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54-741: The Sand Mountain Volcanic Field (also known as the Sand Mountain Field ) is a volcanic field in the upper McKenzie River watershed , located in the United States in Oregon . Part of the Cascade Volcanic Arc , it lies southwest of Mount Jefferson and northwest of Belknap Crater and Mount Washington . Its highest elevation is 5,463 feet (1,665 m). Active during the Holocene epoch,

108-1040: A riffle and pool structure and cooler water temperatures. Rivers with a course that drops in elevation very slowly will have slower water flow and lower force. This in turn produces the other characteristics of a lowland river—a meandering course lacking rapids , a river bed dominated by fine sediments and higher water temperatures. Lowland rivers tend to carry more suspended sediment and organic matter as well, but some lowland rivers have periods of high water clarity in seasonal low-flow periods. The generally clear, cool, fast-flowing waters and bedrock and coarse sediment beds of upland rivers encourage fish species with limited temperature tolerances, high oxygen needs, strong swimming ability and specialised reproductive strategies to prevent eggs or larvae being swept away. These characteristics also encourage invertebrate species with limited temperature tolerances, high oxygen needs and ecologies revolving around coarse sediments and interstices or "gaps" between those coarse sediments. The term "upland"

162-751: A "field" is not well-defined. Volcanic fields usually consist of clusters of up to 100 volcanoes such as cinder cones . Lava flows may also occur. They may occur as a monogenetic volcanic field or a polygenetic volcanic field . Alexander von Humboldt observed in 1823 that geologically young volcanoes are not distributed uniformly across the Earth's surface, but tend to be clustered into specific regions. Young volcanoes are rarely found within cratons , but are characteristic of subduction zones, rift zones , or in ocean basins. Intraplate volcanoes are clustered along hotspot traces. Within regions of volcanic activity, volcanic fields are clusters of volcanoes that share

216-452: A DRE volume of 0.072 cubic miles (0.3 km), and Nash group a DRE volume of 0.053 cubic miles (0.22 km). Past radiometric dating gave Sand Mountain Volcanic Field's age within a 1,000 year range. More precise paleomagnetic dating suggested that the field includes at least 13 distinct eruptive units, which were generated over a short period of time (likely just a few decades) about 2,950 years ago. The Jack Pine vent, which resides at

270-674: A clockwise fashion above the subduction zone , volcanism has moved east in the central Oregon Cascades and moved west in the northern Cascades. The graben of the High Cascades is bounded to the east by the Green Ridge fault zone and to the west by the Horse Creek fault zone. It has a width of 19 miles (30 km) and a depth of 1.2 to 1.9 miles (2 to 3 km). Predominantly, it has generated mafic (rich in magnesium and iron ) lava, producing about 14 cubic miles (60 km) of magma within

324-689: A common magma source. Unlike a large volcano with satellite or subsidiary vents, a volcanic field's vents have their own source of magma, possibly of different compositions (such as basalt and rhyolite ), and these vents may span an area of thousands of square miles. Scoria cones are particularly prone to cluster into volcanic fields, which are typically 30–80 kilometers (19–50 miles) in diameter and consist of several tens to several hundred individual cones. The unusually large Trans-Mexican Volcanic Belt has nearly 1000 cones covering an area of 60,000 square kilometers (23,000 sq mi). Upland and lowland#Lowland Upland and lowland are portions of

378-622: A depth of about 13 feet (4.0 m). Radiocarbon dating analysis suggested that the samples were dated to 3,200 ± 220 and 2,705 ± 200 years Before Present, respectively; radiocarbon dating performed by Licciardi et al. (1999) found a similar result of 2750 ± 45 years Before Present. Later radiocarbon dating of a conifer branch and charcoal on a lateral moraine near Nash Crater in 2004 had respective estimates of 3,440 ± 250 and 2,590 ± 150 years Before Present. Red and oxidized scoria has been quarried from Little Nash Crater for highway supplies near Santiam Pass. The Carmen Smith Hydroelectric Power Scheme

432-682: A fissure that trended from north to south near the northern end of the volcanic field. These eruptions blocked the Lost Creek tributary, forming Lost Lake. The Sand Mountain Field is located 62 miles (100 km) from a population of roughly 500,000 people. It is close to a major transportation corridor from central Oregon to the Willamette Valley as well as a popular ski area, and future eruptions could have "substantial societal consequences" according to Deligne et al. (2016). Lava flows from an eruption in

486-609: A larger volcanic field of Quaternary volcanism in the region, which they refer to as the Central Oregon volcanic field. During the Holocene epoch, volcanic activity has been particularly concentrated between the North Sister volcano and Three Fingered Jack , with at least 125 distinct eruptive centers active since the retreat of Pleistocene glaciers. Eruptive activity in the upper McKenzie River catchment has been taking place since after

540-473: A long period of time, likely partly attributable to interaction with water. Walsh (2012) classifies the eruptions as sub-Plinian . The Nash Crater cinder cone erupted lava flows about 3,850 years ago, which coursed west and blocked a stream to create Fish Lake and Lava Lake. The lava flows were unvegetated and blocky. According to Sherrod et al. (2004), these flows, also known as the Fish Lake lava flow, represent

594-665: A maximum elevation of 5,463 feet (1,665 m). Located within the Willamette National Forest in the McKenzie Ranger District near Santiam Pass , the Sand Mountain Volcanic Field is southwest of Mount Jefferson and northwest of Belknap Crater and Mount Washington . The field borders Clear Lake , the source for the McKenzie River, and lava flows from the field formed a dam that created

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648-555: A plain that are conditionally categorized by their elevation above the sea level . Lowlands are usually no higher than 200 m (660 ft), while uplands are somewhere around 200 m (660 ft) to 500 m (1,600 ft). On unusual occasions, certain lowlands such as the Caspian Depression lie below sea level. Uplands areas tend to spike into valleys and mountains , forming mountain ranges while lowland areas tend to be uniformly flat, although both can vary such as

702-467: A small chamber near its base, which slopes down for another 10 feet (3.0 m). Century Pit lies 150 feet (46 m) to the east of Moss Pit, with an entrance 3 feet (0.91 m) in diameter. Surrounded by a wall of spatter material ranging from 1 to 2 feet (0.30 to 0.61 m) in height, it has a vertical drop of 94 feet (29 m), its lower half widening to a chamber with dimensions of 10 by 25 feet (3.0 by 7.6 m) at its base. The western margin of

756-573: A unique ratio of iron(II) oxide to magnesium oxide, and the Lost Lake Group is distinguished by its lower iron(II) oxide to magnesium oxide ratio and high magnesium oxide content. According to Wood and Kienle (1993), the field has a lava composition of subalkaline basalt and basaltic andesite. Deligne et al (2016) argue that the field also has calc-alkaline basalt. Morphologically, Sand Mountain Field lavas have blocky appearances, reaching thicknesses up to 49 feet (15 m) though certain parts of

810-560: A volume of 0.094 cubic miles (0.39 km). This tephra field is notable because it has a much greater volume and extent than tephra produced by other mafic volcanoes in the central Oregon Cascades. Additionally, the tephra exhibits uniformity with a fine mode grain size of 0.0049 inches (125 μm) to 0.020 inches (0.5 mm) and a lack of lapilli . These tephra deposits vary in age from 3,440 ± 250 to 1,600 years BP, according to radiocarbon dating . They reach thicknesses of greater than 6.6 feet (2 m) as far as 5.6 miles (9 km) from

864-461: Is a lava tube called Lucy's Cavern that funneled the Sand Mountain Volcanic Field flows. It has a length of at least 490 feet (150 m) and reaches depths of 26 to 33 feet (8 to 10 m). Its roof has a vaulted appearance with drip-like features. There are also two circular "vertical pits" that reach depths of 62 feet (19 m) and 98 feet (30 m), respectively. These open vertical conduit lava caves , known as Century and Moss Pits, lie to

918-727: Is also used in wetland ecology , where "upland" plants indicate an area that is not a wetland. The generally more turbid , warm, slow-flowing waters and fine sediment beds of lowland rivers encourage fish species with broad temperature tolerances and greater tolerances to low oxygen levels, and life history and breeding strategies adapted to these and other traits of lowland rivers. These characteristics also encourage invertebrate species with broad temperature tolerances and greater tolerances to low oxygen levels and ecologies revolving around fine sediments or alternative habitats such as submerged woody debris ("snags") or submergent macrophytes ("water weed"). Lowland alluvial plains form when there

972-506: Is fed by the upper McKenzie River and generates about 115 horsepower (86 kW) of electricity. The upper McKenzie River catchment area includes Clear Lake and Tamolitch Pool , which represent popular tourist locations. At Clear Lake, popular activities include canoeing , fishing, and non-motorized boating, with 34 campsites available at the Cold Water Cove Campground and a grocery store, tackle shop, and restaurant located at

1026-413: Is generally considered to be land that is at a higher elevation than the alluvial plain or stream terrace , which are considered to be "lowlands". The term "bottomland" refers to low-lying alluvial land near a river. Much freshwater fish and invertebrate communities around the world show a pattern of specialization into upland or lowland river habitats. Classifying rivers and streams as upland or lowland

1080-404: Is important in freshwater ecology , as the two types of river habitat are very different, and usually support very different populations of fish and invertebrate species. In freshwater ecology, upland rivers and streams are the fast-flowing rivers and streams that drain elevated or mountainous country, often onto broad alluvial plains (where they become lowland rivers). However, elevation is not

1134-653: Is possible, but according to the Volcano Hazards Program of the United States Geological Survey , the threat from the field itself is low. The field lies within the Willamette National Forest near Santiam Pass . It supports some forested areas, which grow well on lava flows with tephra that serves as suitable soil for stands of Douglas fir and western hemlock and less commonly western red cedar . The surroundings represent an area of geological interest, and scoria has been quarried from one of

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1188-461: The Mongolian Plateau . Upland habitats are cold, clear and rocky whose rivers are fast-flowing in mountainous areas; lowland habitats are warm with slow-flowing rivers found in relatively flat lowland areas, with water that is frequently colored by sediment and organic matter. These classifications overlap with the geological definitions of "upland" and "lowland". In geology an "upland"

1242-534: The United States Geological Survey , the threat potential from the field is "Low/Very Low." Eruptive activity within the nearby Cascades Range is likely to resume. Deformation near the Three Sisters complex volcano suggests the presence of intrusive magma in the region, which could eventually lead to eruptions, though the intrusion appears to be currently stalled. Further magma intrusions could lead to eruptions that would create new cinder cones similar to those in

1296-665: The Earth's mantle. The basaltic andesite at Little Nash Crater includes many small plagioclase phenocrysts with less abundant olivine phenocrysts, with silica levels of about 56.8 percent. These flows are younger than 2,590 ± 150 years by radiocarbon dating. Basaltic lava from the Lost Lake cone group contained 2–3 percent olivine phenocrysts, which are slightly porphyritic ; these deposits have been radiocarbon dated to 1,950 ± 150 years BP. At Nash Crater, there are basaltic andesite lava flows with sparse olivine phenocrysts and silica levels of about 53.5 percent. The lava from

1350-496: The Global Volcanism Program, a confirmed eruption dated to 950 BCE ± 200 years had a Volcanic Explosivity Index of 4, while another confirmed eruption at Jack Mountain dated to 5050 BCE had a Volcanic Explosivity Index of 2. While geological evidence suggests that eruptions at Sand Mountain Field were explosive, they differed from violent, Strombolian eruptions because their very explosive eruptions were sustained over

1404-664: The High Cascades graben. Beginning as dikes, these bodies of magma moved through conduits to separate volcanic vents at the surface. The initial magma was basaltic , though this was replaced several hundred years later by more evolved , basaltic andesite magma. Eruptions at Sand Mountain Field were fed by two or three magma chambers , including a number of mafic magma sources over a brief span of distance and time. The Sand Mountain Volcanic Field includes 23 basalt and basaltic andesite cinder cones and associated lava flows , which were produced by two roughly north–south trending alignments of 42 volcanic vents. The two groups cross near

1458-457: The Lost Lake cinder cone group, which lies at the northern–northeastern end of the field. Before that, about 3,000 to 4,000 years ago, lava flows erupted from vents along the chain. They moved west and blocked drainage to create small lakes. Past lava flows from Sand Mountain and the nearby Belknap Crater historically disrupted the McKenzie River, producing highly fractured lava deposits across canyons, lakes, streams, and springs. They also produced

1512-637: The Lost Lake group have a ropy, pāhoehoe surface. The Jack Pine cone in the Sand Mountain Field is composed of absarokites, which are unique within the Cascade Range. Its geochemical signature suggests that it was fed by a distinct magma chamber. Absarokites occur within the forearc of the Cascades and the Central Cascades, so this unique magma may be the result of old, metasomatized material from

1566-677: The Nash and Lost Lake group both consist of four units. The Jack Pine cone has no associated lava deposits, and the SnoPark lava unit has no associated volcanic vent. These two deposits exhibit unique compositions; SnoPark lava has relatively higher levels of barium and potassium oxide than the rest of the field, with the exception of the Jack Pine lava, which has even higher concentrations of barium (and also very high levels of strontium ), at 1081 ppm and 1343 ppm, respectively. Single lava units at

1620-524: The Sahalie Falls and the Koosah Falls, as well as the 1.5-mile (2.4 km) long Clear Lake, which still contains branches and bark from tree debris after the eruption. The overall dense-rock equivalent (DRE) volume for the volcanic field lavas and volcanic cones is estimated to be 0.22 to 0.29 cubic miles (0.9 to 1.2 km). The Sand group has a DRE volume of 0.15 cubic miles (0.64 km), Lost Lake

1674-425: The Sand Mountain Field began erupting about 4,000 years ago. The field includes 23 basaltic and basaltic andesitic cinder cones and lava flows , for a total of 42 volcanic vents within two roughly north–south trending alignments. Its total dense-rock equivalent eruptive output is 0.22 to 0.29 cubic miles (0.92 to 1.21 km), with subfeatures including a tephra field and a lava tube system. Future activity

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1728-475: The Sand Mountain Field. Moreover, hazardous volcanic gases could accumulate after an eruption, such as sulfur dioxide , hydrogen chloride , and hydrogen fluoride . The upper McKenzie River catchment is an area of interest for geological research. The first research there took place in 1929, headed by H. T. Stearns. In 1957, H. Williams produced a reconnaissance geological map, which was followed by further mapping by E. M. Taylor in 1965. Taylor's work determined

1782-464: The Sand Mountain cinder cone and greater than 3.3 feet (1 m) up to 7.5 miles (12 km) from the cinder cone. Microfractures within Sand Mountain clastic rock along with the blocky, equant shapes and density of sideromelane and tachylite clastic rock in the field suggest that Sand Mountain Field lava interacted with water. According to McKay (2012), this likely came from groundwater. There

1836-687: The Sand Mountain cinder cone; their alignments imply the existence of complex volcanic dikes under the field. Sand Mountain marks the largest cinder cone in the field, at a height of 820 feet (250 m). According to the Global Volcanism Program , the field includes six major clusters of volcanic vents, all pyroclastic cones. These are the Central Group, Little Nash Crater, Lost Lake Group, Nash Crater, Sand Mountain Cones, and South Group. Slight variations in vent alignment within groups likely reflect

1890-513: The Sand Mountain volcanic field have fewer western red cedar trees than is common among other forests in the Pacific Northwest region. Fen wetlands surround Lost Lake, which is about 3.1 miles (5 km) north–northeast of the field. Within Clear Lake is a submerged forest of Douglas fir trees. Well-preserved under 120 feet (37 m) of water, they can be seen standing on the bottom of

1944-461: The adjacent Clear Lake Resort. Volcanic formations including lava flows within McKenzie Pass have historically attracted the attention of passing motorists. There is also a ski resort at Santiam Pass. Volcanic field A volcanic field or crater row is an area of Earth 's crust that is prone to localized volcanic activity. The type and number of volcanoes required to be called

1998-408: The base has an opening about 6 feet (1.8 m) deep, and at that depth it is blocked by debris. The lower chambers for both pits may be influenced by a fissure or may form part of an open fissure vent . Deligne et al. (2016) argue that "it is inarguably inappropriate" to consider Sand Mountain a volcanic field despite its official name. They assert that Sand Mountain is a short-lived subfeature of

2052-454: The eruption of Mount Mazama about 7,700 years ago. Thus, it represents one of the youngest volcanic regions in the Cascade Arc. This activity is concentrated in the central Oregon Cascades, at the northwestern margin of the High Cascades graben near the boundary of the High Cascades and Western Cascades. The last eruption in the Sand Mountain Volcanic Field took place about 2,000 years ago at

2106-500: The field have uniform compositions, which is distinct from other young lava deposits within the surrounding region; major distinguishing elements include silicon dioxide (silica), titanium dioxide , magnesium oxide , and calcium oxide . The Sand group has high compositional variation, ranging from basalt to basaltic andesite, while the Lost Lake group is mostly basalt, and the Nash group is completely composed of basaltic andesite. The Nash group shows distinctively high silica content and

2160-503: The field supports mature forests, but other zones with younger lava deposits are barren. Mature forests correspond to lava flow areas with tephra; areas that do not have tephra cover lack soil and support only limited vegetation. Below elevations of 4,300 feet (1,300 m), these forests are typical of the lowland temperate climate of the Pacific Northwest , with Douglas fir and western hemlock predominating. Notably, forests in

2214-488: The field's volcanic cones for highway supplies. Nearby tourist destinations include a ski resort , Tamolitch Falls , and Clear Lake . The Sand Mountain Field is part of the Cascade volcanic arc and is located at the western edge of the High Cascades segment of the central Oregon Cascades, near the upper McKenzie River watershed in Oregon , in the United States . It encompasses an area of 29 square miles (76 km) and has

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2268-507: The lake. Clear Lake encompasses 148 acres (0.60 km) near Oregon Route 126 , with a shallow northern region and a deeper southern zone, which reaches a maximum depth of 175 feet (53 m). Other nearby lakes include Lost Lake, Lava Lake, and Fish Lake. Fish Lake is an ephemeral lake that dries up during the summer season, formed by the damming of local water drainages by a lava flow from Sand Mountain Volcanic Field about 3,850 years ago. Local topography has influenced eruptive activity in

2322-504: The lake. The cold water prevents most life from growing, giving the lake its name, Analysis of samples from the underwater trees in 1965 suggested that the trees were "drowned" about 3,000 years ago, when a lava flow from Sand Mountain created Clear Lake. The eruption altered the ecosystem and created new habitats in the lake, on its shores, and on the new lava flow deposits. Today, life in the lake includes naturally reproducing fish species in Clear Lake such as brook and cutthroat trout , and

2376-474: The main Sand Mountain chain varies from 51.6–53.2 percent silica, thus ranging from basalt to basaltic andesite in composition. Basalt lava at Sand Mountain contains sparse plagioclase and olivine phenocrysts, while basaltic andesite lava only exhibits olivine phenocrysts. These flows vary in age from are 3,850 ± 215 years BP to 2,750 years BP. The field also includes an extensive tephra deposit, which encompasses an area of 59 square miles (154 km) and has

2430-440: The northern edge of the field, has a distinct composition from the field's other landforms; it likely erupted about 4,000 years prior to the rest of the field. Deligne et al. (2016) agree with this age estimate, arguing that tephrochronology evidence and lava composition analysis suggest that Jack Pine erupted about 7,000 years ago, while the main Sand Mountain Volcanic Field eruptions took place circa 3,000 years ago. According to

2484-468: The oldest lava flows near the Santiam and McKenzie Passes after the cataclysmic eruption of Mount Mazama. Radiocarbon dating of a charred conifer branch found in Sand Mountain volcanic ash yielded an age of 3,440 ± 250 years Before Present (BP). Radiocarbon dating of charcoal on a lateral moraine near Nash Crater gave an age of 2,590 ± 150 BP. The Lost Lake cinder cones erupted about 1,950 years ago, along

2538-500: The past 15,000 years. Moreover, many of the identified eruptive vents from the Quaternary include scoria cones or other mafic vents. The High Cascades graben displays a unique geochemical signature with low- K tholeiite magma and a relatively enriched mantle source, produced by extension and heat flux . The Sand Mountain Volcanic Field was formed after magma entered rock that was fractured by faulting related to subsidence of

2592-529: The past, directing lava flows downhill to the west and, with wind, directing tephra to the northeast. Annual precipitation in the Oregon Cascades averages 79 to 150 inches (2,000 to 3,800 mm), with about 80 percent falling in the winter season. In the High Cascades, discharge is steady throughout the year, and precipitation falls mostly as snow, which then melts, seeps into the ground, and reaches springs several years later. The southern part of

2646-586: The presence of 9 lava units at Sand Mountain Volcanic Field and another lava unit from Belknap Crater. A map published by Sherrod et al. (2004) built upon Taylor's studies. In November 1963, the United States Forest Service sent divers from the Whitewater Diver group from Eugene to obtain tree samples from Clear Lake using Aqua-Lung technology. Two samples were acquired from one tree section, both about 1 foot (0.30 m) in diameter, at

2700-715: The small differences in local tectonic stress fields. There is also evidence of vent reoccupation, suggested by lava deposits in close proximity at the Old Wagon Road vent and Great Spring vent eruptive units; one of the Great Spring cones buries part of an Old Wagon Road vent. There are three major geochemical groups in the field: Sand, Lost Lake, and Nash. Together they amount to 13 eruptive units , three of which have not been associated with exposed volcanic vents and one cluster of volcanic cones that do not have associated lava flows. The Sand group includes five eruptive units , while

2754-426: The sole determinant of whether a river is upland or lowland. Arguably the most important determinants are those of stream power and stream gradient . Rivers with a course that drops rapidly in elevation will have faster water flow and higher stream power or "force of water". This in turn produces the other characteristics of an upland river—an incised course , a river bed dominated by bedrock and coarse sediments,

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2808-424: The southwest of Sand Mountain on a ridge of spatter material that trends to the east. There are also remnants of a third open conduit in a former vent, which left a crater about 30 feet (9.1 m) in diameter. Both Moss Pit and Century Pit have vertical, circular entrances with smooth, remelted lining. Moss Pit has a diameter of 8 feet (2.4 m) at the entrance, with a depth of 63 feet (19 m). It also features

2862-415: The surrounding Central Oregon volcanic field could reach highways, but most mafic volcanism in the region is unlikely to threaten transportation given the small number of local roads. Tephra from eruptions at Sand Mountain could reach more than 6.2 miles (10 km) from the vent, and if lava flows reached forested regions they could initiate forest fires. However, according to the Volcano Hazards Program of

2916-728: The water is restocked annually with rainbow trout . The Cascade Range and Cascade Volcanic Arc result from the subduction of the Juan de Fuca tectonic plate under the North American tectonic plate . In the Central Oregon Cascades, there are two subsegments: the Western Cascades (active from about 35 to 5 million years ago) and the High Cascades (active since 5 million years ago). As the North American Plate has rotated in

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