The Continuing Process of Restoration, 1948–Present

Author(s):  
Estella B. Leopold

The process of restoration of the Shack lands did not end with Dad’s passing. Quite the contrary. It was picked up by several of his children and by some key neighbors and Wisconsin-based foundations, and ultimately by the Leopold Foundation staff, which continued by expanding the prairies. In this regard, some special recognition is due my sister Nina and her second husband, Charles Bradley, for their initial work developing new prairie areas in Sauk County. Their methods in building a prairie were novel additions to the work/technology that Aldo Leopold and John Curtis had started at the UW Arboretum in Madison. During the years 1940–1948, Dad continued to purchase more acres, so that by 1948 our holdings were about 350 acres in Fairfield Township, Sauk County. These acres were all contiguous with the original Shack lands. Nearby, Mother and Dad’s friends the Thomas Coleman family had over the years enjoyed the log cabin they had built on their land high above Lake Chapman overlooking the great marsh and floodplain. Reed Coleman, the younger son of Tom Coleman, with conservation in mind, in time wanted to expand the land holdings his father had purchased on the south side of the river road across from Lake Chapman. Reed and his colleague and friend Howard Mead laid a plan for the L. R. Head Foundation to gradually purchase nearby parcels of land as they became available from retiring farmers. The Head Foundation was able to compile a huge protected reserve surrounding the 350 or so acres that Dad had bought. It was a creative effort to protect the land of the region from being degraded by home developers and the like. Over the years from 1950 to the 1970s the Head Foundation succeeded in building what is now called the Aldo Leopold Memorial Reserve. This expansive project served indeed to stave off local development. Reed said that his effort was inspired by witnessing the subdividing of the old Gilbert farm along the river into slices of land for summer homes, and he did not want this to happen around either the Shack or the original Coleman land area.

2020 ◽  
Vol 73 (4) ◽  
pp. 539-550
Author(s):  
Li Yong-Sŏng ◽  
Park Won Kil
Keyword(s):  

AbstractThis paper attempts to give new explanation for the expression agrïp yok bol- occurring in 9th line of the south side of the Bilgä Kagan Inscription. After a thorough survey of former research and several Chinese sources, the authors came to the conclusion that this expression must be a euphemistic expression for being beheaded in a battle. The authors found also that kog säŋün was Guo Yingjie 郭英傑. In sum, the sentence in question is to be read as ulug oglum agrïp yok bolča kog säŋünüg balbal tikä bertim ‘When my oldest son died of a disease, I readily erected General Kog as a balbal (for him).’ The expression agrïp yok bol- is to be regarded as a euphemistic expression for being beheaded in a battle.


Author(s):  
Walter Garstang
Keyword(s):  

The crab whose habits I now describe has not previously been recorded as an inhabitant of British seas. I found two specimens, both male, imbedded in a patch of coarse shell sand on the south side of Drake's Island at low water, spring tides: one on August 11th, 1896, and the other on the following day.


1926 ◽  
Vol 6 (1) ◽  
pp. 59-72 ◽  
Author(s):  
Stanley Casson

The mound of Kilindir (fig. 1) lies about one kilometre south-west of the station of that name on the railway that runs from Salonika to Constantinople via Seres, Dedeagatch and Adrianople. A small stream called Gyol Ayak issues from the south side of Lake Doiran exactly at the modern village at Doiran station. This stream, after passing through nine kilometres of broken and ravined country, issues into more open ground just by the modern Chiflik which represents the pre-war site of the village of Kilindir.


1927 ◽  
Vol 7 (4) ◽  
pp. 438-464 ◽  
Author(s):  
E. Thurlow Leeds

At the end of April of last year the Rev. Charles Overy drew my attention to the presence of broken animal bones, flints, and sherds of pottery in a gravel-pit on the south side of the road from Abingdon to Radley, about a mile out of Abingdon (fig. 1).The pit lies on the very boundary of the parish of Abingdon in a field at about 200 ft. O.D., just over half a mile north of the Thames and some 30 ft. above the river. On its eastern and southern sides it is bounded by the wide trenches which in the days of the splendour of Abingdon Abbey formed part of the Abbey's fish-ponds ; on the north is the road, and on the east the ground drops to a little brook.


1919 ◽  
Vol 23 ◽  
pp. 64-66
Author(s):  
F. B. Welch
Keyword(s):  

I Here describe a few sites on the south side of the valley of the Strymon, which I noticed while stationed there in 1916–1918. All except No. 5 belong to the third type described by Wace and Thompson and consist of large, low flat-topped mounds covered with Hellenistic sherds. This part of the country was anciently inhabited by the Bisaltai.1. At kilometre 70 on the Salonika-Serres road, about three kilometres south-west of Sakavcha, and two-and-a-half kilometres west of Makesh. Round the edges the remains of ancient walls can be easily traced; in places they are still three feet high and the same thickness with small towers at irregular intervals. Remains of house walls can be found everywhere a few feet down.


2006 ◽  
Vol 36 (6) ◽  
pp. 1085-1103 ◽  
Author(s):  
Joseph P. Martin ◽  
Daniel L. Rudnick ◽  
Robert Pinkel

Abstract The density and current structure at the Hawaiian Ridge was observed using SeaSoar and Doppler sonar during a survey extending from Oahu to Brooks Banks. Across- and along-ridge changes in internal wave statistics in the upper ocean within 200 km of the ridge are investigated. Internal waves with trough-to-crest amplitude as large as 60 m and horizontal wavelength of about 50 km are observed repeatedly in across-ridge sections of potential density. Within 150 km of the ridge, kinetic and potential energy density exceed open-ocean values with maxima about 10 times Garrett–Munk levels. In the Kauai Channel (KC), the kinetic energy density is largest along an M2 internal tide ray. The ray originates at the northern edge of the ridge peak at a large across-ridge change in topographic slope and terminates at the ocean surface about 30–40 km south of the ridge peak. Kinetic and potential energy density are larger on the south side of the ridge at KC, the side with larger topographic slope. Energy density is also larger on the south side of the ridge at KC in numerical model results and on the side of steeper topographic slope in analytical model results. Along the ridge, the largest observed values of mean-square shear and mean-square slope of isopycnal depth are collocated with the largest energy density in numerical model results. Mean-square shear and mean-square slope increase with decreasing bottom depth and with increasing M2 barotropic tidal forcing.


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