Permafrost (Other Keyword)

1-4 (4 Records)

Frozen Ground (2015)
DOCUMENT Citation Only Ian Buvit.

Remnants of perennially frozen ground can serve as indicators of past climate changes. Evidence of ground ice like pseudomorphs, or solifluction lobes, for example, has helped us identify cooling events such as the last glacial maximum or the Younger Dryas. Cryogenic activity can also have wide ranging affects on the behavioral context of archaeological sites displacing material from its original location a few millimeters to many meters. Here I illustrate some common types of cryogenic features...


Joint Base Elmendorf-Richardson Resources
PROJECT Uploaded by: Rachel Fernandez

Project metadata for resources within the Joint Base Elmendorf-Richardson cultural heritage resources collection. This project is used to fill metadata for all resources part of the Joint Base Elmendorf-Richardson collection.


Report To BLM of the Archaeological Survey of Operational Material Site Oms 133-2a and Oms 122-3a (1985)
DOCUMENT Citation Only Jean S. Aigner. Dominique Desson. Ralph Lively.

This resource is a citation record only, the Center for Digital Antiquity does not have a copy of this document. The information in this record has been migrated into tDAR from the National Archaeological Database Reports Module (NADB-R) and updated. Most NADB-R records consist of a document citation and other metadata but do not have the documents themselves uploaded. If you have a digital copy of the document and would like to have it curated in tDAR, please contact us at comments@tdar.org.


Summary of Quaternary Geology of the Municipality of Anchorage, Alaska (1999)
DOCUMENT Full-Text Randall G. Updike. Henry R. Schmoll. Lynn A. Yehle.

This report discusses the quaternary geology of the Upper Cook Inlet region which is dominated by deposits of glacier retreats that followed repeated advances from both adjacent and more distant mountains. At several levels high on the mountains, there are remnant glacial deposits and other features of middle or older Pleistocene age.