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Description: PLSSSections_GCDB is the second level of a hierarchical break down of the Public Land Survey System Rectangular surveys. This data is Version 2.0 2015 of the Utah GCDB. This data set represents the GIS Version of the Public Land Survey System. Updates are expected annually as horizontal control positions from published sources and global positioning system (GPS) observations are added. The primary source for the data is cadastral survey records housed by the BLM supplemented with local records and geographic control coordinates from states, counties as well as other federal agencies such as the USGS and USFS. This data was orginally published on 5/1/2015.The PLSS First Division is commonly the section. This is the first set of divisions for a PLSS Township, there are 36 Sections to the usual Township, measuring approximently 1 mile square. (640 Acres)
Copyright Text: Utah BLM, Utah Automated Geographic Reference Center (AGRC),Utah Counties, Premier Data Services
Color: [255, 127, 127, 255] Background Color: N/A Outline Color: N/A Vertical Alignment: baseline Horizontal Alignment: left Right to Left: false Angle: 0 XOffset: 0 YOffset: 0 Size: 8 Font Family: Arial Font Style: normal Font Weight: normal Font Decoration: none
Description: PLSSSections_GCDB is the second level of a hierarchical break down of the Public Land Survey System Rectangular surveys. This data is Version 2.0 2015 of the Utah GCDB. This data set represents the GIS Version of the Public Land Survey System. Updates are expected annually as horizontal control positions from published sources and global positioning system (GPS) observations are added. The primary source for the data is cadastral survey records housed by the BLM supplemented with local records and geographic control coordinates from states, counties as well as other federal agencies such as the USGS and USFS. This data was orginally published on 5/1/2015.The PLSS First Division is commonly the section. This is the first set of divisions for a PLSS Township, there are 36 Sections to the usual Township, measuring approximently 1 mile square. (640 Acres)
Copyright Text: Utah BLM, Utah Automated Geographic Reference Center (AGRC),Utah Counties, Premier Data Services
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Value: Fault, normal, intruded by microdiorite dike, approximately located Label: Fault, normal, intruded by microdiorite dike, approximately located Description: Symbol:
Value: Fault, normal, mapped from linear features, approximately located Label: Fault, normal, mapped from linear features, approximately located Description: Symbol:
Value: Fault, unknown, intruded by microdiorite dike, well located Label: Fault, unknown, intruded by microdiorite dike, well located Description: Symbol:
Value: Fault, unknown, mapped from linear features, approximately located Label: Fault, unknown, mapped from linear features, approximately located Description: Symbol:
Description: This dataset represents geologic map features of the central Mineral Mountains. The map is compiled for use at 1:24,000 scale. It depicts geologic formations, faults, geothermal wells, and other information, and is accompanied by explanatory information including map unit descriptions, geologic symbols, and cross sections.The Mineral Mountains are located in Beaver and Millard Counties, southwestern Utah. The range is a horst located in the transition zone between the Basin and Range and Colorado Plateau (Stokes, 1977) geologic provinces. A multiple-phase Tertiary pluton forms most of the range, with Paleozoic rocks exposed on the north and south and Precambrian metamorphic rocks on the west in the Roosevelt Hot Springs KGRA (Known Geothermal Resource Area). Precambrian banded gneiss and Cambrian carbonate rocks have been intruded by foliated granodioritic to monzonitic rocks of uncertain age. The Tertiary pluton consists of six major phases of quartz monzonitic to leucocratic granitic rocks, two diorite stocks, and several more mafic units that form dikes. During uplift of the mountain block, overlying rocks and the upper part of the pluton were partially removed by denudation faulting to the west. The interplay of these low-angle faults and younger northerly trending Basin and Range faults is responsible for the structural control of the Roosevelt Hot Springs geothermal system. The structural complexity of the Roosevelt Hot Springs KGRA is unique within the range, although the same tectonic style continues throughout the range.During the Quaternary, rhyolite volcanism with active in the central part of the range and basaltic volcanism occurred in the northern portion of the map area. The heat source for the geothermal system is probably related to the Quaternary rhyolite volcanic activity. This [1978-1980] study did not document any additional evidence of recent geothermal activity. It has, however, documented several areas of young basaltic volcanism in the northern portion of the Mineral Mountains. In addition, a structural framework has been developed which will be of use to geothermal explorationists working in the area.Geothermal exploration and development are currently [1980] active in the Roosevelt Hot Springs KGRA on the west-central edge of the range. At present [1980], seven producing wells have been completed and a 20 MWe power plant is planned. The water-dominated geothermal reservoir is structurally controlled (Lenzer and others, 1976; Nielson and others, 1978, 1979).The present [1980] study was undertaken as part of the Industry Coupled Case Studies Program of the Department of Energy, Division of Geothermal Energy. The objectives of the study are to: 1) complete a detailed geologic map of the central part of the Mineral Mountains to determine to what extent the lithologies and structure in the KGRA are unique within the range, and 2) develop a more complete understanding of the plutonic phase and structural history of the Mineral Mountains.
Copyright Text: Program Manager: Grant C. Willis (UGS)
Project Manager: Grant C. Willis (UGS)
Geologic Interpretation: Grant C. Willis (UGS)
GIS and Cartography: Kent D. Brown (UGS)
Funding: Utah Geological Survey and U.S. Department of Energy, DOE award number DE-EE0007080.
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Description: This dataset depicts the 1:24,000 scale land ownership status and areas of responsibility for the State of Utah. Revisions are posted weekly on the AGRC SGID.Maintenance of this data layer is performed by a cooperative federal and state effort. The Utah School and Institutional Trust Lands Administration (SITLA) revises this data regularly to reflect changes in State Trust Lands, other State Land and Private Land as needed. The BLM revises this data regularly to reflect changes in Federal Land as needed. Other information is edited and updated as needed but not on a regular schedule.
Copyright Text: Current Project Manager:
The State of Utah School and Institutional Trust Lands
Lina Haggard, GIS Manager
675 E 500 S Suite 500
Salt Lake City, Utah 84102
801-538-5100
and
The Bureau of Land Management
Rhonda Flynn, Realty Specialist
440 West 200 South, Suite 500
Salt Lake City, UT 84145
Original Project Manager 1993: Colin Homer, Remote Sensing and GIS Laboratories,
Dept. of Geography and Earth Sciences, USU
Original Review: GIS/USU, SITLA
STATE_LGD
(
type: esriFieldTypeString, alias: STATE OF UTAH LEGEND, length: 70
, Coded Values:
[Bankhead-Jones Land Use Lands: Bankhead-Jones Land Use Lands]
, [Bureau of Land Management: Bureau of Land Management]
, [Bureau of Reclamation: Bureau of Reclamation]
, ...13 more...
)
UT_LGD
(
type: esriFieldTypeString, alias: UTAH BLM LEGEND, length: 70
, Coded Values:
[Bankhead-Jones Land Use Lands: Bankhead-Jones Land Use Lands]
, [Bureau of Land Management (BLM): Bureau of Land Management (BLM)]
, [BLM Wilderness Area: BLM Wilderness Area]
, ...15 more...
)
NATL_LGD
(
type: esriFieldTypeString, alias: NATIONAL LEGEND, length: 70
, Coded Values:
[Bankhead-Jones Land Use Lands: Bankhead-Jones Land Use Lands]
, [Bureau of Land Management (BLM): Bureau of Land Management (BLM)]
, [BLM Wilderness Area: BLM Wilderness Area]
, ...14 more...
)