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Tamme Cliffs

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Gyroptychius milleri from the Tamme Cliffs of Estonia: (a) photograph of GIT 365-151; (c) line drawing of GIT 365-151; (b) reproduction of the same specimen by Vorobyeva (1977, fig. 29B). Scale bars 10 mm.
Published: 14 August 2015
Fig. 2. Gyroptychius milleri from the Tamme Cliffs of Estonia: ( a ) photograph of GIT 365-151; ( c ) line drawing of GIT 365-151; ( b ) reproduction of the same specimen by Vorobyeva (1977 , fig. 29B). Scale bars 10 mm.
Journal Article
Published: 22 September 2017
Scottish Journal of Geology (2017) 53 (2): 63–69.
...Michael J. Newman; Jan L. Den Blaauwen; Tormi Tuuling Abstract A coccosteid nuchal bone from the Middle Devonian Tamme Cliffs locality in Estonia is described as Dickosteus cf. threiplandi , D . threiplandi being a common species in the Middle Devonian of the Orcadian Basin, Scotland. A number...
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Image
Gyroptychius milleri from the Devonian of Estonia: (a) GIT 365-165 from Tamme Cliffs in the Kureküla Member; (b) GIT 365-203 from Aruküla Caves in the Viljandi Member. All scale bars 10 mm.
Published: 14 August 2015
Fig. 1. Gyroptychius milleri from the Devonian of Estonia: ( a ) GIT 365-165 from Tamme Cliffs in the Kureküla Member; ( b ) GIT 365-203 from Aruküla Caves in the Viljandi Member. All scale bars 10 mm.
Image
(a) ?Dickosteus sp. GIT 117-8, the anterior third of a right ADL plate from the Tamme Cliffs, Estonia. (b) Dickosteus threiplandi NMS G.2016.22.1, right ADL plate (electronically vertically mirrored) from Marwick Bay, Orkney. (c) Line drawing of a right ADL plate of Coccosteus cuspidatus from Miles & Westoll (1968, fig. 30a). Scale bars 10 mm.
Published: 22 September 2017
Fig. 4. ( a ) ? Dickosteus sp. GIT 117-8, the anterior third of a right ADL plate from the Tamme Cliffs, Estonia. ( b ) Dickosteus threiplandi NMS G.2016.22.1, right ADL plate (electronically vertically mirrored) from Marwick Bay, Orkney. ( c ) Line drawing of a right ADL plate of Coccosteus
Image
Gyroptychius milleri from the Devonian of Scotland and Estonia: (a) BGSE 1224 from Scrabster Hill, Caithness, Scotland; (b) GIT 365-151 from Tamme Cliffs, Estonia; (c) NMS G.2014.4.1 from Point of Buckquoy, Orkney, Scotland; (d) BGSE 10444 from Samuel Geo, Caithness, Scotland; (e) GIT 365-203 from Aruküla Caves, Estonia; (f) BGSE 10445 from Samuels Geo, Caithness, Scotland. All scale bars 10 mm.
Published: 14 August 2015
Fig. 3. Gyroptychius milleri from the Devonian of Scotland and Estonia: ( a ) BGSE 1224 from Scrabster Hill, Caithness, Scotland; ( b ) GIT 365-151 from Tamme Cliffs, Estonia; ( c ) NMS G.2014.4.1 from Point of Buckquoy, Orkney, Scotland; ( d ) BGSE 10444 from Samuel Geo, Caithness, Scotland
Image
(a) Right PDL plate (electronically mirrored horizontally) mostly in visceral view of ?Dickosteus sp. specimen TUG 741-93 from Tamme Cliffs, Estonia. (b) Line drawing of the outer surface of a Coccosteus cuspidatus left PDL plate from Miles (1966, fig. 13B). (c) The outer surface of Dickosteus threiplandi left PDL plate specimen NMS G.1872.2.12A from Aimster, Caithness. (d) Line drawing from Miles (1966, fig. 13A) of NMS G.1872.2.12A. Scale bars 10 mm.
Published: 22 September 2017
Fig. 3. ( a ) Right PDL plate (electronically mirrored horizontally) mostly in visceral view of ? Dickosteus sp. specimen TUG 741-93 from Tamme Cliffs, Estonia. ( b ) Line drawing of the outer surface of a Coccosteus cuspidatus left PDL plate from Miles (1966 , fig. 13B). ( c ) The outer
Image
Nuchal plates: (a, b), TUG 1360-50 Dickosteus cf. threiplandi from the Tamme Cliffs, Estonia, (a) outer view, (b) visceral view; (c, d) NMS G.2016.22.2 Dickosteus threiplandi from the north side of Marwick Head, Orkney, (c) outer view, (d) visceral view. C.cf, area overlapping the central plate; ch.rd.PNu, channel for the ridges of the paranuchal plate; C.oa, area overlapped by the central plates; la.dsp, posterior descending lamina of the nuchal plate; Nu.pmc, posterior median cusp of the nuchal plate; Nu.p.pts, paired pits of the visceral surface of the nuchal plate; PNu.cf, area overlapping the paranuchal plate; PNu.oa, area overlapped by the paranuchal plate. Scale bars 10 mm.
Published: 22 September 2017
Fig. 2. Nuchal plates: ( a , b ), TUG 1360-50 Dickosteus cf. threiplandi from the Tamme Cliffs, Estonia, (a) outer view, (b) visceral view; ( c , d ) NMS G.2016.22.2 Dickosteus threiplandi from the north side of Marwick Head, Orkney, (c) outer view, (d) visceral view. C.cf, area
Journal Article
Published: 14 August 2015
Scottish Journal of Geology (2015) 51 (2): 141–147.
...Fig. 2. Gyroptychius milleri from the Tamme Cliffs of Estonia: ( a ) photograph of GIT 365-151; ( c ) line drawing of GIT 365-151; ( b ) reproduction of the same specimen by Vorobyeva (1977 , fig. 29B). Scale bars 10 mm. ...
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Journal Article
Journal: Geology
Published: 01 April 2008
Geology (2008) 36 (4): 291–294.
...- 39 Ar formation age. We therefore suggest that Transantarctic Mountain microtektites (TAMM) define the southern extension of the Australasian strewn field. The margin of the Australasian strewn field is thus shifted southward by ~3000 km and the maximum distance from the putative parent impact site...
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Journal Article
Published: 01 April 2000
Clays and Clay Minerals (2000) 48 (2): 238–245.
...-rock interactions in low-temperature acid-weathering systems. Previous successful applications were made to acid volcanic lakes and high-temperature fumarolic environments ( Delmelle and Bernard, 1994 ; Africano and Bernard, 2000 ). Studied outcrops are located in the sea cliffs west...
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Journal Article
Published: 01 February 1988
Quarterly Journal of Engineering Geology and Hydrogeology (1988) 21 (1): 33–57.
... of surface retreat of sea-cliffs, based on dated inscriptions. Science, 93 , 617 – 618 . Emery, K. O. 1960 . Weathering of the Great Pyramid. Journal of Sedimentary Petrology, 30 , 140 – 143 . Fookes, P. G. 1980 . An introduction to the influence of natural aggregates...
Journal Article
Published: 01 September 2020
South African Journal of Geology (2020) 123 (3): 343–356.
... an origin by recycling of Palaeoproterozoic (Waterberg, Soutpansberg and Pretoria groups) and Phanerozoic (Karoo Supergroup) cover successions. The latter is dominant in the south and east (Boane, Mahosi, Chilojo Cliffs), and the Palaeoproterozoic sources in the northwest (Pafuri, Wright’s Tower, Masisi...
FIGURES
Journal Article
Published: 01 June 2013
Italian Journal of Geosciences (2013) 132 (2): 254–262.
... of web-shared geological knowledge. Besides the INSPIRE initiative, technical and scientific standards are also developed in the frame of geological DB network both at national (e.g. the U.S. National Geologic Map Database; S oller & S tamm , 2009 ) and global level (e.g. the GEON...
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Journal Article
Published: 28 March 2025
Reviews in Mineralogy and Geochemistry (2025) 91A (1): 413–456.
... extraction method; the method of Mehra and Jackson (1960) is employed. Rennert et al. (2021) note that oxalate extraction has been used for approximately 100 years to extract elements from reactive oxide components of soils, citing the work of Tamm (1922) to extract Al, Fe, Si, and Ti with an ammonium...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 2004
AAPG Bulletin (2004) 88 (5): 587–611.
... and biosynthesis-geochemical biotechnological importance , in W. Hertz , G. W. Kirby , R. E. Moore , W. Steglich , and C. Tamm , eds., Progress in the chemistry of organic natural products : Paris , Springer-Verlag , v. 57 , p. 1 – 70 . Peters , K. E. , and J. M...
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Journal Article
Published: 01 March 2019
South African Journal of Geology (2019) 122 (1): 79–96.
.... , Hawkesworth , C.J. , Storey , C.D. , Dhuime , B. , Leat , P.T. , Meyer , H.-P. and Tamm-Buckle , S. , 2010 . The Annandagstoppane Granite, East Antarctica: Evidence for Archaean Intracrustal Recycling in the Kaapvaal-Grunehogna Craton from Zircon O and Hf Isotopes . Journal...
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Journal Article
Published: 10 February 2020
Geological Magazine (2020) 157 (9): 1428–1450.
... granitic veins are shown in red. Fold data from this locality are shown in Figure 15b . (g) Asymmetric recumbent fold with S-to-SE vergence at Roerkulten and shallow NW-dipping axial plane. Cliff height is c. 100 m. Structural data from this locality are shown in Figure 15c , and the locality is photo...
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Journal Article
Published: 01 January 2004
Rocky Mountain Geology (2004) 39 (2): 113–140.
... et al., 1984 , fig. 5). LMR-C-9: starting at base of cliff, Sec. 4, SE 1/4, T. 136 N., R. 104 W. (see Conway, 1982 ). These sections were used by Belt et al. (1992) . All but PH-B-56 lie in SE quarter of Buck Mountain 7.5′ quadrangle, Montana. PH-B-56 lies in the Locate SW quadrangle...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2015
GSA Bulletin (2015) 127 (5-6): 781–803.
...-Pb analysis. The analytical procedure follows that described by Ickert et al. (2008) . Instrument mass fractionation was corrected using the standard zircon BR266 (δ 18 O = 13.26‰ relative to Vienna standard mean ocean water [VSMOW] standard; J. Cliff and L. Martin, 2013, personal commun...
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Journal Article
Journal: Economic Geology
Published: 01 November 2017
Economic Geology (2017) 112 (7): 1773–1806.
... encircled for scale. (B) Bed 1, comprising a central microbial laminite (ML) surrounded by reduced dolomitic siltstones (RS), at the south end of Coppercap Mountain. Geologist standing 10 m in front of cliff for scale. (C) Weathered surface of microbial laminite. Cupriferous sulfides stand out as high...
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