modoc plateau geology

Geothermal systems with evidence of magmatic heat . Additionally, the Burney Falls area could be affected by regional volcanic events originating within the Mt. The County Environmental Health Department would act as the monitoring body to ensure compliance with the permit. According to available geologic maps from the California Division of Mines and Geology (CDMG), the Modoc Plateau is underlain by Tertiary sediments and recent volcanic rocks that have been block-faulted into north trending ranges, which have resulted in large open valleys. Yields and specific capacities of -wells in the unconfined water body within volcanic rocks and lake deposits range widely . In the Modoc Plateau, Douglas-fir becomes less important, western white pine (Pinus monticola) woodlands dominate many areas, and Jeffrey pine (Pinus jeffreyi) and Washo pine (Pinus washoensis) occur with or replace ponderosa pine. The Modoc Plateau lies in the northeast corner of California as well as parts of Oregon and Nevada. The plateau supports large herds of Mule Deer (Odocoileus hemionus), Rocky Mountain Elk (Cervus canadensis), and Pronghorn (Antilocapra americana). On the McArthur Swamp property, grading activities involved with the construction and development of wetland habitat at the Hollenbeak and Ash fields would have the potential to cause accelerated erosion, unless proper erosion control measures are implemented. 0 Reviews. Water erosion hazard for bare soil is low to moderate, while the wind erosion hazard is low (refer to TableVI-1). The actual distribution of these ten mapping units is complex, and therefore, will be described by bisecting the site into two northern quadrants and a southern half. This mapping unit is typically found at the base of toe slopes where alluvium from basalt has been deposited. It's a Other size geocache, with difficulty of 1.5, terrain of 1.5. . Get this from a library! As shown, may include some rocks older than Oligocene, correlative with upper parts of unit Tea. Reviews aren't verified, but Google checks for and removes fake content when it's identified. Soils located on the Ahjumawi Property consist of the Pastolla muck, 0 to 1 percent slopes, which are similar to those located along the Bowman Ditch, except that it is not artificially drained (NRCS, 2000). Volcanism continued through the Holocene, forming the 300 foot thick basalts of the Cima Volcanic Field or the Barstow-Amboy axis of volcanic craters, which have protected underlying granite from erosion. In places includes interlayers of silicic volcaniclastic rocks and tuffaceous sedimentary rocks. The soils are not considered Prime Farmland and have a Capability Class rating of IV (NRCS, 2000). Better run fast! Elevations vary from 650 to 1300 feet and the bedrock consists of sandstone, siltstone, shale, some limestone and coal. Following the exchange, Burney Falls and Bowman Ditch will be protected from major construction and other soil disturbing activities by the legal restrictions applicable to State parklands. Includes some Mesozoic rocks. Most of the gold deposits date to the Cretaceous and formed in narrow belt around the Melones fault in quartz veins. See Answer. For those that did not, or used other generalized terms for Quaternary rocks, the unit Qal has been used for the general undivided alluvium. Britton Silt Loams, 30 to 50 percent slopes soils are characterized as being relatively shallow (10 to 20inches), and well drained with moderately slow permeability. These soils formed in basins of mixed alluvium and are moderately deep, poorly drained soils with slow permeability and a high shrink-swell potential (see TableVI-1). Dominant land uses are forestry, livestock grazing, recreation and conservation. With the close-proximity of numerous faults, these sites within the Park could potentially be subjected to ground motion from displacement along any of these local and regional faults. The Modoc Plateau is a mile-high expansive prehistoric lava flow, with areas of sparse vegetation, rough broken lava rock, juniper trees, and sagebrush flats in a semi-arid region covering about a half-million acres. These habitats are a critical part of the Pacific flyway, supporting vast numbers of shorebirds and waterfowl, the densest wintering concentration of bald eagles in the world, and many other wildlife species. An exception is the broad Teays Valley which was created by a large, preglacial river. Geology. The Modoc Plateau is located in the northeastern corner of the state, framed by and including the Warner Mountains and Surprise Valley along the Nevada border to the east and west to the edge of the southern Cascades Range. Substantially folding at the edge of the valley creates famous oil producing dome structures like Lost Hills and Kettleman Hills. Much more recent Pliocene terrestrial sedimentary rocks are also common in the northern Peninsular Ranges like the San Timoteo Canyon and Mount Eden conglomerate, sandstone and siltstone which are up to 7000 feet thick. [2] Cities and counties must regulate certain development projects within the zones, which includes withholding permits until geologic investigations demonstrate that development sites are not threatened by future surface displacement (Hart, 1997). Upper Klamath Lake is Oregons largest lake and is the biggest remnant of this wetland system. Includes older alluvium and related deposits of Piper (1942), Willamette Silt (Allison, 1953; Wells and Peck, 1961), alluvial silt, sand, and gravel that form terrace deposits of Wells and others (1983), and Gresham and Estacada Formations of Trimble (1963). The purpose of the Alquist-Priolo Act is to regulate development on or near active fault traces to reduce the hazard of fault rupture and to prohibit the location of most structures for human occupancy across these traces. All Rights Reserved. The latest edition of this popular book explores the state s recent rumblings and tremulous past with the aid of full color illustrations. Includes rhyolite at Owyhee Dam, Jump Creek Rhyolite, and Littlefield Rhyolite, all of Kittleman and others (1965); Dooley Rhyolite Breccia of Gilluly (1937), radiometrically dated at 14.7 0.4 Ma by potassium-argon methods (Fiebelkorn and others, 1983); resurgent domal masses in McDermitt caldera area; and extensive unnamed flows and ash-flow tuffs in the central and southern part of the Owyhee Upland. Many of the ash--flow tuffs exhibit flow features and only obscure vitro-clastic textures. The rocks of eastern California formed a shallow continental shelf, with massive deposition of limestone during the Paleozoic, and sediments from this time are common in the Sierra Nevada, Klamath Mountains and eastern Transverse Range. The water erosion hazard on these soils is low, while the wind erosion hazard is moderate, due to the high percentage of silt (refer to TableVI-1). Site is located on private property in Modoc County, California, approximately 10 kilometers from the Oregon border and 20 kilometers from the Nevada border. What is this giant ro. Major geologic changes began in the Cenozoic with continued continental shelf deposition of shale, sandstone and clay as well as near-shore tropical coal deposits. Additionally, borate deposited during arid conditions, with mining after 1926. These soils formed on stream terraces from alluvium derived from extrusive igneous rocks. They are associated with the Whipp-Cupvar Complex, slightly saline, 0 to 2percent slopes mapping unit which occupies a flanking position to the south. The area extends north to the Oregon border and south to include the Skedaddle Mountains and the Honey Lake Basin. Thick sequences of marine rocks from the Late Cretaceous through the Paleocene and Eocene are common in the mountains and on San Miguel Island. Ash-flow tuff, lava flows, pumice-lapilli tuff, coarse pumicite, flow breccia, and domal complexes of rhyolitic, rhyodacitic, and dacitic composition; in places includes peralkaline rhyolite and some andesite and andesite breccia. Therefore, the Shasta County Building division would not be required to issue a development permit. Finally, the Modoc Plateau, a volcanic table ranging from 4,000 to 6,000 feet (1,200 to 1,800 m) in elevation, separates the Medicine Lake Highlands in the west from the Warner Mountains in the east, covering roughly 1,000,000 acres (400,000 ha) of the forest. Volcanic rocks erupted around Barstow in the Triassic. As with the Bowman Ditch, the Ahjumawi Property is located in a seismically active region with numerous, previously referenced faults and volcanoes situated in the immediate vicinity. These deposited as part of a series of small island arcs, "rafted" against the coast of the proto-North American continent Laurentia. Geothermal systems with evidence of magmatic heat, associated wi Is usually overlain by a few feet of reddish Pleistocene gravel and rests on Chico formation. Read more Print length 384 pages [15] They have a Capability Class rating of IV and are considered Prime Farmland if drained and irrigated (NRCS, 2000). Find many great new & used options and get the best deals for Roadside Geology of Northern and Central California (paperback) at the best online prices at eBay! Hill*s work, however, is of little value in understanding the areal . It is drained by the Pit River, which ultimately reaches Shasta Lake and the Sacramento River. California's Geomorphic Regions Modoc Plateau Location: located east of Cascade Range and adjacent to the Basin & Range Region The Modoc Plateau is the California part of the greater Colombian Volcanic Plateau that extends into Oregon, Washington & Canada Mountains California's Geomorphic Regions: Extensive marine and nonmarine sand deposits, generally near the coast or desert playas. [13]. It is the only state with all three types of plate boundaries, an extraordinary history of earthquakes and volcanoes, and it has many rocks and minerals found nowhere else. Shasta, Lassen Peak, or Medicine Lake volcanic centers, all of which have had activity within the last 500years (CDMD, 1994). Thick Miocene sediments formed in narrow seaways from the Pacific. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. Basalt is aphyric to moderately porphyritic with phenocrysts of plagioclase and olivine and exhibits both subophitic and diktytaxitic textures. Modoc Plateau, and West Cascades Ecoregional Assessments. These soils are moderately deep, moderately well drained and have slow permeability. The monument, established in 1925, includes the sites of many important battles of the Modoc Indian War of 1872-73. [11]. Broad valleys occupy the lowlands between the mountain ridges. Eruptions relatively quiet, but spectacular. Non-seismic hazards addressed in the document include volcanoes, erosion, and expansive soils. The soils are moderately to strongly alkaline. California s geology makes headlines when faults shift, volcanoes puff steam, and coastal bluffs fall into the sea. These are Jurassic and Cretaceous age greywacke, chert, basalt, ultrabasic rocks and serpentinite from modified oceanic crust. The Golden State includes both the highest and lowest point in the continental US and practically every conceivable geological feature known. In places includes flows of platy olivine andesite or basaltic andesite. Basalt flows, flow breccia, and basaltic peperite; minor andesite flows; some interbeds of tuff and tuffaceous sedimentary rocks. Project work may include post fire recovery efforts. During the Miocene, the Coast Ranges were flooded again, with underwater volcanic eruptions in the southern part of the range and deposition of fossil-rich shales like the Monterey formation. Unit is present in all counties. The ecoregion includes a large pumice zone in central Oregon, dominated by lodgepole pine (Pinus contorta), one of the very few places where the species is the climax tree (not replaced by other conifers if fire is suppressed). It is composed of layers of volcanic flows and periodic volcanic uplifts. These mapped faults include the McArthur, Mayfield, Pittville, Hat Creek, and Rocky Ledge faults; whereby the McArthur fault trends northwesterly through the site between Big Lake and Horr Pond (CDMG, 1994). [20] Columbia River / Modoc Plateau basalt. There are no septic tanks or wastewater disposal systems proposed as part of this project, therefore this item is not applicable. Click here to use the California geological interactive map Source: California Geological Survey They are shallow, well drained cobbly loams of moderate permeability and are neutral to mildly acidic. In some areas, decades of fire suppression have resulted in large areas of dense, fire-prone forest. Potassium-argon ages on rocks from unit range from about 36 Ma (Swanson and Robinson, 1968) to about 20 Ma. . Medicine Lake volcano is located at the intersection of major tectonic features including the northwestern extension of the Walker Lane fault zone. A few may date earlier, like the 400 million year old Mule Mountain. in Geology from Syracuse University with a focus on. By contrast, the Trinity ophiolite is found in the east, known for its numerous ultramafic rocks and being one of the most extensive ophiolites in the US. The soils have a Capability Class rating of IV and are not considered Prime Farmland. Furthermore, each of the properties would be subject to regional volcanic events originating from the previously discussed volcanoes. Major Pierson Reading found gold in 1848 in the Trinity River near Douglas City. The Fall River Watershed lies within the volcanic terrain of the Modoc Plateau geomorphic province, and is the largest sub-drainage in the middle reach of the Pit River. This area lies along the northwestern-most flank of the Sierra Nevada Geomorphic Province. In southeast Oregon many domal complexes younger than 11 Ma exhibit a well-defined southeast to northwest age progression (Walker, 1974; MacLeod and others, 1976) from about 11 Ma to less than 1 Ma, Additional scientific data in this geographic area. Soils of the Pittville Sandy Loam, 0 to 5 percent slopes mapping unit occur at the southern fringe of the site. Reference: Chorlton, L.B. Soils comprising the Burney-Arkright Complex, two to nine percent slopes mapping unit, occupy smaller areas in the eastern portion of the transfer property and are underlain by basaltic lava flows. On this Wikipedia the language links are at the top of the page across from the article title. These soils have a Capability Class rating of III to IV, due to erosion hazards and are not considered to be Prime Farmland (NRCS, 2000). Location & Geology. Therefore, the transfer would not expose people or structures to potential substantial adverse effects, including the risk of loss, injury, or death. Map unit used in all counties for recent lake beds, playas, and flood plains. Whipp soils account for approximately 60 percent of these map units, while Cupvar soils account for approximately 25 percent. 12201 Sunrise Valley Drive Reston, VA 20192, Region 2: South Atlantic-Gulf (Includes Puerto Rico and the U.S. Virgin Islands), Region 12: Pacific Islands (American Samoa, Hawaii, Guam, Commonwealth of the Northern Mariana Islands). In places contains mollusks or vertebrate fossils indicating Pleistocene age; mostly deposits of late Pleistocene age, but locally includes some deposits of early Holocene age. Pyroclastic Rock. Very large earthquakes that occur closer to the Northern California coast could cause damaging levels of ground shaking here too. The east side of the Warner Mountains in particular has exposed rock in the many canyons, including finds of petrified wood and assorted gemstones. Funding was provided to WDFW through a state wildlife grant from the United The Clear Lake National Wildlife Refuge and Long Bell State Game Refuge are located on the plateau as well. May include some rocks of middle Miocene age in the area west and northwest of Lakeview. North of the San Joaquin River, the mountains have a tilted-block pattern caused the Sierra Nevada fault, which is interpreted as being similar to the more common Basin and Range terrain to the east. In the southern part of the range, between the Nacimiento and San Andreas fault zones, the metamorphic rocks and granite plutons of the Salinian block make up the basement rock. They have a Capability Class rating of II and are considered Prime Farmland when irrigated (NRCS, 2000). "Modoc County has an area of 3823 square miles. The threat of catastrophic wildfire and competition with barred owls (Strix varia) are concerns for the conservation of the spotted owl, a federally listed species that occurs within the ecoregion. The tribes manage tribally-owned lands on reservations and are also involved in monitoring and research activities on ceded lands. ADVERTISEMENT Compared with the Sierra Nevada, rocks from this time period tend be more calcic than silicic. In 1873, 53 Modoc men held off 650 US troops, killing 70 of them in heavy weather in the lava plateau to the south of Tule Lake. Alluvium, lake, playa, and terrace deposits; unconsolidated and semi-consolidated. The low shield shape, central caldera, and dominance ofmaficlavas are similar to Newberry Volcano of central Oregon, also located in anextensionaltectonicenvironment east of the Cascade arc axis. Includes Picture Rock Basalt of Hampton (1964), radiometrically dated by potassium-argon methods as middle(?) A .gov website belongs to an official government organization in the United States. . It formed as a sandspit filled in to the north from sediment deposited by the Tijuana River and sheltered from wind and waves by the Cretaceous uplands of Point Loma. In some places, ophiolite sequences preserve remnant oceanic crust rock on land, while other parts of the range are intruded with ultrabasic igneous rocks that have serpentinized to peridotite. The McArthur Swamp, Bowman Ditch, and the Ahjumawi Property are located within or adjacent to the McArthur Fault-Rupture Zone. It is in northeastern California about 50 km (31 mi) south of Klamath Falls, Oregon. The San Onofre Breccia also formed during this period with distinct glaucophane schist, gabbro, limestone and greenschist. A lock () or https:// means youve safely connected to the .gov website. Geologists have subdivided the four terranes in the mountain range, referring to them as "plates.". Requires ability to work and study under rigorous conditions. Most of the gold historically mined in California originated in the Mother Lode belt, located in the foothills of the western Sierras. Deccan Traps in India. The Modoc Plateau has a diverse geography, with portions draining into closed basins such as Goose Lake and Surprise Valley, and most of the remainder draining into the Pitt River, a tributary of the Sacramento River. Geology - 156 pages. Shasta, Lassen Peak, or Medicine Lake volcanic centers, all of which have experienced activity within the last 500 years (CDMG, 1994). In the northeastern corner of California, lies a massive volcanic plain known as the Modoc Plateau. It is exposed in the Smith River drainage to the north of US Highway 199 in Del Norte County. In Washington and the rapidly developing areas around Bend in Oregon, timber companies have recently begun to sell their lands in the mid-elevation forest and transition zones to developers. Additionally, each of the properties lie within or adjacent to an Alquist-Priolo Fault-Rupture Study Zone. Axelrod (1966) reported a K-Ar age of . Pillow structures from rapid cooling water indicate underwater volcanism that produced basalt, andesite and diabase flows during the Miocene. Agency The Great Basin Institute Location Susanville, CA Job Category Temporary/Seasonal Positions Salary ~ $1,680 Bi weekly Start Date 05/22/2023 Last Date to Apply The rocks likely formed much further away from the Sierras and were relocated by the dramatic movements of faults. The western gray squirrel is at-risk within the ecoregion in Washington as it is restricted to two isolated populations, but populations in Oregon and California are more robust. With much of the bays only 30 feet deep, human activity has accelerated erosion and filling due to historical hydraulic mining and farming. Older alluvium, lake, playa, and terrace deposits. This 6"x9" paperback has 371 pages that are packed with detailed information about California Geology.

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modoc plateau geology