Fossils from the Fuller's Earth of the Weymouth Anticline

1940 ◽  
Vol 77 (1) ◽  
pp. 42-49 ◽  
Author(s):  
W. J. Arkell—
Keyword(s):  
Geological Survey ◽  
The West ◽  
The Core ◽  
Lower Horizon ◽  
Elliptical Area ◽  
Fuller’S Earth ◽  
Sea Coast

Fuller's Earth was first recorded at the surface in the core of the Weymouth anticline by Damon (1860, p. 12). It was mapped by the Geological Survey in a semi-elliptical area south of Langton Herring, having a sea coast of about 1¼ miles on the West Fleet (1 inch map, sheet 341). The chief feature of interest is a lumachelle or oyster bed composed of a mass up to some 12 feet thick of the small oyster, Ostrea hebridica Forbes (= 0. sowerbyi Morris and Lycett), the var. elongata Dutertre predominating (see Damon, 1860 and 1884, p. 12, fig. 3). The oyster was recorded by Damon and by Strahan (1898, p. 5, and sheet 341) as O. acuminata J. Sowerby, but that species belongs to a lower horizon, below the Fuller's Earth Rock. The Langton Herring oyster bed, which is seen also at Watton Cliff near Bridport, lies in the Upper Fuller's Earth, above the Fuller's Earth Rock, which does not come to the surface in the Weymouth anticline. The lowest beds exposed in the anticline, for a few feet below the oyster bed, are tough clays with mudstone nodules and abundant Rhynchonella smithi (Davidson) (see Arkell, 1933, p. 252). With the Rhynchonellids there weather out also abundant fragments of a typical Fuller's Earth belemnite, which I follow some French authors in calling Belemnopsis bessina (d'Orb.).

V.—Note on two Cephalopods Obtained by Lieut.-Col. Skinner, R.A.M.C., from the Valley of the Tochi River on the North-West Frontier of India

1904 ◽  
Vol 1 (10) ◽  
pp. 490-493
Author(s):  
G. C. Crick
Keyword(s):  
British Empire ◽  
Geological Survey ◽  
The West ◽  
Lower Eocene ◽  
North West ◽  
The Core ◽  
Fossil Remains ◽  
The North ◽  
North And South ◽  
Upper Mesozoic

The valley of the Tochi River is an outlying corner of the British Empire in India forming a portion of Waziristan, the boundary of which was delineated in 1894–5 by an Anglo-Afghan Commission from the Afghan provinces of Khost on the north and Birmul on the west. Mr. F. H. Smith, of the Geological Survey of India, accompanied this Commission as geologist, and his observations “On the Geology of the Tochi Valley” were published in 1895 in the “Records of the Geological Survey of India” (vol. xxxviii, pt. 3, pp. 106–110, pl. iii). On p. 109 he says:—“The range of hills between Idak and Mirán Shah is formed by an anticlinal ridge which approximately strikes north and south, and which is composed of these lower eocene beds. In the core of the anticlinal a considerable thickness of massive dark grey limestone is exposed, in which I could find no fossil remains; the age of this limestone is therefore doubtful, and there is no evidence of any kind to show whether it belongs to the lowest tertiary or upper mesozoic age.”

Further Jurassic Fossils from Kenya Colony

1927 ◽  
Vol 64 (7) ◽  
pp. 325-325 ◽  
Author(s):  
J. W. Gregory
Keyword(s):  
Geological Survey ◽  
The West ◽  
Specific Identification ◽  
Lower Horizon ◽  
Plant Remains

Mr. E. J. Wayland, of the Geological Survey of Uganda, has recently found three interesting fossils which throw further light on the age of the beds to the west and north of Mombasa. One of them is a cast of an ammonite in brown ironstone, which has been kindly examined by Dr. L. F. Spath; he says that being only a cast its specific identification is perhaps impossible. It is a Grossouvria, and he says it is very similar to several examples of G. lateralis (Waagen), from the Callovian anceps beds of Kachh. He identifies it as certainly a member of Siemiradzki's form-series of Perisphinctes balinensis, Neumayr. This identification is of interest as the fossil was obtained at the point 10/6 miles from Mombasa on the Uganda Railway. This position lies to the west of, and therefore at a lower horizon than, the ammonite-bearing shales near Mombasa. At 11 1/9 miles along the railway I found a lamellibranch in some dark shales and Dacqué (Geol. Rundsch., vol. i, 1910, p. 159) has recorded from near by some obscure Cephalopod and plant remains which he identified as Bathonian.

A new cave-dwelling species of the genus Cimmerites Jeannel, 1928 (Coleoptera: Carabidae: Trechini) from the West Caucasus

2011 ◽  
Vol 20 (1) ◽  
pp. 48-53
Author(s):  
I.A. Belousov ◽  
A.G. Koval
Keyword(s):  
New Species ◽  
Black Sea ◽  
Life Form ◽  
Intermediate Position ◽  
The Black Sea ◽  
The West ◽  
Black Sea Coast ◽  
A New Species ◽  
Sea Coast

A new species of the genus Cimmerites Jeannel, 1928, C. maximovitchi sp. nov., is described from the Akhunskaya Cave and Labirintovaya Cave, both located in the Akhun Karst Massif on the Black Sea Coast of the West Caucasus (Krasnodar Territory, Russia). The new species is rather isolated within the genus Cimmerites and occupies an intermediate position between species related to C. kryzhanovskii Belousov, 1998 and species close to C. vagabundus Belousov, 1998. Though both C. maximovitchi sp. nov. and C. kryzhanovskii are still known only from caves, these species are quite similar in their life form to other members of the genus which are all true endogean species.

scholarly journals Environmental justice, settler colonialism, and more-than-humans in the occupied West Bank: An introduction

2021 ◽  
Vol 4 (1) ◽  
pp. 3-27
Author(s):  
Irus Braverman
Keyword(s):  
United States ◽  
Environmental Justice ◽  
West Bank ◽  
Settler Colonialism ◽  
The United States ◽  
Special Issue ◽  
The West ◽  
The Core ◽  
Waste Concrete

Our special issue provides a first-of-its kind attempt to examine environmental injustices in the occupied West Bank through interdisciplinary perspectives, pointing to the broader settler colonial and neoliberal contexts within which they occur and to their more-than-human implications. Specifically, we seek to understand what environmental justice—a movement originating from, and rooted in, the United States—means in the context of Palestine/Israel. Moving beyond the settler-native dialectic, we draw attention to the more-than-human flows that occur in the region—which include water, air, waste, cement, trees, donkeys, watermelons, and insects—to consider the dynamic, and often gradational, meanings of frontier, enclosure, and Indigeneity in the West Bank, challenging the all-too-binary assumptions at the core of settler colonialism. Against the backdrop of the settler colonial project of territorial dispossession and elimination, we illuminate the infrastructural connections and disruptions among lives and matter in the West Bank, interpreting these through the lens of environmental justice. We finally ask what forms of ecological decolonization might emerge from this landscape of accumulating waste, concrete, and ruin. Such alternative visions that move beyond the single axis of settler-native enable the emergence of more nuanced, and even hopeful, ecological imaginaries that focus on sumud, dignity, and recognition.

A GRASP ON THE NATURE OF LUNDAYEH THROUGH THEIR TRADITIONAL DANCE CULTURE

2015 ◽  
Vol 3 (2) ◽  
pp. 1-22
Author(s):  
LEE SUAN CHONG
Keyword(s):  
Ethnic Groups ◽  
West Coast ◽  
Dance Music ◽  
Human Knowledge ◽  
The West ◽  
Dance Culture ◽  
The Core ◽  
The World ◽  
Religious Aspects ◽  
Life Philosophies

AbstrakPenduduk Lundayeh terdapat di Tenom, Sipitang dan Long Pa Sia, di sepanjang pantai barat Sabah, Malaysia. Bentuk dan sistem tarian Lundayeh telah melalui perubahan dan variasi sejak kewujudan mereka di Borneo. Artikel ini mengkaji dalam pelbagai aspek, termasuk muzik, pakaian, pergerakan, fungsi dancerita-cerita daripada tarian tradisional yang diamalkan dalam masyarakat Lundayeh hari ini di Kemabong, Sabah. Tarian tradisional Lundayeh yang masih diamalkan berdasar terutamanya kepada aspek budaya, sosial dan agama hidup Lundayeh. Kajian ini membawa kepada penemuan corak pemikiran, falsafahhidup dan perspektif dunia Lundayeh yang dipengaruhi oleh agama dan budaya purba mereka. Tarian tradisional Lundayeh berfungsi sebagai satu saluran untuk memahami sifat orang Lundayeh sebagai salah satu kumpulan etnik kecil di dunia. Pemahaman tentang sifat orang Lundayeh akan terus menyumbang ke arah perkongsian dan penemuan dalam dimensi ilmu kemanusiaan yang baru.   AbstractLundayeh populations are found in the areas of Tenom, Sipitang and Long Pa Sia, along the west coast of Sabah, Malaysia. Lundayeh dance forms and systems have gone through changes and variations since their existence in Borneo. This paper looks into a variety of aspects, including music, costumes, movements, functions and stories of the traditional dances practiced in today’s Lundayeh communities in Kemabong, Sabah. The surviving traditional dances found to have stemmed from the core of Lundayeh cultural, social and religious aspects of life. The study leads to the discovery of the thinking patterns, life philosophies and world perspectives of Lundayeh that are strongly influenced by their religion and ancient culture. Dance music ultimately serves as a tool to understand the nature of Lundayeh people as one of the minor ethnic groups in the world. The understanding of the nature of Lundayeh would further contribute toward sharing and discovering another dimension of human knowledge and wisdom.

scholarly journals III.—On the Relation between the Older and Newer Palæozoics of West Cornwall.

1906 ◽  
Vol 3 (5) ◽  
pp. 206-216 ◽  
Author(s):  
J. B. Hill
Keyword(s):  
The Other ◽  
Recent Survey ◽  
Geological Survey ◽  
The West ◽  
Natural Sequence ◽  
Lower Silurian ◽  
Other Hand ◽  
Coastal Belt ◽  
Broad Generalization ◽  
Organic Remains

The author, who has long been engaged on the Palæozoics of West Cornwall, divided the killas extending westward from Gerrans Bay into four groups that formed a natural sequence. Moreover, as they included definite Lower Silurian horizons, as characterized by the fossiliferous quartzite of Carne, these divisions were linked with the Lower Palæozoics. They consist of the Veryan, Portscatho, Falmouth, and Mylor groups. On the latest issues of the old Survey maps the area occupied by the first of these divisions is coloured as Silurian, and the region occupied by the remainder as Devonian. That colouring, however, was not adopted by De la Beche, who surveyed the region, nor was it the result of any subsequent survey of the area. In the original Geological Survey map of Cornwall the killas was separated by De la Beche into two divisions, viz., a grauwacke group and a carbonaceous series. Thus, the former lying below the Culm-measures was undifferentiated for the reason, as explained in his Report, that the progress of geology at that time only warranted the broadest generalizations. He moreover expressed the opinion that the terms Cambrian and Silurian should be restricted to the areas that gave rise to the prolonged researches of Murchison and Sedgwick, and deprecated the extension of that nomenclature to districts that had not received the same detailed investigations. In a later and undated issue of the map the grauwacke group is divided into Devonian and Silurian, presumably by the authority Sir Roderick Murchison. The Devonian colour was not only applied to fossiliferous strata in East and Mid Cornwall, but was extended over the unfossiliferous strata in the west. The Silurian tint, on the other hand, was restricted to a zone that had yielded organic remains. Murchison, however, was of opinion that the older zone extended far beyond those limits into the barren strata coloured as Devonian, and it is evident that the latter tint was adopted as a matter of convenience, as no re-examination of the area seems to have been undertaken. The known Silurian region was confined to the coastal belt between Chapel Point and Gerrans Bay, a boundary connecting those localities admitting of the ready isolation of that zone from the rest of the country. That such a broad generalization, however, was only regarded as provisional may be inferred from the absence of a line on the map between the two divisions. It will be seen, therefore, that the subdivision of the killas, as the result of the recent survey, neither invalidates the map published by De la Beche nor the subsequent conclusions of Murcliison. It has, on the other hand, not only brought their generalizations within more definite limits, but has carried the investigation a step farther by demonstrating the relations between the older and newer Palæozoics of Cornwall.

Fear on the Campaign Trail

2017 ◽  
Author(s):  
Adam I. P. Smith
Keyword(s):  
Federal Government ◽  
Abraham Lincoln ◽  
Effective Solution ◽  
The West ◽  
Campaign Strategies ◽  
Presidential Candidates ◽  
The Core ◽  
White Settlers

This chapter discusses the campaign strategies of the two main presidential candidates in the free states in the 1860 election, Abraham Lincoln and Stephen A. Douglas. Both appealed to voters’ desire to contain the Slave Power and assure access to the West for free white settlers. The core difference between Douglasites and Lincolnites was over the role of the Federal government in resolving the crisis: Republicans wanted to take control in Washington to prevent the nationalisation of slavery; Democrats continued to believe that the most effective solution was decentralisation.

Introduction

2019 ◽  
pp. 1-7
Author(s):  
Mitchell A. Orenstein
Keyword(s):  
European Union ◽  
Political Polarization ◽  
Delayed Response ◽  
Eastern European ◽  
The European Union ◽  
The West ◽  
Western Countries ◽  
The Core ◽  
Hybrid War

This introductory chapter outlines the core argument of the book: that as Russia ramped up its hybrid war on the West starting around 2007, politics in Western countries has become more similar to politics in the vulnerable “lands in between.” Russia’s hybrid war on the West has contributed to political polarization by promoting extremist parties and creating a sense that every election presents voters with a “civilizational choice” between Russia and the West or authoritarianism and democracy. Paradoxically, many of the leaders that rise to the top in these conditions are those who find ways to profit from both sides. They benefit from the sponsorship of pro-Russia and pro-Western interests to enrich themselves in the process. The plan of this book is simple. It starts with exploring the nature of Russia’s hybrid war on the West and the West’s delayed response. Then it shows how this conflict shapes the politics of the lands in between, Central and Eastern European member states of the European Union, and core Western countries.

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