Culture Sequence at the Old Fort, Saline County, Missouri

1973 ◽  
Vol 38 (1) ◽  
pp. 101-111 ◽  
Author(s):  
W. Raymond Wood
Keyword(s):  
Soil Profile ◽  
Field Data ◽  
Missouri River ◽  
Middle Woodland ◽  
The North ◽  
Culture Sequence ◽  
High Ridge ◽  
Habitation Site ◽  
North End ◽  
Saline County

AbstractThe Old Fort (23SA104), an earthwork enclosure and mound complex on a high ridge near the Missouri River in central Missouri, has long been considered a Middle Woodland or Hopewell construction. Excavations in 1970 cross-trenched prehistoric ditches and embankments on the north end of the enclosure. A well-developed soil profile containing predominantly Middle Woodland pottery was exposed, into which aboriginal ditches had been cut. Oneota pottery lay on the floors of these ditches, embedded in a thin laminated horizon of alluvium. Oneota and Middle Woodland pottery are mixed in ditch fills. Field data, although limited, thus support the identification of the enclosure as Oneota, aboriginally constructed on a Middle Woodland habitation site.

scholarly journals Ritual Economy and the Organization of Scioto Hopewell Craft Production: Insights from the Outskirts of the Mound City Group

2020 ◽  
Vol 85 (2) ◽  
pp. 279-304
Author(s):  
Timothy D. Everhart ◽  
Bret J. Ruby
Keyword(s):  
Craft Production ◽  
Small Scale ◽  
Magnetic Survey ◽  
Middle Woodland ◽  
The North ◽  
Large Structures ◽  
Production Site ◽  
Production And Consumption ◽  
Ritual Economy ◽  
City Group

This article offers insights into the organization of Scioto Hopewell craft production and examines the implications of this organization through the lens of ritual economy. We present a novel analysis of investigations at the North 40 site, concluding that it is a craft production site located on the outskirts of the renowned Mound City Group. High-resolution landscape-scale magnetic survey revealed a cluster of three large structures and two rows of associated pits; one of the buildings and three of the pits were sampled in excavations. Evidence from the North 40 site marks this as the best-documented Scioto Hopewell craft production site. Mica, chert, and copper were crafted here in contexts organized outside the realm of domestic household production and consumption. Other material remains from the site suggest that crafting was specialized and embedded in ceremonial contexts. This analysis of the complex organization of Scioto Hopewell craft production provides grounds for further understanding the elaborate ceremonialism practiced by Middle Woodland (AD 1–400) societies and adds to the known complexity of craft production in small-scale societies. Furthermore, this article contributes to a growing body of literature demonstrating the utility of ritual economy as a framework for approaching the sociality of small-scale societies.

VI. Antiquities discovered in Lancaster, 1776. By Mr. West, Author of the “Antiquities of Furness.” Communicated by Mr. Lort

Archaeologia ◽  
1779 ◽  
Vol 5 ◽  
pp. 98-100
Author(s):  
West
Keyword(s):  
Very Old ◽  
Human Skull ◽  
The North ◽  
Burnt Wood ◽  
Roman Coins ◽  
The Dead ◽  
Large House ◽  
North End

On sinking the cellars for a large house at the upper part of Church-street in this town, now building by Daniel Wilson, esq. on the site of which stood some very old houses (formerly called the Judge's lodgings), was discovered, at about six feet below the present surface of the street, a supposed Roman burying-place; as burnt wood, bones, and ashes, broken paterae, urns, Roman brick, gutter tiles, coins, horns of animals, &c. were found; also, two fragments of thick walls, at about five yards distant from each other, in a direction from front to back, and seeming to continue under Church-street, be-twixt which were several large stones, some of which were hewn. By this it may be conjectured, to have been a vault to deposit the ashes of the dead, and fallen-in, or pulled down, at some time, as there were found, within the walls, several pieces of urns, an earthen sepulchral lamp entire (the end of the spout where the wick came out was burnt black), broken paterae, burnt bones, ashes, a large human skull, Roman coins, &c. also, at the North-end a well, filled with hewn stones, but not meddled with.

4. Results of Makerstoun Observations, No. III. On the Solar and Lunar periods of the Magnetic Declination.

1851 ◽  
Vol 2 ◽  
pp. 144-145
Author(s):  
J. A. Broun
Keyword(s):  
The North ◽  
Magnetic Declination ◽  
The Mean ◽  
The Absolute ◽  
Annual Period ◽  
North End

The absolute westerly declination at Makerstoun, for the mean epoch, June 1844 = 25° 17′·12.The annual motion of the north end of the needle towards the east = 5′·67.The annual periodof magnetic declination consists of a double oscillation, having nearly the following epochs of maxima and minima.

scholarly journals “Sermo eorum sicut cancer serpit”. Chromatius of Aquileia against heresies

Vox Patrum ◽  
2018 ◽  
Vol 68 ◽  
pp. 443-455
Author(s):  
Miran Sajovic
Keyword(s):  
20Th Century ◽  
Adriatic Sea ◽  
Conference Paper ◽  
The North ◽  
Trade Center ◽  
The Impact ◽  
North End

Bishop Chromatius (in office from 388 to 407), whose episcopal see was a cosmopolitan trade-center at the north end of the Adriatic Sea with the name of Aquileia, was one of the most prominent bishops in the period. He is acquaint­ed with notable figures such as Ambrosius, Hieronymus, Rufinus, and Ioannes Chrysostomus and forth. Before being created a bishop, he was the secretary of bi­shop Valerianus and in the occasion of Council of Aquileia in 381, he had spoken against Arians. This Council was presided by Ambrosius and with its scale it could almost be considered as an ecumenical one. As shown in some of the Chromatius’ sermons, which are unearthed in the 20th century, he opposed not only to the ideas of Arians but also to the teaching of Fotinus, bishop of Sirmium. Chromatius was a very zealous fighter and he practically succeeded to uproot all heretical ideas in his diocese. The academia usually sees him as an anti-Arian theologian. After the Council of Constantinople (381), the Arian heresy seemed to be abated, but Chromatius said in one of his Tractatus, “Cuius (sc. Arii) discipuli hodieque oues Dei fallere ac decipere conantur per aliquantas ecclesias, sed iamdudum, magistro perfidiae prodito, discipuli latere non possunt”; it is evident that, the followers of Arius could still be found (with the mentioning of “hodie”, i.e. today) in the area of Aquileia, meanwhile one must not neglect the presence of the followers of Fotinus of Sirmium. The first part of my conference paper would be a general presentation of the religious situation in Aquileia at the time where Chromatius served as the local bishop; thus I will proceed with an in-depth reading on several passages of the Aquilerian bishop’s sermons (Sermones and Tractatus), in order to show the impact of the those heresies on his works and to identity his theological arguments against them. Among those teachings, there is the “unconquerable faith (invicta fide)”, which led to the surmounting (suppression) of heresies.

scholarly journals Effect of slope aspect on transformation of clay minerals in Alpine soils

Clay Minerals ◽  
2007 ◽  
Vol 42 (3) ◽  
pp. 373-398 ◽  
Author(s):  
M. Egli ◽  
A. Mirabella ◽  
G. Sartori ◽  
D. Giaccai ◽  
R. Zanelli ◽  
...  
Keyword(s):  
Clay Minerals ◽  
Soil Profile ◽  
Water Flux ◽  
Layer Charge ◽  
Slope Aspect ◽  
X Ray Diffraction ◽  
The South ◽  
Octahedral Sheet ◽  
The North ◽  
Low Charge

AbstractTwo soil profile sequences on paragneiss debris in the Val di Rabbi (Northern Italy) along an altitude gradient ranging from 1200 to 2400 m a.s.l. were studied to evaluate the effect of aspect on the weathering of clay minerals. All the soils had a coarse structure, a sandy texture and a low pH. Greater weathering intensities of clay-sized phyllosilicates (greater content of smectites) were observed in soils on the north-facing slope. On the south-facing slope, smectite was found only in the surface horizon of the soil profile at the highest altitude. Hot citrate treatment of north-facing soils revealed the presence of low-charged 2:1 clay minerals, the expansion of which was hindered in the untreated state by interlayered polymers. However, the hot citrate treatment encountered some problems with the samples of the south-facing soils: as confirmed by Fourier transform infrared spectroscopy, the hot citrate treatment was unable to remove all interlayer Al polymers. The 2:1 phyllosilicates were not expanded by ethylene glycol solvation in several samples, although thermogravimetric analyses indicated the presence of clay minerals with interlayer H2O. At the same time, the collapse of clay minerals to 1.0 nm following K-saturation was evident. Theoretically, this should indicate that 2:1 phyllosilicates had no evident substitution of trioctahedral cations (Mg2+, Fe2+) by dioctahedral cations (Al3+ and Fe3+). X-ray diffraction analysis of the d060 region and determination of the layer charge of clay minerals by the long-chain (C18) alkylammonium ion, however, did not confirm this. A transformation from trioctahedral to dioctahedral species was observed and low-charge clay minerals (ξ ~0.30) were identified in the surface horizons of the south-facing sites. In the south-facing soils, the podzolization process was less pronounced because of a lower water flux through the soil and probably less complexing organic molecules that would remove the interlayer polymers. Besides the eluviation process, clay minerals underwent a process of ionic substitutions in the octahedral sheet that led to the reduction of the layer charge. This process was more obvious in the north-facing sites.

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