Investigate historical ownership changes and registration details by initiating a reverse Whois lookup for the name Beacon Leaf Real Estate.

Uncover historical ownership history and changes over time by performing a reverse Whois lookup for the company beacon-leaf-real-estate.

This location is part of the Arizona Mineral Industry Location System (AzMILS), an inventory of mineral occurences, prospects and mine locations in Arizona. Cochise675 is located in T16S R19E Sec 16 NE in the Galleta Flat West - 7.5 Min quad. This collection consists of various reports, maps, records and related materials acquired by the Arizona Department of Mines and Mineral Resources regarding mining properties in Arizona. Information was obtained by various means, including the property owners, exploration companies, consultants, verbal interviews, field visits, newspapers and publications. Some sections may be redacted for copyright. Please see the access statement.

Beacon Properties Cc Company Export Import Records. Follow the Eximpedia platform for HS code, importer-exporter records, and customs shipment details.

This location is part of the Arizona Mineral Industry Location System (AzMILS), an inventory of mineral occurences, prospects and mine locations in Arizona. Gila174C is located in T1N R15.5E Sec 15 C in the Globe - 7.5 Min quad. This collection consists of various reports, maps, records and related materials acquired by the Arizona Department of Mines and Mineral Resources regarding mining properties in Arizona. Information was obtained by various means, including the property owners, exploration companies, consultants, verbal interviews, field visits, newspapers and publications. Some sections may be redacted for copyright. Please see the access statement.

36 Outcrop and Glacial erratic samples of Beacon Sandstone were collected from Escalade Peak, Tate Peak, Halfway Nunatak, Neve Nunatak and Clinker Bluff. These samples are accompanied by the geomorphic, petrographic, and structural information, and GPS position and elevation data.

The Beacon Group stratigraphy and paleontology between the Boomerang and Olympus Ranges was investigated in two phases. The first phase involved visits to ranges and nunataks around the Skelton Neve including visits to Boomerang Range, Warren Range, Portal Mountain and Mt Metschel, by toboggan. The second phase was helicopter assisted and visits were made to Table Mountain, Knobhead Mountain, Aztec mountain, Maya Mountain, Kennar Valley, Mt Fleming and the western Asgaard and Olympus Ranges. The aim was to provide a more detailed stratigraphy for the lower Beacon Group sediments (i.e. the Devonian, Carboniferous and Permian) and to improve if at all possible the most promising paleontological collections of fish in the Boomerang Range by increasing the collection size. The general work conducted included examination and preparation of detailed sections (measured with jacob staff) at several sites, a distinct regional unconformity separating the top of the tillite from the overlying Permian coal measure was traced from north to south over approximately 70 miles and special attention was paid to the lithostratigraphy of Devonian sediments including a critical re-examination of the Odin Arkose, Boreas subgreywacke, Beacon Heights Orthoquartzite and Aztec siltstone, the New Mountain Sandstone, the Pyramid Sandstone, the Terra Cotta Windy Gully member and the Altar Mountain Formation to determine a better nomenclature for these rock groups. Collections of Devonian fish fossils including fin spines, plates, skull plates, jaws, teeth, etc., collection of Permian plant fossils and Devonian lycopods were taken back to New Zealand. In addition, a large collection of rock samples were collected for petrographic analysis, including arkoses, orthoquartzites, siltstones and claystones.

A beacon is a prominent, specially constructed object forming a conspicuous mark as a fixed aid to navigation or for use in hydrographic survey. A cardinal beacon is used in conjunction with the compass to indicate where the mariner may find the best navigable water. It is placed in one of the four quadrants (North, East, South and West), bounded by inter-cardinal bearings from the point marked.

S-57 Object Class: Beacon, cardinal

S-57 Acronym: BCNCAR

This data was compiled for the use in the scale range 1:4,000 to 1:22,000.

THIS DATA DOES NOT REPLACE NAUTICAL CHARTS AND MUST NOT BE USED FOR NAVIGATION.

This data is based on the S-57 data format used in Electronic Navigational Charts (ENCs) published and maintained by the New Zealand Hydrographic Authority at Land Information New Zealand (LINZ). Refer to the following link for information about S-57 data: http://www.linz.govt.nz/hydro/regulation/

Samples from pits, surface rocks, stones and from outcrops were collected for examination and analysis to determine the processes which quartz grains from the Beacon sandstone have been through before being deposited in the tills which they were sampled from. The first pit was located on lower level moraine on Aztec Ridge immediately above the western wall of Beacon Valley and excavated to 24 cm. Three sites in New Valley, immediately east of New Mountain, 12-14 km west of Aztec Ridge were sampled with pits excavated 1.7 m, 1.2 m and 0.7 m deep. Surface rocks, stones and samples from outcrops were collected in the near vicinity to the pits.

This dataset provides information about the number of properties, residents, and average property values for Beacon Hill Drive cross streets in West Linn, OR.

Devonian strata from south Victoria Land has been variously interpreted as marine and non-marine due to the presence of trace fossils that have previously been considered to indicate marine environments in sediments which are strongly indicative of alluvial plain deposition. The local and large scale depositional setting of the Beacon in south Victoria Land was examined. Field work was concentrated on solving problems such as paleoenvironment, paleoslope, basin shape and provenence of the sediment, with computer based modelling used to examine the regional tectonic setting. Exposures of Beacon strata in the Darwin Mountains, Cook Mountains and Britannia Range and in the Convoy Range - Allan Hills area were visited. Measurements of stratigraphic sections, paleocurrent directions, facies interpretation and a systematic study of trace fossil distribution was undertaken. A new fossil fish locality was found near the summit peak of Mt Hughes in the Cook Mountains.

A beacon is a prominent specially constructed object forming a conspicuous mark as a fixed aid to navigation or for use in hydrographic survey. A lateral beacon is used to indicate the port or starboard hand side of the route to be followed. They are generally used for well defined channels and are used in conjunction with a conventional direction of buoyage.

S-57 Object Class: Beacon, lateral

S-57 Acronym: BCNLAT

This data was compiled for the use in the scale range 1:22,000 to 1:90,000.

THIS DATA DOES NOT REPLACE NAUTICAL CHARTS AND MUST NOT BE USED FOR NAVIGATION.

This data is based on the S-57 data format used in Electronic Navigational Charts (ENCs) published and maintained by the New Zealand Hydrographic Authority at Land Information New Zealand (LINZ). Refer to the following link for information about S-57 data: http://www.linz.govt.nz/hydro/regulation/

Intellectual Merit: The goal of this project is to address relationships between foreland basins and their tectonic settings by combining detrital zircon isotope characteristics and sedimentological data. To accomplish this goal the PIs will develop a detailed geochronology and analyze Hf- and O-isotopes of detrital zircons in sandstones of the Devonian Taylor Group and the Permian-Triassic Victoria Group. These data will allow them to better determine provenance and basin fill, and to understand the nature of the now ice covered source regions in East and West Antarctica. The PIs will document possible unexposed/unknown crustal terrains in West Antarctica, investigate sub-glacial terrains of East Antarctica that were exposed to erosion during Devonian to Triassic time, and determine the evolving provenance and tectonic history of the Devonian to Triassic Gondwana basins in the central Transantarctic Mountains. Detrital zircon data will be interpreted in the context of fluvial dispersal/drainage patterns, sandstone petrology, and sequence stratigraphy. This interpretation will identify source terrains and evolving sediment provenances. Paleocurrent analysis and sequence stratigraphy will determine the timing and nature of changing tectonic conditions associated with development of the depositional basins and document the tectonic history of the Antarctic sector of Gondwana. Results from this study will answer questions about the Panthalassan margin of Gondwana, the Antarctic craton, and the Beacon depositional basin and their respective roles in global tectonics and the geologic and biotic history of Antarctica. The Beacon basin and adjacent uplands played an important role in the development and demise of Gondwanan glaciation through modification of polar climates, development of peat-forming mires, colonization of the landscape by plants, and were a migration route for Mesozoic vertebrates into Antarctica.

Broader impacts: This proposal includes support for two graduate students who will participate in the fieldwork, and also support for other students to participate in laboratory studies. Results of the research will be incorporated in classroom teaching at the undergraduate and graduate levels and will help train the next generation of field geologists. Interactions with K-12 science classes will be achieved by video/computer conferencing and satellite phone connections from Antarctica. Another outreach effort is the developing cooperation between the Byrd Polar Research Center and the Center of Science and Industry in Columbus.

Beacon and Ferrar rocks were studied just west of the Dry Valleys, between the Skelton Neve and the Mackay Glacier area. Detailed stratigraphic sections were measured with staff and level at Mistake Peak, Shapeless Mountain, Skew Peak, Mount Bastion, Robison Peak, Mount Fleming, Mount Feather, Mount Warren, Escalade Peak, Swartz Nunatak, Mount Kempe and Rotunda. Collections of rock samples were taken for petrographic description and analysis from all sections measured. Fossils of leaves and stems from the Permian and Triassic coal measures were collected. Glossopteris leaves up to 40cm long with veins clearly preserved were found at Mt Fleming and a varied collection of well preserved calamitid stems, ginkow and fern like fronds up to 50cm across were recovered from a locality at Shapeless Mountain. In addition, Glossopteris and Gangamopteris leaves were found in shale that graded down into the uppermost glacial beds 30cm below. Dating of the carbonaceous beds was attempted from samples of fossil pollen and spores. Further geological data was gathered for the compilation of a 1:250,000 map of the Mount Harmsworth 'Quadrangle' and samples were collected from the rhythmically layered Mount Warren intrusion to continue studies on this unusual feature.

It had been previously found that sampled rocks from Beacon sandstones at Mt Bastion, Beacon Heights and Table Mountain were very weakly magnetised and their magnetic direction had been reset at the time of the massive dolerite intrusions during the Jurassic period. The reson for this is not clear and further investigation were conducted. Only the red beds which occur at two periods within the Beacon Supergroup were sampled. The first period is near the base of the section - the Terra Cotta siltstone and probably Lower Devonian in age. The second is in the Upper Devonian, near the boundary with the Permian, called the Aztec siltstone. The Terra Cotta siltstone outcrops at Mt Kempe, Table Mountain and Knobhead were sampled and the Aztec siltstone outcrops at Portal Mountain, Alligator Peak and Mount Crean were sampled. Rock samples were collected using rock coring equipment. In addition, samples of the dykes (of Ordovician age) in the Wright and Miers Valley and the volcanic of Ross Island (strongly magnetised basalt from a series of flows on Observation Hill) were also collected. Palaeomagnetic measurements were made on all samples.

To understand the subsurface properties of polygonal patterned ground (PPG) and to attempt to resolve competing theories of PPG activity, non-invasive, non-destructive geophysical methods were used to obtain three dimensional images of the subsurface beneath PPG at two sites in the Dry Valleys: Victoria Valley and Beacon Valley. In Victoria Valley an initial reconnaissance of the area was completed, two polygon sets and a long transect line was selected for surveys. The first polygon set was surveyed with 3D ground penetrating radar (GPR) and photogrammetry, then with time lapse electrical resistivity tomography (ERT). The second polygon was surveyed with ERT and photogrammetry and then with lapse 3D GPR. Detailed topography was acquired over the second polygon and each polygon set was finally surveyed with horizontal loop electromagnetic system (HLEM) for lateral electrical conductivity variations. The long transect ran from near the top of the ridge to the SW of the upper Victoria Valley to the other side of the narrows in the lower Lake Victoria. The transect was initially profiled using ERT, then a series of contiguous, sometimes overlapping time-domain EM soundings were acquired in the valley along the transect. A deep GPR profile was acquired and a total magnetic field survey line was completed. Finally, the topography of the transect was surveyed. These geophysical images target the deeper bedrock and massive ice targets. In Beacon Valley an initial reconnaissance of the area was completed and two polygons were selected for detailed geophysical imaging and a 1.2km transect running NW-SE across the valley was completed for large-scale deeper structure and stratigraphy. The two polygons were both surveyed using 3D GPR imaging, ERT, HLEM and detailed topography. Deep GPR and ERT profiles, as well as topographic surveys were acquired along the transect.

A beacon is a prominent specially constructed object forming a conspicuous mark as a fixed aid to navigation or for use in hydrographic survey. A special purpose beacon is primarily used to indicate an area or feature, the nature of which is apparent from reference to a chart, Sailing Directions or Notices to Mariners. Beacon in general: A beacon whose appearance or purpose is not adequately known.

S-57 Object Class: Beacon, special purpose/general

S-57 Acronym: BCNSPP

This data was compiled for the use in the scale range 1:1,500,000 and smaller.

THIS DATA DOES NOT REPLACE NAUTICAL CHARTS AND MUST NOT BE USED FOR NAVIGATION.

This data is based on the S-57 data format used in Electronic Navigational Charts (ENCs) published and maintained by the New Zealand Hydrographic Authority at Land Information New Zealand (LINZ). Refer to the following link for information about S-57 data: http://www.linz.govt.nz/hydro/regulation/

A beacon is a prominent specially constructed object forming a conspicuous mark as a fixed aid to navigation or for use in hydrographic survey. A safe water beacon may be used to indicate that there is navigable water around the mark.

S-57 Object Class: Beacon, safe water

S-57 Acronym: BCNSAW

This data was compiled for the use in the scale range 1:4,000 to 1:22,000.

THIS DATA DOES NOT REPLACE NAUTICAL CHARTS AND MUST NOT BE USED FOR NAVIGATION.

This data is based on the S-57 data format used in Electronic Navigational Charts (ENCs) published and maintained by the New Zealand Hydrographic Authority at Land Information New Zealand (LINZ). Refer to the following link for information about S-57 data: http://www.linz.govt.nz/hydro/regulation/

A beacon is a prominent specially constructed object forming a conspicuous mark as a fixed aid to navigation or for use in hydrographic survey. An isolated danger beacon is a beacon erected on an isolated danger of limited extent, which has navigable water all around it.

S-57 Object Class: Beacon, isolated danger

S-57 Acronym: BCNISD

This data was compiled for the use in the scale range 1:22,000 to 1:90,000.

THIS DATA DOES NOT REPLACE NAUTICAL CHARTS AND MUST NOT BE USED FOR NAVIGATION.

This data is based on the S-57 data format used in Electronic Navigational Charts (ENCs) published and maintained by the New Zealand Hydrographic Authority at Land Information New Zealand (LINZ). Refer to the following link for information about S-57 data: http://www.linz.govt.nz/hydro/regulation/