineral deposits of southeastern Alaska: U.S. Geological Survey Bulletin 800, 398 p., 2 sheets, scale 1:500,000. PDF and MAP

Lemke, R.W., and Yehle, L.A., 1972, Reconnaissance engineering geology of the Haines area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 72-229, 109 p., 2 sheets, scale 1:24,000. PDF and MAP

Lemke, R.W., and Yehle, L.A., 1972, Reconnaissance engineering geology of the Haines area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open File Report: Technical Data Unit classification number 515, 109 p., 2 sheets. LINK

Lemke, R.W., and Yehle, L.A., 1972, Regional and other general factors bearing on evaluation of earthquake and other geologic hazards to coastal communities of southeastern Alaska: U.S. Geological Survey Open-File Report 72-230, 99 p. PDF

Lemke, R.W., 1974, Reconnaissance engineering geology of the Wrangell area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 74-1062, 103 p., 1 sheet, scale 1:7,200. PDF and MAP

Lemke, R.W., 1974, Reconnaissance engineering geology of the Wrangell area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open File Report: Technical Data Unit classification number 596, 103 p. LINK

Lemke, R.W., 1975, Reconnaissance engineering geology of the Ketchikan area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 75-250, 65 p., 1 sheet, scale 1:63,360. PDF and MAP

Miller, R.D., 1972, Surficial geology of the Juneau urban area and vicinity, Alaska, with emphasis on earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 72-255, 108 p., 7 sheets, scale 1:24,000. PDF and MAP

Miller, R.D., 1973a. Two diamictons in a landslide scarp on Admiralty island, Alaska, and the tectonic insignificance of an intervening peat bed. Journal of Research of the US Geological Survey1(3), pp.309-314. PDF

Miller, R.D., 1973b, Gastineau Channel Formation, a composite glaciomarine deposit near Juneau, Alaska: U.S. Geological Survey Bulletin 1394-C, p. C1-C20. PDF

Miller, R.D., 1975, Surficial geologic map of the Juneau urban area and vicinity, Alaska: U.S. Geological Survey Miscellaneous Investigations Series Map 885, 1 sheet, scale 1:48,000. MAP

Twenhofel, W.S., 1952. Recent shore-line changes along the Pacific coast of Alaska. American journal of Science250(7), pp.523-548. PDF

Yehle, L.A., and Lemke, R.W., 1972, Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 72-454, 108 p., 4 sheets, scale 1:96,000. PDF and MAP

Yehle, L.A., and Lemke, R.W., 1972, Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open File Report: Technical Data Unit classification number 550, 108 p., 4 sheets. LINK

Yehle, L.A., 1974, Reconnaissance engineering geology of Sitka and vicinity, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 74-53, 104 p., 3 sheets. PDF and MAP

Yehle, L.A., 1978, Reconnaissance engineering geology of the Petersburg area, southeastern Alaska, with emphasis on geologic hazards: U.S. Geological Survey Open-File Report 78-675, 92 p., 2 sheets. PDF and MAP

Yehle, L.A., 1979, Reconnaissance engineering geology of the Yakutat area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Professional Paper 1074, 44 p., 1 sheet, scale 1:63,360. PDF and MAP

Station Location/
Sites

Station Locations 

Montana Creek Trail
Montana Creek Bridge Series
Auke Bay School, Back of Cave
  Auke Bay School, Bank below Cave
  Auke Bay School, Bank below playground
  Spalding Trail Parking Lot
13870 Glacier Highway
  Eastside 13870 Glacier Highway
  Stream bank east of 13870 Glacier Highway
Auke Rec By-Pass
Auke Village Sign
  Otter Drive #3
  Auke Rec
  Auke Rec Stream Bottom
Otter Drive-Glacier Highway Power Pole
  Otter Drive#1, #2
  3189 National Park Road
North Douglas Highway
Power pole #1, #2, #3, #4, #5
10 Petersen Creek
11 Salmon Creek Trail #1, #2
12 Salmon Creek Trail #3, #4
13 Thane Road
14 Glory Hole #5

Caral at work in the field.jpg
 
Site Locations

Site Locations