Geology of areas of the Bellefonte, Tyrone and Lock Haven Quadrangles. First Annual Field Conference of Pennsylvania Geologists, 1931.
Road logs were not included with this guidebook but five trips were conducted. 1. American Lime and Stone Company at Bellefonte. 2. Silurian and Lower Devonian rocks of the Bald Eagle Valley from Bellefonte to Lock Haven. 3. Stratigraphy of the Allegheny Front from Gallitzen to Altoona. 4. Tyrone [Birmingham] thrust fault structures.
Around and Near the "Forks of the Delaware," and Various and Sundry "Gaps." Second Annual Field Conference of Pennsylvania Geologists, 1932.
Six field trips with road logs are in the guidebook. Two one-half day trips examined Triassic rocks and the slate and cement district. The main excursion traversed the Lehigh and Delaware gaps followed by three one-half day trips in the Saucon Valley, Pleistocene drifts, and the Spitzenberg.
Geology of Central Pennsylvania. Third Annual Field Conference of Pennsylvania Geologists, 1933.
This conference included six field trips in central Pennsylvania. 1. Cornwall Mines. la. Cornwall Mines and Triassic. 2. Third Mountain. 3. Susquehanna-Juniata Valleys. 4. South Mountain. 5. Western Perry County.
Geology of Western Pennsylvania. Fourth Annual Field Conference of Pennsylvania Geologists, 1934.
Areas near Pittsburgh were explored during this conference. Trips conducted were: la. Wildwood underground coal mine; lb. Herron Hill Reservoir and Allegheny River Boulevard; 1c. the Carnegie Museum. 2. Beaver Valley area. 3. Uniontown and Ohiopyle area.
Philadelphia Area of Southeastern Pennsylvania. Fifth Annual Field Conference of Pennsylvania Geologists, 1935.
Five field trips were taken during this conference. They included: 1. Physiographic trip southwest of Philadelphia. 2. Mineralogic and petrologic localities north of Philadelphia. 3. Crystalline rocks of the Piedmont north and west of Philadelphia. 4. Lower Paleozoic Formations and their relations to the Pre-Cambrian rocks. 5. Coastal Plain excursion in New Jersey.
Conference Hosts: Academy of Natural Sciences, Bryn Mawr College, Lehigh University, University of Pennsylvania, and Atlantic Refining Co.
Geological Inspection of Anthracite Region. Sixth Annual Field Conference of Pennsylvania Geologists, 1936.
Conference members examined the geology of the anthracite region as well as the mining methods used and the problems encountered while mining coal as well as mine fires. Road logs are indicated for trips in the northern, middle and southern anthracite fields. This conference was conducted in association with the New York State Geological Association.
Bradford District Trip. Seventh Annual Field Conference of Pennsylvania Geologists, 1937.
The stratigraphy of the oil fields of the Bradford District is discussed. Two field trips traversing McKean and Warren Counties are included. A trip was also conducted to Presque Isle to study Pleistocene and shoreline features.
Virginia Trip. Eighth Annual Field Conference of Pennsylvania Geologists, 1938.
This field trip traversed northern Virginia, and parts of West Virginia, and Maryland examining Paleozoic rocks and included a trip on the Skyline Drive. The guidebook was published as Virginia Geological Survey Guide Leaflet No. 1.
West Virginia Trip. Ninth Annual Field Conference of Pennsylvania Geologists, 1939.
This field trip went from Morgantown to Berkeley Springs, WV examining the major outcrops along the route. A geologic column is included.
The Geology of New Jersey. Tenth Annual Field Conference of Pennsylvania Geologists, 1940.
Four field trips were conducted. 1. Geology of the Culvers Gap to Newfoundland area. 2. Geology of the Franklin district. 3. Physiography, glaciation and soils. 4. Cretaceous and tertiary stratigraphy of the Coastal Plain.
Allegheny Front Trip: Blue Knob-East Freedom-Hollidaysburg-Williamsburg Area, Pennsylvania. Eleventh Annual Field Conference of Pennsylvania Geologists, 1941.
The field trip examined Cambrian-Pennsylvanian rocks along the Allegheny Front.
From the Cambrian to the Silurian near State College and Tyrone. Twelfth Annual Field Conference of Pennsylvania Geologists, 1946.
The trip outlined was concerned with lower Paleozoic rocks of the Appalachian Valley and Ridge Province and the Allegheny Plateau. Upper Devonian to Pennsylvanian rocks along the Horse Shoe Curve near Altoona were also included.
Thirteenth Annual Field Conference of Pennsylvania Geologists, 1947.
Northampton and Lehigh Counties were explored during this field conference. Field trips outlined included: 1. Nazareth Cement Plant. 2. Saucon Valley Zinc Mines and Triassic intrusives. 3. The Valley of the Lehigh. 4. West from Bethlehem. 5. Triassic fanglomerates of Delaware Valley.
Fourteenth Annual Field Conference of Pennsylvania Geologists, 1948.
South-central Pennsylvania was the site of this field conference. Four field trips are outlined in this guidebook. 1. South Mountain. 2. Pennsylvania Turnpike. 3. Cornwall Mine. 4. Susquehanna-Juniata River.
Fifteenth Annual Field Conference of Pennsylvania Geologists, 1949.
This conference, centered in Lancaster County, included three field trips. 1. Old metal mines and Mine Ridge Anticline. 2. "Martic Overthrust" area. 3. Appalachian drainage and Pleistocene terraces.
Sixteenth Annual Field Conference of Pennsylvania Geologists, 1950.
Three field trips are included. 1. Visit to Jones and Laughlin Steel Company, Aliquippa Plant. 2. Glacial Foreland, Northwest Pennsylvania. This trip examined the evidence of glacier-dammed lakes in the Slippery Rock and Muddy Creek valleys in Butler County, and the resulting drainage diversions through the Slippery Rock Gorge in Lawrence County. 3. Chestnut Ridge Anticline.
Guidebook Illustrating the Geology of the Philadelphia Area. Seventeenth Annual Field Conference of Pennsylvania Geologists, 1951.
The geology of the Chester Valley was explored, giving participants a general overview of the mineralogy and geology of the area.
Sussex County, New Jersey. Eighteenth Annual Field Conference of Pennsylvania Geologists, 1952.
Field trips were conducted. 1. Pleistocene geology. 2. Dikes of special petrologic interest. 3. Silurian and Devonian stratigraphy. 4. Cambro-Ordovician and Pre-Cambrian rocks. 5. Silurian-Devonian of Nearpass quarries.
Nineteenth Annual Field Conference of Pennsylvania Geologists, 1953.
This conference, held in Northampton County, summarized the geology of the area through its four field trips. 1. North from Easton to slate and cement areas. 2. Mineral collecting trip to serpentine quarries north of Easton. 3. North from Easton to Panther Valley anthracite region. 4. South from Easton to Riegelsville.
Twentieth Annual Field Conference of Pennsylvania Geologists, 1954.
The field trips taken at this conference were almost entirely in Lebanon County. The routes were in the Great Valley section of the Ridge and Valley province. Trips included: 1. Cornwall iron deposits. 2. Cambro- Ordovician limestones of Lebanon County. 3. Martinsburg Formation and associated eruptive rocks of the Jonestown area.
Twenty-first Annual Field Conference of Pennsylvania Geologists, 1955.
This field conference provided participants with a general review of the geology of parts of central Pennsylvania. They were: 1. Stratigraphy of Ordovician limestones and dolomites of Nittany Valley from Bellefonte to Pleasant Gap. 2. Stratigraphy and structure of Ridge and Valley area from University Park to Tyrone, Mt. Union, and Lewistown. 3. Stratigraphy and structure of Pennsylvania sediments of the Plateau area near Philipsburg and Clearfield.
Twenty-second Annual Field Conference of Pennsylvania Geologists, 1956.
This guidebook summarized the geology of the major physiographic provinces and Coastal Plain sediments near Trenton, New Jersey, and included a stop at Limeport, Bucks County, Pennsylvania.
Structural Geology of South Mountain and Appalachians in Maryland. Twenty-third Annual Field Conference of Pennsylvania Geologists, 1958.
This guidebook was published as the Johns Hopkins University Studies in Geology No. 17 and is available from University Microfilms, 300 North Zeebs Road, Ann Arbor, Michigan 48106.
The South Mountain anticlinorium and the Appalachians to the west are examined. The route does not extend into Pennsylvania.
Twenty-fourth Annual Field Conference of Pennsylvania Geologists, 1959.
The field conference celebrated the centennial of the Drake well and included trips throughout northwestern Pennsylvania. 1. The glacial geology of Crawford and Erie Counties. 2. Bedrock and oil geology of northwestern Pennsylvania and the great Oildorado. 3. Erosion channel in Penn Dixie limestone mine. A history of the Drake well and a visit to the museum are included in this guidebook.
Some Tectonics and Structural Problems of the Appalachian Piedmont along the Susquehanna River. Twenty-fifth Annual Field Conference of Pennsylvania Geologists, 1960.
This trip examined the intensely deformed, metamorphosed and intruded inner Piedmont, Triassic fanglomerates, nappe structures and Ordovician volcanics.
Structure and Stratigraphy of the Reading Hills and Lehigh Valley in Northampton and Lehigh Counties, Pennsylvania. Twenty-sixth Annual Field Conference of Pennsylvania Geologists, 1961.
The field trip was designed to examine and compare the structural features of the rocks of the Reading Hills and those of the Lehigh Valley in Northampton and Lehigh Counties, Pennsylvania and adjacent parts of New Jersey and to examine the relationship between early Paleozoic tectonism and sedimentation.
Stratigraphy, Structure, and Economic Geology of Southern Somerset County and Adjacent Parts of Bedford and Fayette Counties, Pennsylvania. Twenty-seventh Annual Field Conference of Pennsylvania Geologists, 1962.
The general geology of Devonian and Carboniferous rocks in the Appalachian Plateau of Pennsylvania are examined.
Stratigraphy and Structure of Upper and Middle Devonian Rocks in Northeastern Pennsylvania. Twenty-eighth Annual Field Conference of Pennsylvania Geologists, 1963.
The field guide describes, evaluates, and interprets the stratigraphic and structural framework of Catskill and related strata in northeast Pennsylvania. A two day field trip, including eleven stops, begins and ends in Stroudsburg.
Cyclic Sedimentation in the Carboniferous of Western Pennsylvania. Twenty-ninth Annual Field Conference of Pennsylvania Geologists, 1964.
This field trip is concerned with the existence, character, and genesis of cyclothems in the Carboniferous rocks of western Pennsylvania. It provides conceptional and physical frameworks within which some important aspects of Carboniferous sedimentation and stratigraphy can be observed.
Stratigraphy of the Pennsylvanian and Permian Rocks of Washington, Mercer, and Lawrence Counties, Pennsylvania. Thirtieth Annual Field Conference of Pennsylvania Geologists, 1965.
The guide includes two field trips: 1. Stratigraphy of Upper Pennsylvanian and Lower Permian rocks, Washington County. 2. Stratigraphy of the Pottsville and Allegheny groups of Mercer and Lawrence Counties.
Comparative Tectonics and Stratigraphy of the Cumberland and Lebanon Valleys. Thirty- first Annual Field Conference of Pennsylvania Geologists, 1966.
The Cumberland and Lebanon Valley stratigraphic sequences are examined at various locations. The structural and stratigraphic discontinuities between them is demonstrated.
Geology in the Region of the Delaware to Lehigh Water Gaps. Thirty-second Annual Field Conference of Pennsylvania Geologists, 1967.
The interrelationship of the stratigraphy, structure, geomorphology, glacial geology, and economic geology of the Middle Ordovician through part of the Middle Devonian strata and overlying surficial deposits in the area between the Delaware and Lehigh Rivers in eastern Pennsylvania is demonstrated by this guide. A two day field trip log is included.
The Geology of Mineral Deposits in South-Central Pennsylvania. Thirty-third Annual Field Conference of Pennsylvania Geologists, 1968.
The guide for a two day field trip begins and ends in Harrisburg. It contains detailed discussions of mineral deposits of the region. Each deposit is discussed separately. Stops were made at the GAF greenstone quarry, Hanover quarry, Thomasville stone quarry, Bender's quarry, Mt. Holly white clay deposits, Millard quarry, and Eschelmann's quarry.
The Pocono Formation in Northeastern Pennsylvania. Thirty-fourth Annual Field Conference of Pennsylvania Geologists, 1969.
A detailed description of the Mississippian Pocono Formation is given. The trip, 240 miles long with nine stops, begins and ends in Hazleton.
New Interpretations of Eastern Piedmont Geology of Maryland. Thirty-fifth Annual Field Conference of Pennsylvania Geologists, 1970.
The area visited by this field conference is the northeastern Piedmont of Maryland mainly Baltimore, Cecil, and Harford Counties. The trip does not extend into Pennsylvania.
Upper Devonian Sedimentation in Susquehanna County and Hydrology, Glacial Geology and Environmental Geology of the Wyoming-Lackawanna Valley. Thirty-sixth Annual Field Conference of Pennsylvania Geologists, 1971.
The first trip presents a discussion of the geology, composition, texture, and physical properties of the flagstones of northeastern Pennsylvania and of the properties of flagstone that affect their discovery, development, and use. The second shows environmental problems resulting from the removal of the coal in the northern anthracite field and examines exposures of Pleistocene deposits.
Stratigraphy, Sedimentology, and Structure of Silurian and Devonian Rocks Along the Allegheny Front in Bedford County, Pennsylvania, Allegheny County, Maryland, and Mineral and Grant Counties, West Virginia. Thirty-seventh Annual Field Conference of Pennsylvania Geologists, 1972.
This guidebook brings together the varied structural and stratigraphic research concerned with the Allegheny Front. It traces the geology from Pennsylvania southward across Maryland to West Virginia demonstrating the regional continuity of certain stratigraphic and structural trends.
Structure and Silurian-Devonian Stratigraphy of the Valley and Ridge Province, Central Pennsylvania. Thirty-eighth Annual Field Conference of Pennsylvania Geologists, 1973.
The Valley and Ridge Province of the Appalachians has been considered a classic area of relatively simple geologic structures with complete and undeformed Paleozoic stratigraphic sections. Revisions of the structural geology and stratigraphy are demonstrated in this field trip guide.
Geology of the Piedmont of Southeastern Pennsylvania. Thirty-ninth Annual Field Conference of Pennsylvania Geologists, 1974.
The guidebook contains a group of studies dealing with the Pennsylvania Piedmont, including an introduction to crystalline rocks, deformation and metamorphism in the Wissahickon Formation, and an examination of sinkholes.
The Late Wisconsinan Drift Border in Northeastern Pennsylvania. Fortieth Annual Field Conference of Pennsylvania Geologists, 1975.
The character and availability of the Late Wisconsinan drift materials, similarities and differences between the Late Wisconsinan drift and pre-Late Wisconsinan-post Sangamonian drift, the character of the Illinoian glacial drift, the character of deposits of periglacial origin, and the reasoning used in differentiating and dating these various deposits are included in this field guide.
Bedrock and Glacial Geology of Northwestern Pennsylvania in Crawford, Forest and Venango Counties. Forty-first Annual Field Conference of Pennsylvania Geologists, 1976.
The area examined by this trip is near the boundary between the glaciated and unglaciated sections of the Allegheny Plateau Province. The Mapledale and Titusville Tills, with their respective glaciofluvial deposits, are examined, as are exposures of Upper Devonian(?), Mississippian, and Lower Pennsylvanian rocks. The controversial Carbon-14 dating site that placed the Titusville Till in the early Wisconsinan was visited.
Stratigraphy and Applied Geology of the Lower Paleozoic Carbonates in Northwestern New Jersey. Forty-second Annual Field Conference of Pennsylvania Geologists, 1977.
The intent of this field trip is to present the subdivision of the Cambro-Ordovician "Kittatinny" carbonate sequence and to cite some case histories of environmental, geohydrologic, and engineering problems. Two field trips, covering northwestern New Jersey, are outlined in the guidebook.
Uranium in Carbon, Lycoming, Sullivan, and Columbia Counties, Pennsylvania. Forty-third Annual Field Conference of Pennsylvania Geologists, 1978.
Sedimentological and geochemical models were presented to account for the primary distribution of the uranium minerals and their enclosing rocks. A post-depositional model was also presented to explain the present localizations of these minerals.
Devonian Shales in South-Central Pennsylvania and Maryland. Forty-fourth Annual Field Conference of Pennsylvania Geologists, 1979.
The authors describe the major purpose of this field conference as to demonstrate the outcrop stratigraphic relationships and nomenclatural changes among the Brallier Formation, Harrell and Burket Shales, Tully Limestone, and Mahantango Formation. A secondary purpose is to illustrate the facies and faunal changes within the Needmore Shale and Huntersville chert.
Land Use and Abuse – The Allegheny County Problem. Forty-fifth Annual Field Conference of Pennsylvania Geologists, 1980.
The field conference highlighted the geology of the Pittsburgh area. Included are the geology of the area, coal geology, oil geology, and geologic hazard problems.
Geology of Tioga and Bradford Counties, Pennsylvania. Forty-sixth Annual Field Conference of Pennsylvania Geologists, 1981.
The guidebook was for an area untouched by a geologic study in recent years. Included are the stratigraphy, sedimentology, glacial geology, economic geology, and groundwater geology.
Geology of the Middle Ordovician Martinsburg Formation and related rocks in Pennsylvania. Forty-seventh Annual Field Conference of Pennsylvania Geologists, 1982.
This field conference allowed participants to examine outcrops, lithologies, and structures of the Martinsburg Formation. The discussion examined the structure, stratigraphy, sedimentology, and plate tectonics of the formation. The first day of the field trip was spent west of Harrisburg in the Great Valley. The second day was spent east of Harrisburg in the allochthonous "Hamburg klippe".
Silurian Depositional History and Alleghanian Deformation in the Pennsylvania Valley and Ridge. Forth-eighth Annual Field Conference of Pennsylvania Geologists, 1983.
This field conference examined the landscape of central Pennsylvania which is dominated by linear ridges and fertile valleys. For the Lower and Middle Silurian units, a pattern in the complex paleoenvironmental patterns that is related to Appalachian Basin configuration, source area tectonics, and sea-level fluctuations, were examined. Strain features which help explain the Alleghany Orogeny are also examined.
Geology of an Accreted Terrane: The Eastern Hamburg Klippe and Surrounding Rocks, Eastern Pennsylvania. Forty-ninth Annual Field Conference of Pennsylvania Geologists, 1984.
Participants had the opportunity to see Cambro-Ordovician rocks of the eastern Hamburg klippe, nearby Ordovician rocks of the Shochary Ridge and the Martinsburg Formation, as well as Silurian and Devonian rocks in the Valley and Ridge north of Reading, PA.
Central Pennsylvania Geology Revisited: Coral Reef; The Catskill Clastics; Quaternary and Tertiary Geology; Deformed Zones; Exploration and Exploitation of Coal. Fiftieth Annual Field Conference of Pennsylvania Geologists, 1985- The Golden Jubilee.
The Golden Jubilee Conference returned to topics examined at the first Field Conference emphasizing the advances made in our understanding since that time. In addition, and to emphasize the prominent role geology plays in society today, two applied topics-Geology in the Exploration and Exploitation of Coal, and Application of Quaternary and Tertiary Geology to Environmental Problems in a Carbonate Valley in Central Pennsylvania were presented as was an opportunity to visit an undolomitized Silurian coral-Bryozoan reef.
Selected Geology of Bedford and Huntingdon Counties-. Fifty-first Annual Field Conference of Pennsylvania Geologists, 1986- In celebration of the Sesquicentennial of the Pennsylvania Geological Survey: 1836 to 1986.
In the spring of 1836, three geologists of the First Geological Survey of Pennsylvania made a trip across Pennsylvania examining rocks along a traverse which included the valleys of the Little Juniata and Juniata Rivers in Huntingdon County. Later that summer field work began with the measurement of the Paleozoic section from the Broad Top along the course of Yellow Creek. This field work established the correct sequence of Paleozoic stratigraphy for the Appalachians. The 1986 Field Conference revisited some of the outcrops first examined in 1836 and considered them in light of modern geologic thought. The trip examined much of the Paleozoic section and included structures in Bedford and Huntingdon Counties, as well as the first ever Field Conference stop in the coal-bearing rocks of the Broad Top.
Pleistocene and Holocene Geology on a Dynamic Coast. Fifty-second Annual Field Conference of Pennsylvania Geologists, 1987.
The Field Conference examined some of the ice-marginal landforms, and some landforms developed by changing lake level. Attendees examined various diamicts, and sand and gravel facies which comprise these landforms. Problems of determining sedimentary environments and related sedimentological history were emphasized.
Bedrock and Glacial Geology of the North Branch Susquehanna Lowland and the Eastern Middle Anthracite Field. Fifty-third Annual Field Conference of Pennsylvania Geologists, 1988.
Geology in the Laurel Highlands of Southwestern Pennsylvania. Fifty-fourth Annual Field Conference of Pennsylvania Geologists, 1989.
The 54th Field Conference examined the stratigraphy and sedimentary geology of the latest Devonian and earliest Mississippian rocks exposed in western Pennsylvania, the geology of Mississippian carbonates, Pennsylvanian freshwater limestones and flint clays, geochemistry of calcium carbonate polymorphs in Pennsylvanian marine fossils, coal mining and related environmental problems. And an overview of the infamous Johnstown floods.
Carbonates, Schists, and Geomorphology in the Vicinity of the Lower Reaches of the Susquehanna River. Fifty-fifth Annual Field Conference of Pennsylvania Geologists, 1990.
The 55th Field Conference focused on three topics of new field work and new thinking about the geology of western Lancaster and eastern York Counties. These are: 1) the age, facies, and tectonic relationships of the carbonate rocks which are extensively quarried in the two counties, 2) the structural history of the schists (and related rocks) which lie south of the Martic Line, and 3) the origin and age of the dramatic landscape in and around the gorge of the lower Susquehanna River.
Conference Hosts: Elizabethtown College, J.E. Baker Company, Millersville University, Pennsylvania Geological Survey, Tethys Consultants, Inc.
Geology in the South Mountain Area, Pennsylvania. Fifty-sixth Annual Field Conference of Pennsylvania Geologists, 1991.
Precambrian metavolcanics and Cambrian clastics comprise the rocks deformed during the development of the South Mountain Anticlinorium. Their lithologies and metamorphosed sedimentary structures provide considerable insight into the ancient geologic history of South Mountain. Topographic forms, various surficial deposits, and weathering products provide enticing glimpses of more recent climate/process development of the present landscape.
Geology of the Upper Allegheny River Region in Warren County, Northwestern Pennsylvania. Fifty-seventh Annual Field Conference of Pennsylvania Geologists, 1992.
Warren County was the site of such pioneering geological investigations as John Carll's oil and gas studies in the 1880's and Charles Butts' folio-mapping in the early 1900's. The Warren Field Conference emphasized 1) some new and exciting regional findings obtained from a concurrent PaGS mapping effort, and 2) the results of a variety of related topical studies (ranging from Upper Devonian stratigraphy to periglacial phenomena and forest ecology).
Geology of the Southern Somerset County Region, Southwestern Pennsylvania. Fifty-eighth Annual Field Conference of Pennsylvania Geologists, 1993.
Several excellent outcrops demonstrated sedimentological interpretations of rocks of Devonian, Mississippian, and Pennsylvanian age. Newly discovered Devonian fish bone horizons and "fish wallows" highlight one stop. Multiple point-bar and crevasse splay deposits were exposed in an active strip mine. In the Allegheny Mountain section of the Appalachian Plateaus province, the diverse and spectacular erosional topography reflects rock structure differently than in adjacent physiographic sections and provinces. The highest point in Pennsylvania, Mount Davis, was visited.
Various Aspects of Piedmont Geology in Lancaster and Chester Counties, Pennsylvania. Fifty-ninth Annual Field Conference of Pennsylvania Geologists, 1994.
The trip examined carbonates, siliciclastic rocks, metabasalts, and pre-Taconian to Late Alleghanian structures. Attendees also observed the results of Piedmont landscape evolution, and the evolution of Late Cenozoic terraces along the lower Susquehanna River.
Applied Geology in the Lock Haven and Williamsport Region, Clinton, Lycoming, and Tioga Counties, Northcentral Pennsylvania. Sixtieth Annual Field Conference of Pennsylvania Geologists, 1995.
This trip focused upon the role that earth sciences play in solving some of society's problems, including treatment of natural hazards, halting environmental degradation, and safe extraction of natural resources.
Structures of the Ridge and Valley Province, commonly ascribed to the Alleghany Orogeny, did not form simultaneously, but rather, were created in a sequence of stages including: (1) horizontal layer-parallel shortening (LPS) and transport to the northwest along major bedding detachments, (2) imbricate thrusting and major folding, (3) vertical extension on steep fold limbs, (4) steep, out-of-sequence reverse faulting, only found on the southwest limb of the Pennsylvania Salient. During this sequence, the principle shortening direction progressively rotated clockwise on the northeast limb of the Pennsylvania Salient and counter-clockwise on its southwest limb.
Geology of the Wyoming-Lackawanna Valley and its Mountain Rim, northeastern Pennsylvania. Sixty-second Annual Field Conference of Pennsylvania Geologists, 1997.
Focus of the conference was the Carboniferous stratigraphy and Pleistocene geomorphology of the Wilkes-Barre/Scranton area of the Northern Anthracite field. Stops of the two-day conference field trip concentrated on the radical changes in thickness and lithology which occur in the Mississippian units (particularly the Spechty Kopf and Mauch Chunk Formations) northeastward around the fringes of the Lackawanna basin, the lithologic and depositional characteristics of Loyalhanna Member-equivalent rocks in the Mauch Chunk Formation, the nature and extent of disconformities beneath the "Loyalhanna Member" and the Pottsville Formation in northeastern Pennsylvania, and the origin and geologic significance of scenic Pleistocene and post-Pleistocene "potholes" and bedrock gorges. Other topics considered at various stops included the complex-and often spectacular-tectonic structures at and near the Pottsville-Mauch Chunk contact, coalbed stratigraphy of the lower Llewellyn Formation, calcretes in the upper Llewellyn, the "infamous" Wal-Mart rockslide at Dickson City, and environmental geology of the Keystone Landfill northeast of Scranton.
Two pre-conference field trips were held, one to Nay Aug Park supplementing the stratigraphic and geomorphologic emphases of the main conference and the other featuring a descent into the Lackawanna Coal Mine.
Geotectonic Environment of the Lake Erie Crustal Block. Sixty-third Annual Field Conference of Pennsylvania Geologists, 1998.
Whereas past interpretation of the Erie area included little of tectonic features, this field trip demonstrated the influence of movements along the bounding cross-strike structural discontinuities throughout the Phanerozoic on depositional environments and their resulting sedimentary rocks. The compressional features seen in northwestern Pennsylvania are a result of reactivation of pre-existing major fault zones. These zones are reactivated due to lineation with the current lithospheric horizontal stress field.
Stops on the trip illustrated Paleozoic sedimentation, sequence stratigraphy, oil and gas development, geology of the Lake Erie coastline, and horseshoe crab fossil sites.
Economic and Environmental Geology and Topography in the Allentown – Bethlehem Area. Sixty-fourth Annual Field Conference of Pennsylvania Geologists, 1999.
The Field Conference examined two of the active mainstay mineral industries of the Allentown-Bethlehem area – cement and aggregate – as well as a site of the now dormant jasper industry possibly used by Indians for as long as 10,000 years. The conference also examined the Heleva superfund site and a smaller, unheralded environmental site that poses numerous issues. In addition, attendees saw some of the oldest glacial deposits in Pennsylvania and the Ringing Rocks Boulder Field. The trip concluded with the view from the top of South Mountain and a discussion of the controls of the landscape.
Pittsburgh at the Millennium: the Impact of Geoscience on a Changing Metropolitan Area. Sixty-fifth Annual Field Conference of Pennsylvania Geologists, 2000.
Day one included a brief overview of the Pittsburgh area from atop Mt. Washington for orientation. After a stop to examine the impact of an old coal mine on the construction of the Mon-Fayette expressway, we boarded the US Army Corps of Engineers' "pleasure barge" for an excursion down the Monongahela and Ohio Rivers from Braddock to Emsworth. Field slowdowns along the way gave conferees the opportunity to view the making of a new dam, the redevelopment of old brownfields, and a variety of geotechnical problems associated with attempting to build and maintain roads on Pittsburgh's steep hillsides. Day two featured a visit to the Bruce Mansfield Power Plant in Beaver County where conferees had the opportunity to view the process of recycling scrubber sludge to make wallboard. We traveled to northern Allegheny County to examine what purportedly is the oldest documented major landslide in the world (Pennsylvanian age), and the structurally most complex area in Allegheny County. We also visited Fall Run Park, a small slice of native western Pennsylvania which has been severely impacted by surrounding sprawl.
2001: A Delware River Odyssey. Sixty-sixth Annual Field Conference of Pennsylvania Geologists, 2001.
Much of the conference took place in the Delaware Water Gap National Recreation Area (DEWA) (New Jersey and Pennsylvania). Emphases was on stratigraphy, structural geology, glacial geology, geomorphology, paleontology, and geoarcheology—but guidebook articles, field-trip stops, and pre-conference trips also dealt with mineral resources, historical geography, and ecology, among other topics. Day 1 of the conference field trip was mostly in New Jersey and highlighted stops at Delaware Water Gap, the Yards Creek Pump Storage Project, and High Point State Park. Day 2 was entirely in Pennsylvania and featured stops in the Schoharie Formation/Onondaga Limestone, an ice-contact delta, and a Mahantango shale-chip rubble deposit. The trip concluded with a grand synthesis of stratigraphy, glacial history, geomorphology, and geoarcheology at Raymondskill Creek and Falls.
From Tunkhannock to Starrucca: Bluestone, Glacial Lakes, and Great Bridges in the "Endless Mountains" of Northeastern Pennsylvania. Sixty-seventh Annual Field Conference of Pennsylvania Geologists, 2002.
The conference dealt mainly with the bedrock and glacial geology of Susquehanna County. Highlights of the field trip were stops at several active "bluestone," crushed-stone, and sand-and-gravel quarries, as well as visits to two of Pennsylvania's most impressive and historic railroad bridges, the great Starrucca (1848) and Tunkhannock (1915) Viaducts. Tying all these various aspects of the trip together is the "Summit sluiceway," a remarkable valley that cuts across the east-west stream divide in the central part of Susquehanna County. Formed by overflow from the various generations (pre-Illinoian to late Wisconsinan) of Glacial Lake Great Bend, the sluiceway was utilized by the Delaware, Lackawanna & Western Railroad as its major northward route from Scranton to the Great Lakes—culminating early in the 20th century with the completion of the "Summit cut-off" and the Tunkhannock Viaduct.
Geology on the Edge: Selected Geology of Bedford, Blair, Cambria, and Somerset Counties. Sixty-eighth Annual Field Conference of Pennsylvania Geologists, 2003.
For the first time in its history, the 2003 Annual Field Conference of Pennsylvania Geologists visited the Altoona area in west-central PA. Here, the Ridge and Valley Physiographic Province meets the Appalachian Plateaus Province along the Allegheny Front. Stops on Day 1 focused on the Silurian-Devonian carbonates in the lowlands of the Ridge and Valley. We examined excellent exposures of these units and addressed their stratigraphy, sedimentology, and paleontology, as well as their economic potential. In contrast, stops throughout Day 2 addressed the challenges of the geology and the landscape to the region's history, and blended the past and the present across the Allegheny Front. Highlights included: Fort Roberdeau, a reconstructed American Revolutionary stockade; a train excursion up the Front around the Horseshoe Curve and through Gallitzin's Tunnel Hill (re-enacting the first Field Conference in 1931); the Allegheny Portage Railroad National Historic Site; and an active strip-mine operation.
Conference Hosts: Pennsylvania Geological Survey, The Pennsylvania State University. New Enterprise Stone & Lime Co., Inc., Lock Haven University of Pennsylvania, Mountain Research, LLC.
For the first time in Field Conference history, we traveled to Delaware to examine the Wissahickon and the Wilmington Complex. A highlight of the Delaware excursion on Day 1 was a ride on the section of the historic Wilmington and Western Railroad that has been repaired since 2003's pre-hurricane storm rained destruction on the Delaware Valley. We then got a taste of our neighbors' hospitality with lunch at stop leader Peg Plank's house where we will also visit her quarry in the "Mt. Cuba" Wissahickon. We headed back through horse country in Chester County, PA to visit a quarry in the Cockeysville Marble and a typical Piedmont roadside outcrop of "Doe Run" Wissahickon. On Day 2, we visited Delaware County, PA to further explore the relationship of the Wissahickon to the Wilmington Complex arc and (finally!) see some "type" Wissahickon. We also looked at the Wissahickon in contact with Grenvillian gneiss of the Avondale Massif. At least we thought it was Grenvillian until zircons from the contact zone in this railroad cut gave a Silurian age.
The 2005 Field Conference visited glacial and bedrock sections in the Shenango and Beaver River valleys in northwestern Pennsylvania. The glacial sections included a complex section of glaciolacustrine sediments with a plethora of sedimentary structures at Cochranton. A lake bluff section on Pymatuning Reservoir at Pymatuning State Park addressed problems of glacial stratigraphy, history, sedimentology, and geomorphology. The Booth Run section exposed all 5 of White and others' (1969) Titusville Till sheets, separated by sand and gravel beds, and displayed some complicated weathering patterns. The bedrock sections include two type sections (Mercer and Homewood) described by I.C. White in the late 1800s. These were compared to modern exposures of the lower Allegheny – upper Pottsville interval, and illustrated why some of the type sections are "stereotype" sections. Also included were a stop at the Vanport Limestone, and an unusual asymmetric fold with multiple thrust faults at New Castle.
The 71st Annual Field Conference of Pennsylvania took place amid some of the grandest scenery in the northeastern United States, counting among its attractions two of Pennsylvania's most picturesque and geologically interesting state parks—Ricketts Glen and Worlds End. Ricketts Glen boasts 22 named waterfalls among its many attractions, and Worlds End has two spectacular scenic overlooks and (as far as we know) the biggest Pottsville "rock city" on the High Plateau. Emphasis was on the geomorphological development and glacial history of the region that encompasses North Mountain, Eagles Mere, and the uplands bordering Loyalsock Creek, but STOPS dealing with the stratigraphy and paleontology of the Lock Haven, Catskill, and Huntley Mountain Formations were also be included. Of particular stratigraphic and sedimentologic interest was a pre-Conference field trip to the enigmatic "Haystacks" in the upper part of the Huntley Mountain Formation on Loyalsock Creek. A second pre-conference field trip involved an all-day hike through the Glens and along the Highland Trail at Ricketts Glen State Park. A late addition to the "road log" will be discussions of the damage inflicted by the "no-name" flood of late June 2006.
The 72nd Annual Field Conference of Pennsylvania took place in the scenic and geologically fascinating area near Lewistown, located in the heart of Pennsylvania's picturesque Ridge and Valley province. The trip emphasized the products of recent geological mapping in the area surrounding the beautiful Kishacoquillas Valley – a locus of Amish and Mennonite farming. Geologic emphasis was on the reinterpreted structural geology of the area, which highlights pre-Alleghenian thrust faults that demonstrably were later refolded during the development of the Appalachian Mountains. Ordovician, Silurian and Devonian stratigraphy of the area was also highlighted with its local variations. The first day included examining the spectacular newly created road cut at the east end of the Lewistown Narrows where the Tuscarora and Rose Hill Formations may be seen in two very different structural settings. The remainder of the day included stops in no less than three quarries, each with structural complexities, including one in semi-consolidated Ridgeley sandstone with fossils. Day one lunch was atop Jacks Mountain featuring panoramic views of both adjacent valleys and ridge top quartzite stratigraphy. The first three stops of the second day examined the structural relationships of the pre-Alleghenian thrusting in the Kishacoquillas Valley starting with a stop at Reedsville to view "Trenton-Black River" stratigraphy and thrust fault structure. Overturned Bald Eagle conglomerate was seen at a stop demonstrating additional structures in the footwall of a refolded thrust fault. Then to road outcrops in the Ridgeley sandstone with a cross-bedded crag and a giant sinkhole in the Tonoloway Formation. Two pre-Conference Trips included a trip to an enigmatic boulder field of Ridgely sandstone that has no apparent source, and an underground excursion through the Rupert Cave in the Old Port Formation.
The 73rd Annual Field Conference of Pennsylvania offered a duel focus: the geology of the Mesozoic Gettysburg basin and the military geology of the battle of Gettysburg. In the history of the Field Conference only one STOP has examined Mesozoic rocks. An entire day was devoted to a geological transect across the Gettysburg basin. The Gettysburg basin is an erosional remnant of the early Mesozoic Birdsboro basin, formed on the roots of the Permian Alleghanian orogeny in the middle of Pangea near the edge of what was to become the Atlantic Ocean in the middle Jurassic. Approximately 7,000 m of mostly terrigenous sediment accumulated in an elongate trough (the Birdsboro basin) during the late Triassic and earliest Jurassic. We visited deposits of the various depositional environments, including the basal fanglomerate, the fluvial playa, the lacustrine and shoreline, and the upper fanglomerates. We also entered a quarry that exposes cycles in the Ordovician Beekmantown, and considered the tectonic implications for its presence within the Gettysburg basin. The second day of the Field Conference was spent entirely within the Gettysburg National Military Park. No famous land battle in all the annals of military history exemplifies the influence of topography and geology on the course and outcome of the engagement more than the battle of Gettysburg. From the Blue Ridge-South Mountain barrier that shielded the Confederate Army of Northern Virginia from the Union Army of the Potomac both during the movement to and retreat from Gettysburg to the spoke-like road network that led both armies to the fatal field to the rocky diabase fishhook upon which the Union forces anchored their final defensive position, the landscape dominated every phase of the Gettysburg campaign. We visited several of the well-known sites at Gettysburg National Military Park, including the railroad cuts west of town, the Lee Memorial on Seminary Ridge, Little Round Top, Devil's Den, the Peach Orchard, and the High Water Mark on Cemetery Ridge-emphasizing at each STOP how topographic and geologic conditions affected military tactics and results.
The 74th Annual Field Conference of Pennsylvania Geologists returned to northwestern Pennsylvania to celebrate the 150th anniversary of the founding of the modern petroleum industry by the successful completion of the Drake Well in Titusville on August 27, 1859. The first day of the field trip began by looking at an excellent outcrop of the uppermost Devonian Berea Sandstone and adjacent rocks in Oil City. From there we headed north along Oil Creek to relive the history of the early oil days. Stops included: the McClintock #1 well, the world's oldest producing oil well; Petroleum Centre, the heart of the industry during the early days; an early attempt to mine to the oil reservoirs; Blood Farm, with much of its old oilfield equipment still extant; Pithole, the famous ghost town that provides a sobering look at the rise and fall of an area in the throes of "black gold fever;" and Drake Well Museum where it all started. At the Drake Well, conferees also had the opportunity to examine an outcrop of the Upper Devonian "Drake Well Formation" (informal name) and search for fossils. The morning of day two was spent at a very complete esker-delta-lacustrine plain complex in northern Butler County. The new lidar images clearly show the complex. The story includes a couple of drainage diversions caused by the delta resulting in a stream that flows across and up its valley. In addition to the geomorphic relationships of the complex, we also had an opportunity to visit an active sand and gravel pit in the delta, and see the type of sedimentation that occurs in that environment. The afternoon of the second day of the Field Conference was devoted to reexamining the long-studied and long-debated end-Devonian stratigraphic succession in northwest Pennsylvania. Advances in global geochronology, recognition of the importance of the Hangenberg mass-extinction event, plus recent discoveries of apparent end-Devonian glacial activity have raised the stakes for improving our knowledge of the stratigraphy and paleontology in this regional time-slice. The results of extensive fieldwork in Crawford County and surrounding areas, as well as a partial review of the extensive and complex history of stratigraphic investigations of area sections will be presented.
In 1960 the Field Conference of Pennsylvania Geologists trip addressed "Some structural and tectonic problems of the Appalachian Piedmont along the Susquehanna River." Now on the 75th anniversary of the Field Conference and 50th anniversary of that trip, it is time to see what a host of geologists and other scientists enlightened by a half-century's diligent work and several scientific revolutions have done toward solving some of those 1960 problems. Many of those old problems have been largely solved whereas new data and greater sophistication have generated a new array of questions for the next generation. This trip is designed to take a brief look backwards at what has been accomplished, to provide an update of our present understanding of Piedmont tectonics and geology, and perhaps to provide a new set of problems for geologists of the next half century to puzzle over.
A pre-trip symposium on the afternoon preceding the trip will attempt to cover its basic tectonic themes in ten short talks summarizing different aspects of the region. The sequence of presentations is organized into a four-hour lecture series to give an overview through both time and space of the latest thinking and evidence about the tectonics of the Susquehanna Piedmont. A "map blast" and informal poster session will follow the symposium.
The second day's trip will focus on the Taconic foreland basin mostly in Dauphin and Lebanon Counties. Recent work by Ganis, Repetski and others has produced about 50 sites with high quality graptolite and/or condont dates. With these constraints, new mapping by Ganis and Blackmer has begun to make sense out of the Martinsburg flysch and its allochthons. These are now named as a separate formation, the sub-Martinsburg Dauphin Formation that has been thrust emplaced onto the carbonate platform and folded along with those carbonates and the overlying flysch into the Lebanon Valley nappe complex. These map relationships are at complete odds to traditional views of the Hamburg klippe as an erosionally isolated part of a late stage thrust sheet and suggest the "Hamburg klippe" term should be abandoned. The stops will demonstrate the stages of evolution of the Cocalico-Dauphin-Martinsburg foreland basin from the Myerstown Formation first disturbances of the platform carbonates, through emplacement from some distant deep sea source of the deep water Dauphin allochthons, to deposition of the overlying Martinsburg flysch and ultimately to gross overturning of it all as part of the Lebanon Valley nappe complex.
The 2011 Field Conference of Pennsylvania Geologists focused on the Permian- Carboniferous age rocks of the Dunkard Basin in Southwestern Pennsylvania, the northern panhandle of West Virginia, and Eastern Ohio. We looked at the youngest Paleozoic strata of the Appalachians exposed along winding roads built on the steep valley walls of this remote region. We closely examined the various lithologic features and fossils, touched on dramatic north to south facies change in the basin, and considered the paleoenvironmental and paleoclimatic implications of all of this. We once again asked the question about the age of Dunkard strata – Pennsylvanian or Permian? Attention was also be given to the unique topographic features of the region – the narrow, sinuous ridge tops and deep valleys shaped by strong headward erosion of streams and extensive landslides.
The Field Conference of Pennsylvania Geologists has in the past visited many sites along the Ordovician-Silurian boundary. The "transitional" contact between Silurian and Ordovician rocks in central Pennsylvania becomes unconformable in eastern Pennsylvania to southeastern New York as the hiatus widens. Following the northeastward decrease in intensity of deformation in the Ridge and Valley through New Jersey, this trip will begin with the high-angle contact between the Tuscarora and Hamburg sequence at the Schuylkill River and proceed for 120 miles along the very low-angle unconformable contact between Lehigh Gap, PA and Ellenville, NY. We will suggest predominant Alleghanian deformation along the contact and, in New Jersey and New York, propose zones of increasing southeastward Taconic deformation away from the contact. We will demonstrate the relative intensities and trends of Taconic and Alleghanian deformation in New York, and will comment on the northeastward dying-out of Alleghanian structures in the Shawangunk Mountains. The perplexing story of events during the Taconic hiatus, lasting perhaps 10-20 million years, will be illuminated by an unusual diamictite in southeastern New York.
The tale of two provinces examines the Great Amphitheater of Pennsylvania, the Nippenose Valley of Lycoming and Clinton Counties, inside and out on day one. The floor of this breached anticline exposes the Middle to Upper Ordovician, Bellefonte through Reedsville Formations. Just outside of the amphitheater are great exposures of the Marcellus, Tully, and Mifflintown. The second day is along US Route 15 corridor. There we examine excellent exposures of the stratigraphic succession from the Devonian Brallier/Harrell/Lock Haven into the Pennsylvanian Bloss coal complex of Pottsville/ Allegheny age, only to return back to the Lock Haven. It's a wild roller coaster ride from Williamsport to the New York border as you cross six "time zones" trying to figure out if it is half past the Devonian or a quarter after the Mississippian.
Ten sites present surficial, bedrock and economic geology, structure and geomorphology of South Mountain, the Great Valley and Blue Mountain, principally in Cumberland County. Of the ten, revisited with new interpretations are four classic sites visited by the Conference (one in 1982 and three in 1991). Five viewed quarries produce sandstone, limestone, shale and colluvium/alluvium. Presented are their diverse economic importance as well as their geologic aspects and interpreted history. Featured at one site are dye tracing of long distance ground water travel to a large springs. Paleontology is a sub-focus at two sites. Viewed respectively at two sites is autochthonous and allocthonous Ordovician Martinsburg sediments and markedly diverse structure. Friday evening banquet topic is the history of 19th century iron mining. Recent geomorphic investigations using LIDAR imagery provide new interpretations that allow reconstruction of Cenozoic paleotopography. Cretaceous lignite recovered in a core will be available for examination.
Date: October 16-18, 2014- GUIDEBOOK has three parts, due to size constraints. The last part is several of the preconference trips.
The first geological survey of Pennsylvania passed to the right and left of Indiana County leaving it a veritable "nether world" of geology. Since then, the "nether world" has been fleshed out and the 81st Annual Field Conference of Pennsylvania Geologists will highlight Indiana County and adjacent areas, rich in both energy and non-fuel minerals for over 100 years. We will look at past and present environments–warts and all. Stops and preconference trips currently being contemplated include: Johnstown 1889 flood site, Miss-Penn unconformity west of Johnstown, flint clay locales, Blacklick Gorge Geology along the Ghost Town Trail, Loyalhanna Limestone outcrops, a caving trip, local whitewater rafting and an AMD treatment site.
Day 1 (Friday morning) for a brief orientation on the geology (emphasizing the stratigraphy, structure and geomorphology) of Nittany Valley, from the Jo Hays look-out on Tussey Mountain. Thereafter Group 1 will proceed on the Shale Hills Critical Zone Observatory for the rest of the morning and relocate at the Pavilion for lunch at nearby Lake Perez. Group 2 will drive onto Huntingdon to examine outcrops of the Marcellus Shale, plumose joints in the Brallier Sandstone, and thin-skinned deformation in the shoaling upwards tidalite cycles of the Wills Creek Formation. Then Saturday groups will be segregated into disciplinary preferences themes of (a) Environmental/hydrogeology or (b) stratigraphy/engineering geology.
Leaders: David "Duff" Gold, Charlie Miller, Arnold Doden, Hubert Barnes, Richard Perizek, William White, David Yoxtheimer, Roman DiBiase, Ryan Mathur, Terry Engelder, Randy Farmerie, Michael Smith, Barry Scheetz.


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Titans Complete Interviews With Browns Assistant GM/VP of Player Personnel Glenn Cook, 49ers Director of Player Personnel Ran Carthon for the Team's General Manager Position
Jim Wyatt
Senior Writer/Editor
NASHVILLE – The Titans on Friday interviewed with Browns Assistant General Manager/VP of Player Personnel Glenn Cook and 49ers Director of Player Personnel Ran Carthon for the team's General Manager position.
Cook just finished his first season as the Browns assistant general manager and vice president of player personnel after being promoted from vice president of player personnel following the 2020 and 2021 seasons. Cook spent the previous four years as the club's assistant director of pro scouting.
According to the Browns media guide, in his role Cook works with Executive Vice President of Football Operations and General Manager Andrew Berry, as well as the rest of the senior football staff to contribute to all roster and strategic football decisions. Additionally, he leads the day-to-day operations of the player personnel department, including driving the free agency and draft processes. He also aids in managing the football operational functions of the team.
Cook, who played college football at Miami (Fla.) came to the Browns after spending four years in Green Bay (2012-15), working as a pro scout for the Packers.
Prior to joining the Packers in May 2012, Cook worked as a scouting assistant with the Indianapolis Colts beginning in June 2011.
Carthon is in his second season as director of player personnel with the 49ers after serving five seasons as the director of pro personnel in San Francisco.
According to the 49ers media guide, in his role Carthon is responsible for evaluating the top college prospects and assists in the construction of the pro free agency board and evaluations. He also works with the football administration staff with player market analysis and unrestricted free agency strategy.
Carthon joined the 49ers after spending five seasons (2012-16) as the director of pro personnel with the St. Louis/Los Angeles Rams.
Carthon also spent four seasons (2008-11) as a pro scout with the Atlanta Falcons.
Prior to his time in Atlanta, Carthon enjoyed a three-year playing career in the NFL after playing in college at the University of Florida. He broke into the league as an undrafted rookie with the Indianapolis Colts in 2004 and played with the club through the 2006 campaign.
The Titans on Thursday interviewed in-house candidates Ryan Cowden and Monti Ossenfort for the team's general manager position.
Interviews with other candidates will continue in the coming days.
Back on December 6, Titans controlling owner Amy Adams Strunk made the decision to part ways with general manager Jon Robinson, who was hired prior to the 2016 season.
Strunk is leading the process of finding his replacement, and the plan is to interview a large number of candidates, including personnel evaluators across the NFL.
Strunk said a committee including herself, Kenneth S. Adams, IV from the ownership group, President and CEO Burke Nihill, Senior VP/Business Affairs and Chief Legal Officer Adolpho Birch III and Senior VP/General Counsel & Chief of Staff Dan Werly will be involved in the interviews.
"We want someone who is an exceptional talent evaluator, exceptional at roster building, and someone who is an excellent decision-maker," Strunk said in recent interview. "I also want someone who is a collaborator, someone who is able to find and build consensus to get to the best answers for the team, someone who is open to innovation and evaluating talent beyond the traditional avenues. Just really a talented person in all areas. But more than anything I want someone that can collaborate – that is super important to me, being able to find this person who can collaborate so we're all working together, rowing the same direction.
"I am excited about the process, and I am excited about finding the right person. I think this is going to be a great reset for us going forward, a chance to bring in new ideas, a new way of doing things."
From the Senior Bowl: Titans Assistant Clinton McMillan Coaching Prospects – and Also Learning About Them – Leading Up to the NFL Draft
McMillan, who just finished his second season with the Titans and his first year as defensive line assistant, is coaching linebackers for the American Team this week.
From the Senior Bowl: Titans HC Mike Vrabel Talks Draft Prospects, Working With New GM Ran Carthon and More
First impressions mean a lot to Titans coach Mike Vrabel, and here at the Senior Bowl, he's getting a look at some of college football's top prospects for the first time.
From the Senior Bowl: Titans GM Ran Carthon Living His Childhood Dream While Keeping His Focus on the "Main Thing"
Here at the Mobile Convention Center and at Hancock Whitney Stadium on the campus at the University of South Alabama, Carthon has received a lot of handshakes and hugs from those wishing him congratulations.
From the Senior Bowl: Former Vols QB Hendon Hooker Looking to Make a Good Impression on NFL Teams
While Hooker can't take part in the action right now because of the torn ACL he suffered in November, he's doing everything else to feel a part of it as he embarks on his NFL career.
Why the Titans Are Switching to Turf at Nissan Stadium Starting in 2023
The new playing field at Nissan Stadium will be similar to the surface and infill that is currently used inside the team's indoor practice facility at Ascension Saint Thomas Sports Park, and also used in other practice facilities across the NFL.
Tuesday Mailbag: Jim Wyatt Answers Questions From the Senior Bowl
Senior Writer and Editor Jim Wyatt tackles another batch of questions from Titans fans.
Titans Center Ben Jones Named to Pro Bowl Roster
Jones on Monday was named to the Pro Bowl roster as a replacement for Chiefs center Creed Humphrey, who is headed to the Super Bowl.
Who Will the Titans Pick? First Tour of the Mock Drafts at the Start of Senior Bowl Week
The Titans are scheduled to pick at No. 11 in the NFL Draft. So, who will the Titans pick? Let's take our first your of the mocks, and a look at what draft analysts think the Titans will do.
Weekend Mailbag: Jim Wyatt Answers Questions From Titans Fans
Senior Writer and Editor Jim Wyatt tackles another batch of questions in the latest edition of the mailbag.
Titans LB David Long Jr. on His Future in Tennessee: "Of Course I'd Love to Stay Here"
In four NFL seasons, Long has tallied 226 tackles, 12 quarterback pressures, and four interceptions while playing in 50 games, with 26 starts.
After an Injury-Shortened Rookie Season, Titans WR Kyle Philips Motivated to do More in 2023
A fifth-round pick in the 2022 NFL Draft by the Titans, the shifty receiver from UCLA turned heads during offseason workouts. When training camp began, he picked up where he left off, winning one-on-ones against teammates, and also against veteran DBs in work against the Buccaneers and Cardinals.
ESPN's Mel Kiper Jr. Tackles Pick No.11 for Titans in his First Mock Draft
ESPN's Mel Kiper Jr. released his first mock for the upcoming draft, and the draft guru has the Titans taking Ohio State offensive tackle Paris Johnson Jr. in the first round.

redpajama_set_name: RedPajamaCommonCrawl


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Ellington's Belgravia Heights I project in JVC breaks ground
Ellington / Media Center / Ellington Properties Dubai News / Ellington's Belgravia Heights I project in JVC breaks ground
· The brand new development boasts a landscaped podium level with a resort-style pool, children's play area and a modern fitness centre
Dubai, UAE; March 7, 2018: Ellington, the Dubai-born design-led boutique developer with a growing portfolio of bespoke, aesthetic and high-quality homes, broke ground on its Belgravia Heights I project.
Belgravia Heights I is situated in Dubai's popular Jumeirah Village Circle (JVC), and follows the successful introduction of three projects under the same brand name of Belgravia.
The ground-breaking ceremony took place in the presence of home owners, architects, investors, agents and other partners.
Robert Booth, Managing Director, Ellington, said: "Belgravia Heights' I architects have followed the signature design of the Belgravia collection as we extended the brand to reflect Ellington's key values and commitment to timeless design and quality. The residential building follows its sister projects Belgravia I, II and III, and commands a signature position along one of the main boulevards running through the community."
Ideal for young couples and families, Belgravia Heights I is a uniquely designed residential building in the heart of JVC with 155 spacious studios, and 1 and 2-bedroom units. It has a landscaped podium level with a resort-style pool; children's play area and a modern fitness centre. The interiors are serene with warm colours offering a contemporary edge that enables residents to define their personal style.
The design of the building together with an active retail streetscape and elevated amenity floor creates a dynamic and engaging community feel to all aspects of the development.
Other projects announced recently by Ellington include the highly sought-after Wilton Terraces I and II at Mohammed bin Rashid City (MBR City), a freehold community of lavish villas, Quad homes and apartments, set along the Dubai Water Canal; and the 'topping out' of Eaton Place – a building elegant and contemporary in architecture, offering 1 and 2 bedroom residences which will be completed in mid-2018.


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Peter Konstantinov Deunov (en , translittération latine Petăr Konstantinov Dănov, prononciation ) (- à Sofia) est un philosophe et maître spirituel à l'origine de la Fraternité Blanche.

Il était appelé Maître Beinsa Douno (en bulgare: Учителя ) par ses disciples.

Biographie

Peter Deunov naît le  à Nikolaevka (tout près de Varna, Bulgarie). Troisième enfant du pope orthodoxe Constantin Dǎnovski et de Dobra Georgieva. Son grand-père maternel était Atanas Georgiev (1805-1865), une figure publique active dans la lutte pour l'indépendance de l'Église bulgare lors du rétablissement de la nation bulgare aux , quand la Bulgarie était sous domination turque. Son père, Constantin Dǎnovski (1830-1918) était le premier professeur bulgare dans la région de Varna et le premier pasteur de Varna, avant la libération de la Bulgarie de l'Empire ottoman (1878).

Peter Deunov est élève à l'école secondaire de Varna de 1880 jusqu'au printemps 1884 quand il tombe gravement malade. Cette maladie est un tournant dans sa vie. Guéri, il poursuit ses études à partir de janvier 1885 à l'École américaine des sciences et de la théologie à Svištov. Là, ses études au lycée de Varna sont reconnues et après un an et demi à Svishtov, le 24 juin 1887 il reçoit un certificat d'achèvement d'un programme d'études complet de cinq ans au département de théologie de l'école américaine.

Au cours de l'année scolaire 1887/88, Petar Deunov était prédicateur et enseignant à l'école primaire méthodiste du village Hotantsa, près de Roussé.

En été 1888, il part pour les États-Unis avec recommandations pour étudier avec une bourse au Séminaire méthodiste théologique de Drew de Madison, au New Jersey. Il s'inscrit et y complète ses études . Puis il devient etudiant à l'école de théologie de l'université de Boston, dans le Massachusetts, où il présente une thèse sur La migration des peuples germaniques et leur christianisation et obtient son diplôme en . À partir de 1893, il est étudiant à l'école de théologie de l'université de Boston.

En 1895 (à 31 ans), Peter Deunov décide de retourner en Bulgarie et s'établit à Varna. Il refuse tous les postes qui lui sont offerts comme pasteur méthodiste et théosophique mais participe activement à la vie publique, s'efforcant d'élever l'esprit, l'éducation et la culture du peuple. En 1896, il publie le livre Science et Éducation, dans lequel montre les directions de son travail futur et les principes de base, qu'il développera plus tard en détail : la relation entre la religion et la science et la nécessité de leur interaction, la nécessité de moderniser et d'appréhender scientifiquement la vision du monde religieuse, le développement de la capacités de la nature supérieure (le principe divin en l'homme) grâce à des méthodes scientifiques et éducatives correctes, l'idée de l'intégrité de l'univers et de l'homme dans le cadre d'un organisme collectif commun.

En 1896, il est l'un des fondateurs du Centre culturel et communautaire « P. R. Slavejkov ». Il y est élu bibliothécaire, et dans les années suivantes il prononce les conférences suivantes devant les habitants de Varna : « L'origine de l'homme », « Étude sur les philosophies ancienne et moderne », « Science et philosophie », « Pourquoi et comment nous vivons » et « La base de l'éclaircissement ».

En 1897, à 33 ans, Peter Danov a une expérience mystique - la descente de l'Esprit Divin sur lui. C'est un moment clé de sa vie (comme la maladie qui le tourne vers le Dieu). Cela se passe le 7 mars à Varna. On pense qu'alors il accepte le « devoir »  d'un Maître spirituel qui s'est incarné dans son corps. Cette obligation spirituelle, combinée à une position civique, Peter Danov suivit avec constance jusqu'à la fin de sa vie terrestre, travaillant parmi le peuple bulgare «pour leur acceptation de l'amour divin, de la sagesse et de la vérité, comme l'idéal le plus élevé pour l'homme».

En même année 1897, Peter Deunov, avec quelques-uns de ses partisans, fonde à Varna une Sociét pour l'Élévation de l'Esprit Religieux du peuple bulgare. Les membres sont suivants (selon le protocole de 1903) : Georgi Mirkovič, Maria Kazakova, Todor Stojanov, Penju Kirov, Anastasia Jelyazkova et Milkon Partomjan. Il écrit une brochure de textes mystiques intitulée Hio-Eli-Meli-Mesail (publiée plus tard, en 1900). Pendant l'année suivante, il écrit et donne une conférence, Appel à mon peuple - fils bulgares de la famille slave, devant la Société de la Charité de la Mère de Varna. Cette conférence est un appel à l'auto-identification sociale et spirituelle. En 1899, il enregistre Les dix témoignages de Dieu et La promesse divine.

Les événements de 1897 le placent au centre de la société spirituelle qu'on  commence d'appeler la Chaîne.  Plus tard, en 1912, Petar Deunov dit qu'ils représentent la Fraternité Blanche, déclarée par lui comme une branche de la Fraternité Blanche Universelle, représentée dans le passé par les Bogomiles en Bulgarie. Après 1897, il est fait référence à lui comme Maître Beinsa Douno, nom qui apparait dans les publications littéraires dans les années 1930. L'étymologie du nom Beinsa Douno a probablement des racines en Sanskrit et se traduit par : « Celui qui amène le bon à travers les mots ».

À partir de 1900, Beinsa Douno convoque des réunions annuelles, d'abord nommées Réunions de la Chaîne. Dès lors et jusqu'en 1942, la Fraternité Blanche a tenu ses réunions annuelles du mois d'août en plusieurs lieux : Varna (1900, 1903, 1906-1909), Bourgas (1901, 1902 et 1904), Veliko Tărnovo (1910-1925), Sofia (1926-1941), et sur les  montagnes du Rila et du Vitocha.

De 1901 à 1912, il voyage en divers lieux de Bulgarie, donne des conférences et fait des interprétations phrénologiques d'individus sélectionnés parmi les gens. Dès 1904, il réside assez longtemps à Sofia et commence à donner ses conférences publiques. La figure historique, cosmique et métaphysique du Christ a une place centrale dans ses conférences. En 1912, dans le village d'Arbanasi (près de Veliko Tărnovo), il travaille sur la Bible et prépare Le testament des rayons de couleur de la lumière qui sort en septembre de la même année. La page titre avait une devise : « Je serai toujours un esclave fidèle au Seigneur Jésus-Christ - le Fils de Dieu, , Tărnovo ».

Le , il donne sa première causerie dominicale qui a été prise en sténographie et ayant pour titre : Voici l'homme; elle débute la série Force et vie. Le maître Beinsa Douno expose les principes généraux de son enseignement qu'il appelle Le Nouvel Enseignement de la Fraternité Blanche Universelle. Le  à Sofia, il commence une autre série de conférences spéciales pour les femmes mariées, connu comme le cycle Grande Mère, qui va durer chaque jeudi jusqu'au . Pendant la période 1917-1918, au cours de la Première Guerre mondiale, le gouvernement de Vasil Radoslavov l'envoie en exil à Varna sous prétexte que son enseignement affaiblit l'esprit des soldats au front, et à cause de son opinion que la Bulgarie ne devrait pas participer à la guerre. Il habite l'hôtel de Londres (actuel hôtel Mousala) et correspond avec ses partisans. À la fin de la Première Guerre mondiale en 1918, le nombre de ses partisans dans tout le pays grandit rapidement; vers 1936, on en compte approximativement , et il y a aussi ceux de l'étranger.

Le , il ouvre une école ésotérique à Sofia qu'il appelle École de la Fraternité Blanche Universelle. Le cours consiste en deux classes d'étudiants : classe ésotérique générale et classe ésotérique spéciale. La classe ésotérique générale est destinée aux auditeurs de tout âge et de tout statut matrimonial, et la classe ésotérique spéciale est réservée aux jeunes personnellement invités par lui. Les conférences ont été données devant les deux classes ésotériques une fois chaque semaine pendant 22 ans — jusqu'en .

En 1927, le maître Beinsa Douno s'implante dans le village d'Izgrev près de Sofia (aujourd'hui un secteur résidentiel de la ville) où il rassemble son public, ses partisans et disciples pour avoir un centre où l'école ésotérique peut travailler. Il s'installe en permanence à Izgrev, où il partage plusieurs parties de son enseignement. Dès le , il donne une série de conférences lors de la réunion annuelle de la Fraternité Blanche, série qui comprend entre autres l'intitulé : La voie d'un disciple.

Entre 1929 et 1932, Maître Beinsa Douno établit le contact avec l'ex-théosophe Jiddu Krishnamurti (dans la ville d'Ommen, aux Pays-Bas) qui vient de quitter à cette époque la Société théosophique, après avoir dissous le  l'Ordre de l'Étoile d'Orient.

À l'été 1929, il amène ses disciples camper pour la première fois près des Sept Lacs du Rila. Le , il ouvre une nouvelle session de son enseignement, appelée « conférence du dimanche matin » et qui a duré jusqu'en . En 1934, il commence à travailler sur la Paneurythmie : une série de vingt-huit exercices qui consistent en mélodies, textes et mouvements plastiques. Plus tard, il ajoute les exercices sur les rayons solaires et le pentagramme.

Le , il est sauvagement battu et malmené par un extrémiste politique, ce qui lui cause une hémorragie cérébrale et une paralysie. Malgré cela, à peine rétabli mais encore faible, le maître Beinsa Douno va camper avec ses partisans, le , tout près des Sept Lacs du Rila. Le , il estime avoir récupéré la santé.

Le , il écrit un message à ses disciples intitulé Le testament éternel de l'Esprit.

Au début de l'an 1944, lors des attaques aériennes à Sofia, il va avec un petite groupe à Mărčaevo (un village non loin de Sofia) et demeurent chez un de ses disciples (aujourd'hui maison-musée de Deunov). Beaucoup d'autres arrivent aussi еt s'installent dans le village, et d'autres arrivent périodiquement de Sofia. La vie de la Fraternité continue dans ce village au pied de Vitosha, où a lieu sa dernière réunion annuelle

Il revient à Izgrev le . Le , il donne sa dernière conférence, La dernière parole, à la classe ésotérique générale.

Il décède le . Son corps est enterré à Izgreva.

Peter Konstantinov Deunov était végétarien.

Contribution créative

Doctrine idéologique et méthodologique

Plusieurs aspects dans l'enseignement du maître Beinsa Douno sont disposés et développés dans plus de  conférences, qui ont été données et sténographiées durant la période 1900-1944. Elles ont été publiées dans plusieurs séries de volume : les conférences devant la classe ésotérique générale ou devant la classe ésotérique spéciale, les causeries dominicales, les conférences de la Réunion Annuelles, les conférences matinales, etc.

Les principaux thèmes de son enseignement sont : l'amour, la sagesse, la vérité, la justice et la vertu, compris comme attributs du Christ historique, cosmique et mystique. L'amour est une catégorie centrale du macrocosme et du microcosme, qui fonctionne dans plusieurs aspects de l'existence humaine comme aspiration (dans la sphère émotionnelle ou le cœur), sentiment (dans l'âme), pouvoir (dans la sphère idéale du « je » ou la raison) et principe (dans l'esprit). La Grande Fraternité Universelle est la vision fondamentale cosmogonique. Elle est décrite comme un organisme, consistant en âmes humaines avancées (loges du Grand Initié et leurs disciples) et les neuf hiérarchies d'êtres super-sensibles (les Anges, les Archanges, les Principautés, les Vertus, les Puissances, les Dominations, les Trônes, les Chérubins et les Séraphins). D'après le Maître Beinsa Douno, le Christ est le gouverneur suprême de la Grande Fraternité Blanche Universelle.

L'histoire de la culture mondiale est vue comme la projection d'un rythme cosmique, structuré dans des périodes globales et des sous-périodes. Les périodes sont comme suit : Polaire, Hyperboréenne, Lémurienne, Atlantéenne, Cinquième, Sixième et Septième périodes. Les sous-périodes de l'actuelle Cinquième période sont aussi appelées ères culturelles : l'ère du Cancer (Indien Ancien), du Gémeaux (Persan Ancien), du Taureau (Égyptien Ancien), du Bélier (Grèce Ancienne et Rome), du Poisson (Européen De l'ouest), du Verseau (Slave) etc. La conscience humaine se manifeste et se développe à travers des étapes collectives, individuelles, collectives suprêmes et cosmiques. D'après le Maître Beinsa Douno l'humanité entre dans l'ère du Verseau depuis 1914, c.-à-d. la mise en œuvre de la transition évolutionnaire de la cinquième à la sixième ère culturelle dans la cinquième période. Pendant cette ère, d'après le Maître Beinsa Douno, la race Indo-européenne est chef de file dans un aspect évolutionnaire. Les premières étapes dans la conscience collective suprême sont faites pendant l'étape de la transition actuelle. Une de ses formes sociales s'est accomplie à travers les aspects suprêmes de l'amour - la vie pour le Tout. La conscience collective étendue, en rendant effective la vie pour le Tout, est considérée comme un attribut de la prochaine sixième ère culturelle et de la future sixième race qui provient d'elle. D'après le Maître Beinsa Douno, la sixième race se manifestera dans la future sixième grande ère et rendra effective la culture de l'amour à une bien plus grande étendue.

L'aspect psychologique du développement humain d'après le Maître Beinsa Douno est une transformation importante à travers quatre archétypes culturels : l'Ancien Testament, le Nouveau Testament, le Vertueux et le Disciple. Cette dernière transition comprend un ensemble de méthodes scolaires ésotériques, qui vise la transformation de la conscience idéale et conceptuelle dans l'imaginaire et est désigné par l'expression : l'épanouissement de l'âme humaine. D'après le Maître Beinsa Douno, les disciples ésotériques lient leur conscience en permanence avec le Christ, l'expérimentent constamment dans leur intellect, leur émotion et leur volonté et apprennent constamment de ce qu'Il accomplit en eux. Donc la conscience du disciple, ou plus spécifiquement son corps éthérique, est perçu comme objet et sujet du soi-disant Second avènement du Christ.

Les principales méthodes employées pour le travail spirituel à l'École de la Fraternité Blanche sont : les prières communes, les exercices musicaux et respiratoires, les lectures de la parole du Maître Peter Deunov, le salut au soleil levant, des sorties dans les montagnes, la vie fraternelle en communauté, des rassemblements annuels, etc. Les méthodes particulières sont : Le Testament des couleurs et la danse de la Paneurhythmie. Toutes ces méthodes sont regardées comme des pratiques pour une expérience du Christ à travers l'être humain entier, et plus particulièrement le corps éthérique.

Paneurythmie et musique

La paneurythmie est un système d'exercices spécifiques avec accompagnement musical créé par Peter Deunov entre 1927 et 1944, visant à la fois à améliorer et à maintenir la santé et à stimuler le développement harmonieux de la personnalité, en atteignant l'harmonie avec la nature (l'univers).

La paneurythmie a une base philosophique profonde et combine la musique, le mouvement, la pensée et la parole dans un tout harmonieux. Sous un autre aspect, elle est aussi « à la fois prière, méditation, contemplation et maîtrise ».

La paneurythmie se compose de trois parties, qui sont exécutées l'une après l'autre : la première partie, appelée 28 exercices, la deuxième partie — Rayons de soleil, et la troisième partie — Pentagramme. La durée est au total d'environ 70 minutes ou plus.

Peter Deunov a écrit de nombreux chants et diverses compositions. Il jouait remarquablement du violon.

Livres
« L'enseignement du Maître Deunov » a été donné sous forme de conférences, sténographiées par ses disciples dès 1921.
 Le Maître parle, Courrier du livre, 1964, 129 p. : « La Vie, l'Âme, la Vérité, l'Amour... »
 La Vie pour le Tout, Courrier du livre, 3° éd. 1989, 126 p.
 Dans le Royaume de la Nature vivante, Courrier du livre, 1989, 119 p.
 Le futur credo de l'humanité
 Au cœur de la santé, Books on Demand, 2008, 300 p.
 L'amour universel, source de vie (1942), Courrier du livre, 1964, 175 p.
 La Loi suprême (1925), Courrier du livre, 1990, 125 p.
 L'enseignement de vie nouvelle, Courrier du livre, t. I 1983, t. II 1991.
 Le livre des anges, Ultima, 2007, 254 p.
 Le livre de l'éveil. L'entrée de la conscience dans les mondes supérieurs, Ultima, 2006, 268 p.
 Paneurythmie, Éditions Amour et Vie, 1954, 29 p.
 Propos sur l'avenir (1944)  Prophétie.
 Conversations avec le Maître, in L'enseignement de Maître Deunov. Présentation, témoignages, textes et entretiens, Le Courrier du Livre, 1990, .
 La Respiration dans l'enseignement du Maître Deunov, Le Courrier du Livre, 1984, 128 pages.

Musique
 Chants de la F.B.U., Fréjus, Prosveta, 2007, 265 p.
 Chants mystiques bulgares (1923-1924), Fréjus, Prosveta, 1997 (disque compact)
 Paneurythmie. Version orchestrée, Fréjus, Prosveta, 2002.

Omraam Mikhaël Aïvanhov
L'organisation française Fraternité Blanche Universelle est instituée par son disciple Mihail Ivanov, connu comme Omraam Mikhaël Aïvanhov (1900-1986) qui a rencontré Peter Deunov à dix-sept ans, en 1917, à Varna, et l'a suivi jusqu'en 1937.

Selon Aïvanhov, « C'est donc sur la demande du Maître Peter Deunov que je suis venu en France [] pour continuer à faire vivre son enseignement. Bien sûr, il ne m'a pas ordonné de partir, un véritable Maître n'exige pas l'obéissance et la soumission de ses disciples. C'est moi qui ai senti que ce qu'il me demandait était pour le bien, et j'ai accepté. » Cependant, selon les témoignages des disciples dе Deunov, Ivanov n'a pas été envoyé par le Maître. En 1937, il part pour la France à l'Exposition universelle et reste à Paris. N'ayant contact direct avec Deunov, il demande dans une lettre Boyan Boev, une des figures proches de Deunov, de demander le Maître si c'est bien d'y rester pour faire des études; la réponse (toujours transmise par Boev) est que, s'il a la possibilité et les moyens d'étudier, qu'il y reste. Ivanov commence à donner des conférences publiques sur des sujets spirituels.

Notes et références

Voir aussi

Études sur Peter Deunov
 Omraam Mikhaël Aïvanhov, Auprès du Maître Peter Deunov, Éléments d'autobiographie 2, Fréjus, éditions Prosveta, 2010, 452 p.
 Omraam Mikhaël Aïvanhov, Hommage au Maître Peter Deunov, Fréjus, éditions Prosveta, 1991, 114 p.
 M. Konstantinov, etc., Le Maître Deunov, Omnium littéraire, 1959.
 L'enseignement de Maître Deunov. Présentation, témoignages, textes et entretiens, Courrier du livre, 1990, 319 p.
 Frida Theodosy, L'art du chant divin : méthode de développement spirituel et d'union cosmique suivant l'enseignement des maîtres Peter Deunov et O. M. Aïvanhov, Hérouville-Saint-Clair, Éd. Télesma, 1990, 96 p.

Articles connexes
 Fraternité Blanche Universelle

Liens externes

Religieux bulgare
Philosophe bulgare
Occultiste
Chef religieux du XIXe siècle
Chef religieux du XXe siècle
Naissance en Bulgarie
Naissance en juillet 1864
Décès en décembre 1944
Décès à 80 ans
Personnalité végétarienne
Décès à Sofia

redpajama_set_name: RedPajamaWikipedia


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text:
Enar Alexius Werner, född 27 juni 1902 i Göteborg, död 17 april 1981 i Falsterbo, var en svensk väg- och vattenbyggnadsingenjör.

Werner, som var son till handlanden Theodor Werner och Olga Strömbom, avlade studentexamen 1921 och utexaminerades från Chalmers tekniska institut 1925. Han var ingenjör på stadsingenjörskontoret i Göteborgs stad 1926 och 1928–1930, på gatukontoret där 1925 och 1927, hos länsarkitekt Nils A. Blanck i Malmö 1930, stadsplaneingenjör på stadsingenjörskontoret och stadsplanekontoret i Göteborgs stad 1931–1955, blev överingenjör där 1955 och utredningschef för planeringen av Angered och Bergum på stadsbyggnadskontoret i Göteborgs stad från 1962. Han skrev Angered-Bergum. Göteborg växer norrut (i Göteborg förr och nu, 1964).

Källor

Svenska väg- och vattenbyggnadsingenjörer
Kommunaltekniker i Göteborg
Födda 1902
Avlidna 1981
Män
Ingenjörer från Göteborg
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In 2018 global sales of plug-in light electric vehicles reached 2 million.
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What a 5 Hour Drive to Lubbock, Texas is Like
December 13, 2019 July 2, 2016 by Eva Chung
During my one month stay in Texas, my boyfriend and I took a drive to Lubbock because he had to visit for school orientation. We stayed there for 2 days. I have to say though, Lubbock has nothing there but Texas Tech School. The school is gorgeous, stunning, and large, but every where else in the general area, meh. I don't have too many pictures from Lubbock because we were simply too tired from the long 5 hour drive there. However, I did take some pictures of our drive there to pass the time.
On a side note, I'm not one to enjoy long car trips because I have a bladder the size of a tennis ball, so it wasn't too pleasant of a trip. I was thirsty from not drinking water and had to constantly resist the urge to go to the washroom and limit it to once per drive there and back. The views was the only thing that kept me sane (beside my boyfriend as well) on the drive to Lubbock.
I honestly never thought I would like windmills so much because they're so straight forward and plain. However, after driving by many fields and seeing them up close, they're actually very therapeutic to look at and stunning in a minimalistic way. Does anyone else feel that way when look at windmills?
The drive there was also interesting. We went from Frisco to Lubbock and there were many tiny towns that we drove through. They were very old-school looking, much like that I had imagined the Wild West of Texas to look like from cartoon stereotypes. The lifestyle seemed very simple and quiet. I think in one point of my life, I'd love to try living in one of those tiny towns to see what it's like.
Where in Texas would you recommend me visiting next time?
Looking to travel to Texas soon? Check these out:
16 Instagram Worthy Places on Texas Tech University
A Day at the Palo Dura Canyon, Texas
What You'll Find in the Dallas Arboretum Botanical Garden
Follow me on Instagram @itsevachung for more pictures!
Categories Travel, United States Tags dallas, lubbock, road trip, texas, texas tech, travel diary, wanderlust Post navigation
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Area Schools Face Deep Budget Cuts
A proposed $84.8 million cut in the FY2012 annual Superintendent's budget will force the area schools in the county to have less staff and larger class sizes.
The original proposed budget was $1.68 billion, with a projected $64 million shortfall from the state. The governor has announced an additional $20.8 million cut to school system funding.
The new cuts would increase class sizes and eliminate more than 700 in-school positions, according to PGCPS documents.
The proposed budget cuts have prompted the school board to wage a campaign asking school parents to call Gov. O'Mally " Please help Maryland hold its place as #1 by fully funding education. Funding cuts hurt Prince George's County more than any other school system in the State", says school board's website.
The proposed cuts follow a similar cut in the previous year, which resulted in almost 800 job cuts. The job cuts put Prince George's County at the top for job cuts for all school systems in the Washington area.
Last Thursday, the Board of Education arranged a public hearing, where many parents, school teachers spoke against the proposed cuts.
Additional public hearings have been scheduled on February 8, & February 10. The Board of Education will have FY 2012 budget work sessions on February 24, when it is expected to adopt the new budget.
School | Fazlul Kabir February 5, 2011