Law Building

Jordan & Anderson, architects. Completed in 1863. Served as Law School for 60 years; contained University Chapel until 1873 and Library until 1883. Addition in 1893 included tower; additional space added in 1898. Tower removed in 1898 addition and renovation. Room for Regents built in new south wing; they met there for 35 years. Upon completion of Hutchins Hall in 1933, the Law Building was renamed Haven Hall and was used by Literature Science & the Arts. It burned on June 6, 1950. It was located at the northwest corner of the Diag, corner of State and North University.

Law Building

Jordan & Anderson, architects. Completed in 1863. Served as Law School for 60 years; contained University Chapel until 1873 and Library until 1883. Addition in 1893 included tower; additional space added in 1898. Tower removed in 1898 addition and renovation. Room for Regents built in new south wing; they met there for 35 years. Upon completion of Hutchins Hall in 1933, the Law Building was renamed Haven Hall and was used by Literature Science & the Arts. It burned on June 6, 1950. It was located at the northwest corner of the Diag, corner of State and North University. With picket fence.

Law Building

Jordan & Anderson, architects. Completed in 1863. Served as Law School for 60 years; contained University Chapel until 1873 and Library until 1883. Addition in 1893 included tower; additional space added in 1898. Tower removed in 1898 addition and renovation. Room for Regents built in new south wing; they met there for 35 years. Upon completion of Hutchins Hall in 1933, the Law Building was renamed Haven Hall and was used by Literature Science & the Arts. It burned on June 6, 1950. It was located at the northwest corner of the Diag, corner of State and North University. With picket fence. On verso: Photographed in 1887 by A.L. Colton, class of '89.

Law Building

Jordan & Anderson, architects. Completed in 1863. Served as Law School for 60 years; contained University Chapel until 1873 and Library until 1883. Addition in 1893 included tower; additional space added in 1898. Tower removed in 1898 addition and renovation. Room for Regents built in new south wing; they met there for 35 years. Upon completion of Hutchins Hall in 1933, the Law Building was renamed Haven Hall and was used by Literature Science & the Arts. It burned on June 6, 1950. It was located at the northwest corner of the Diag, corner of State and North University. Several people in distance.

Law Building

Jordan & Anderson, architects. Completed in 1863. Served as Law School for 60 years; contained University Chapel until 1873 and Library until 1883. Addition in 1893 included tower; additional space added in 1898. Tower removed in 1898 addition and renovation. Room for Regents built in new south wing; they met there for 35 years. Upon completion of Hutchins Hall in 1933, the Law Building was renamed Haven Hall and was used by Literature Science & the Arts. It burned on June 6, 1950. It was located at the northwest corner of the Diag, corner of State and North University.

The temple of Deir el Bahari,

Twelfth memoir: 32 1/2 x 25cm.

Report of the Illinois Green Government Coordinating Council.

The Illinois Green Government Coordinating Council promotes the incorporation of pollution prevention and resource conservation practices into government management and operations. The Council works with state agencies to reduce waste, improve energy efficiency, conserve water, increase recycling and reuse of materials, incorporate green building principles into new construction and renovation projects, and acquire and use environmentally friendly products.

Sustainability planning guide for Illinois state agencies.

The Illinois Green Government Coordinating Council promotes the incorporation of pollution prevention and resource conservation practices into government management and operations. The Council works with state agencies to reduce waste, improve energy efficiency, conserve water, increase recycling and reuse of materials, incorporate green building principles into new construction and renovation projects, and acquire and use environmentally friendly products.

Rackham Blg. [Building] construction

View facing north and cityscape. Framing for terrace room east end of building. Additional framing third floor west end. Scaffolding from east tower to building. No. 22 of chronological series of construction photographs, numbered 1 to 32. Smith, Hinchman & Grylls, architects. W.B. Wood Co., construction

Rackham Blg. [Building] construction

Stonework begun in terrace room. Friezes in place on second floor front of building. No. 28 of chronological series of construction photographs, numbered 1 to 32. Smith, Hinchman & Grylls, architects. W.B. Wood Co., construction

Athletics Ad. Bldg. [Administrative Building], June 1950

Fry and Kasurin, architects. Building had several uses. From 1912-1913, it was a clubhouse; from 1917-1955 an administrative building. In 1925 there was extensive renovation on the building. Back of building faces west. Demolished in 1974.

Field House

Fry and Kasurin, architects. Building had several uses. From 1912-1913, it was a clubhouse; from 1917-1955 an administrative building. In 1925 there was extensive renovation on the building. Back of building faces west. Demolished in 1974. Several people in image. Printed in Germany. On verso: Athletic Club House, Ferry Field

La educación primaria en los campos de la provincia de Buenos Aires (1943-1955)

El artículo se ocupa de las políticas educativas dirigidas al ámbito rural. El objetivo es caracterizar las escuelas primarias en la campaña bonaerense y examinar las demandas, la legislación y los proyectos que tuvieron lugar en relación con dichas escuelas durante el primer Peronismo. Se utiliza una metodología cualitativa que toma como fuentes de información normativas, discursos, estadísticas y proyectos de reformas. Se concluye que, si bien las demandas materiales dieron lugar a planes que en la mayor parte de los casos se concretaron, las peticiones para atender a la especificidad de la escuela rural fueron más difíciles de efectivizar

Dominant wave energy and sediment movement on intertidal beaches in Freshwater Bay, Washington, U.S.A.

Freshwater Bay (FWB), Washington did not undergo significant erosion of its shoreline after the construction of the Elwha and Glines Canyon Dams, unlike the shoreline east of Angeles Point (the Elwha River’s lobate delta). In this paper I compare the wave energy density in the western and eastern ends of the Strait of Juan de Fuca with the wave energy density at the Elwha River delta. This indicates seasonal high- and low-energy regimes in the energy density data. I group multi-year surveys of four cross-shore transects in FWB along this seasonal divide and search for seasonal trends in profile on the foreshore. After documenting changes in elevation at specific datums on the foreshore, I compare digital images of one datum to determine the particle sizes that are transported during deposition and scour events on this section of the FWB foreshore. Repeat surveys of four cross-shore transects over a five-year period indicate a highly mobile slope break between the upper foreshore and the low-tide delta. Post-2011, profiles in eastern FWB record deposition in the landward portion of the low-tide terrace and also in the upper intertidal. Western FWB experiences transient deposition on the low-tide terrace and high intra-annual variability in beach profile. Profile elevation at the slope break in western FWB can vary 0.5 m in the course of weeks. Changes in surface sediment that range from sand to cobble are co-incident with these changes in elevation. High sediment mobility and profile variation are inconsistent with shoreline stability and decreased sediment from the presumed source on the Elwha River delta.

Geology and landslide geomorphology of the Burpee Hills, Skagit County, Washington, USA

Landforms within the Skagit Valley record a complex history of land evolution from Late Pleistocene to the present. Late Pleistocene glacial deposits and subsequent incision by the Skagit River formed the Burpee Hills terrace. The Burpee Hills comprises an approximately 205-m-thick sequence of sediments, including glacio-lacustrine silts and clays, overlain by sandy advance outwash and capped by coarse till, creating a sediment-mantled landscape where mass wasting occurs in the form of debris flows and deep-seated landslides (Heller, 1980; Skagit County, 2014). Landslide probability and location are necessary metrics for informing citizens and policy makers of the frequency of natural hazards. Remote geomorphometric analysis of the site area using airborne LiDAR combined with field investigation provide the information to determine relative ages of landslide deposits, to classify geologic units involved, and to interpret the recent hillslope evolution. Thirty-two percent of the 28-km2 Burpee Hills landform has been mapped as landslide deposits. Eighty-five percent of the south-facing slope is mapped as landslide deposits. The mapped landslides occur predominantly within the advance outwash deposits (Qgav), this glacial unit has a slope angle ranging from 27 to 36 degrees. Quantifying surface roughness as a function of standard deviation of slope provides a relative age of landslide deposits, laying the groundwork for frequency analysis of landslides on the slopes of the Burpee Hills. The south-facing slopes are predominately affected by deep-seated landslides as a result of Skagit River erosion patterns within the floodplain. The slopes eroded at the toe by the Skagit River have the highest roughness coefficients, suggesting that areas with more frequent disturbance at the toe are more prone to sliding or remobilization. Future work including radiocarbon dating and hydrologic-cycle investigations will provide a more accurate timeline of the Burpee Hills hillslope evolution, and better information for emergency management and planners in the future.