Historic preservation news and notes

The State Historic Preservation Office at the South Carolina Department of Archives and History publishes a monthly newsletter featuring agency programs and events, and highlights those of state and national preservation groups.

Historic preservation news and notes

The State Historic Preservation Office at the South Carolina Department of Archives and History publishes a monthly newsletter featuring agency programs and events, and highlights those of state and national preservation groups.

Historic preservation news and notes

The State Historic Preservation Office at the South Carolina Department of Archives and History publishes a monthly newsletter featuring agency programs and events, and highlights those of state and national preservation groups.

Historic preservation news and notes

The State Historic Preservation Office at the South Carolina Department of Archives and History publishes a monthly newsletter featuring agency programs and events, and highlights those of state and national preservation groups.

Historic preservation news and notes

The State Historic Preservation Office at the South Carolina Department of Archives and History publishes a monthly newsletter featuring agency programs and events, and highlights those of state and national preservation groups.

Dynamics and variability of the alongshore flows on the northwestern iberian margin

Tese de doutoramento, Ciências Geofísicas e da Geoinformação (Oceanografia), Universidade de Lisboa, Faculdade de Ciências, 2014

The Contemporary Group Program Notes, May 15, 1974

Concert program for The Contemporary Group Program Notes, May 15, 1974

Synthesis of the Piacenzian onshore record between the Aveiro and Setubal parallels (Western portuguese margin)

Onshore, the Piacenzianof the Mondego and Lower Tagus Tertiary basins comprises siliciclastic sediments deposited in shallow marine to continental environments. The outcrops of the deposits are relatively widespread in the Aveiro and Seuibal region. A lithostratigraphic synthesis based on the correlation of geological sections, is presented for the two basins. In general, the Piacenzian sediments display a regressive sucession. The Late Tortonian-Zanclean (?) confined drainage pattern changed at the beginning of Piazencian, to fluvial systems draining to the Atlantic, and capturing the drainage of the inner parts of the Hesperic Meseta. The Piacenzian sedimentary sequence post-dates one of the uprising phases during Neogene compression, recorded by a strong regional unconformity. Some local active faulting - as in Lousa, Rio Maior and Senibal- Pinhal Novo - allowed the local thickening of the sedimentary record. Later compressive tectonism continues to generate reverse faulting and diapiric reactivation, affecting those sediments. Currently, the Piacenzian deposits culminates the marginal piedmonts, widely eroded by the Quaternary fluvial dissection.