Wind-blown glacial deposits are called

Deposits of windblown silt are called. 2009 Pearson Education, Inc., Upper ... Materials deposited directly by glacial ice are known as. 18. A broad ramplike ...

The loess forms an almost continuous deposit on the land, ranging from about 165 to 260 feet (50 to 80 meters) in depth in most places. In some parts of the plateau, however, the loess deposits are as much as 1,000 feet (300 meters) thick. Because of its unconsolidated nature, when bare loess is soaked with water, significant erosion can occur.Aeolian Deposits Aeolian deposits include sand seas and dune fields, deposits of silt (loess), and fine-grained material that forms a significant component of desert margin and other soils. Aeolian deposits—silt and clay size. Deposits of wind-transported, silt-sized quartz particles, termed loess, cover as much as 10% of Earth’s land surface. Nov 4, 2017 · a'a—a lava rock with a ropey, frothy surface texture formed as a cooling crust on a fluid lava flow.ablation—the removal of snow and ice by melting or evaporation, typically from a glacier or ice field.abrasion—the process of wearing down or rubbing away by means of friction, typically by wind-blown dust or sand.absolute dating—general term applied to a range of techniques that provide ... Compacted layers of wind-blown sediment are known as loess. Loess commonly starts as finely ground-up rock flour created by glaciers. Such deposits cover thousands of square miles in the Midwestern United States. Loess may also form in desert regions (see Chapter 13). Silt for the Loess Plateau in China came from the Gobi Desert in China and ... Transportation by wind sorts material by size. The smallest grains (clay) may be blown far away and spread over a large area, as noted above in the case of Asian dust in Hawai'i. Somewhat larger sizes (silt) may form deposits on the edge of deserts called loess. The enormous loess deposits on the edge of China's Gobi desert provide the Huang He ... Loess - wind-blown silt deposits common along the Mississippi River Valley; Erosional Features. Ventifacts are geomorphic features made of rocks that are abraded, pitted, etched, grooved, or polished by wind-driven sand or ice crystals. They are most typically found in arid environments with little vegetation to interfere with these erosive ...Deposits of windblown dust are called loess . Loess deposits cover wide areas ... Wind-blown silt, mainly formed from glacial processes. Thick glaciers that ...Study with Quizlet and memorize flashcards containing terms like 01) Sediment that begins as rocks on continents or islands is called ________. A) biogenous sediment B) hydrogenous sediment C) cosmogenous sediment D) lithogenous (terrigenous) sediment, 02) High-energy environments are most likely to deposit which one of the following? A) Cosmogenous sediments B) Silt-sized particles C ...

wind commonly deposit sand in mounds or ridges called_____. ice sheets ... a fan-shaped deposit of sediment formed when a stream's slope is abruptly reduced is called an _____ _____. desert ... are depressions created when a block of ice becomes lodged in glacial deposits and subsequently melts.The rocks and sand picked up by the glaciers were later left where the ice began to melt. These deposits are called glacial till. 0270-0098. Image 14: Parts of ...the sharp ends of a jagged ridge formed by glaciers. the end of an ice sheet that is floating in the sea. a pile of sediment deposited at the end of the glacier. the final time that two glaciers come together. A pile of sediment deposited at the end of the glacier. If waves approach the shore at an angle they: die out before they reach the shore. Wind-blown wind deposit. An example of an estuary is. Chesapeake Bay. ... -glacial deposits called till. Deposition of Clay-indicate low energy-sheltered from waves Glaciers are solid ice that moves exceptionally slowly along the land surface. They erode and shape the underlying rocks. Glaciers also deposit sediments in characteristic landforms. The two types of glaciers are: continental and alpine. Continental glaciers are large ice sheets that cover relatively flat ground. These glaciers flow outward ...24 Oca 2018 ... ... known as loess. The loess deposits produce desert or downwind of glacial outwash, where the fine particles are obtainable. The loess ...For example, wind-blown sands are typically extremely well sorted, while glacial deposits are typically poorly sorted. These characteristics help identify the type of erosion process that occurred. Coarse-grained sediment and poorly sorted rocks are usually found nearer to the source of sediment , while fine sediments are carried farther away. Oct 21, 2020 · Deposits of fine silt blown by wind is called as _____ (a) Loess (b) Barchans (c) Hamada (d) Ripples Answer: (a) Loess. Question 7. Stacks are formed by _____. (a) Wave erosion (b) River erosion (c) Glacial erosion (d) Wind deposion Answer: (a) Wave erosion. Question 8. _____ erosion is responsible for the formation of cirque (a) wind (b ...

Glacial Moraines: The material carried by the glacier, such as rocks big and small, sand and silt, gets deposited and forms glacial moraines. Work of wind. Wind: In the desert, an active agent of erosion and deposition is wind. Mushroom Rocks: In deserts, rocks can be shaped like a mushroom, commonly called mushroom rocks. Sand Dunes: When the ...physical science. Write a general equation that illustrates the difference between an exothermic reaction and an endothermic reaction. You only need to use the following items in your general equation: reactants, products, and energy. Be sure to include an arrow in writing your equation. Verified answer.Wind-blown wind deposit. An example of an estuary is. Chesapeake Bay. Black fine-grained sediments are typically deposited in. The deep marine. ... -glacial deposits called till. Deposition of Clay-indicate low energy-sheltered from waves-commonly formed in lagoons-shale splits into thin layersOct 19, 2023 · This layer of fine, mineral-rich material is called loess. Loess is mostly created by wind, but can also be formed by glaciers. When glaciers grind rocks to a fine powder, loess can form. Streams carry the powder to the end of the glacier. This sediment becomes loess. Loess ranges in thickness from a few centimeters to more than 91 meters (300 ... 1. water is minimal or absent; 2. sparse vegetation. Why are deserts strongly impacted by wind processes. suspended load. all material temporarily or permanently suspended in the flow. bed load. the material the current carries along the bed by sliding and rolling. saltation. an intermittent jumping motion along the bed.

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It is the great equalizer of the atmosphere, transporting heat, moisture, pollutants, and dust great distances around the globe. Landforms, processes, and impacts of wind are called Aeolian landforms, such as sand dunes and Loess deposits, which are deposits of silt. Differences in atmospheric pressure generate winds.Deflation is a serious problem for farmers. T. Wind erosion is most effective in moist regions with relatively hard rocks. F. The windward side of a dune has a steeper slope than the slipface. F. Ventifacts are rocks that are smoothed by wind abrasion. T. All the material eroded by the wind is eventually deposited.Examine the five words and/or phrases and determine the relationship among the majority of words/phrases. Choose the one option that does not fit the pattern. A. chalk B. coccolithophores C. diatoms D. limestone E. stromatolites. C. diatoms. Study Chapter 4 flashcards. Create flashcards for FREE and quiz yourself with an interactive flipper. Typical loess (so called “primary loess”) usually has a yellow or pale yellow color. Coarse silt particles (10–50 μm in diameter) make 40–70% of typical loess by weight. This size fraction of particles is characteristic of eolian dust deposits and commonly is called the “basic,” “loess” or “loessic” fraction. The percentage ..." 100 Km. Page 2. INTERPRETATION OF WIND-BLOWN (AEOLIAN) DEPOSITS OF WISCONSIN ... are developed at least in part from a blanket of wind-laid silt called loess ...Glaciers, Deserts & Wind, Oceans & Shorelines. Terms in this set (224) ... The line separating areas where snow, deposited during the winter, disappears during the summer from those areas where the snow remains throughout the year. Alpine or Valley Glacier. form on mountain summits and flow downslope, following former stream valleys. ...

Oct 19, 2023 · This layer of fine, mineral-rich material is called loess. Loess is mostly created by wind, but can also be formed by glaciers. When glaciers grind rocks to a fine powder, loess can form. Streams carry the powder to the end of the glacier. This sediment becomes loess. Loess ranges in thickness from a few centimeters to more than 91 meters (300 ... Loess deposits and wind-blown dust. Wind-blown atmospheric dust is a major driver of global climate change. Dust impacts incoming solar radiation, changes cloud formation and drives changes in oceanic productivity. Sequences of wind-blown dust called loess have been deposited over 10s of millions of years and cover 10% of the continents, while ...a deposit of wind blown silt and clay composed of unweathered, angular grains of quartz, feldspar, and other minerals weakly cemented by calcite ... cobble that has been polished and abraded by wind action is called a. ventifact. A deeply curved dune with its horns pointing downwind is a. barchan dune. ... Glaciers and Glaciation. 50 terms ...This layer of fine, mineral-rich material is called loess. Loess is mostly created by wind, but can also be formed by glaciers. When glaciers grind rocks to a fine powder, loess can form. Streams carry the powder to the end of the glacier. This sediment becomes loess. Loess ranges in thickness from a few centimeters to more than 91 meters (300 ...The term "glacial drift" applies to: a. glacial deposits of very fine particles that eventually become wind-blown. b. glacial deposits that are carried by meltwater into nearby streams. c. all glacial deposits, collectively. d. the redistribution of glacial deposits by consecutive advances. Deposits of fine-grained wind-blown glacial sediment are called loess. Fluvial [ edit ] In geology , physical geography , and sediment transport, fluvial processes relate to flowing water in natural systems.Wind-blown deposits and ___ lakes are features of desert environments. ... Drift deposited by fluvial processes issuing from melting glaciers is called ___. Upgrade ... Yukon paleosol. The lower glacial outwash deposits have a clay-rich, reddish soil horizon indicating a long period of soil formation and soil weathering. The upper wind-blown loess deposit is much younger and is less weathered. The sand wedge into the outwash deposit is evidence of a period of intensive frost action that affected the lower soil ... • marine deposits (glaciomarine) • loess (wind-blown silt) • sand dunes (usually reworked outwash) Glaciofluvial deposits (these are also called glacial outwash) • Mainly sand and gravel; fine material (silt and clay) is either carried farther downstream into areas not recognizably glacial, or blown away by the windTypical loess (so called “primary loess”) usually has a yellow or pale yellow color. Coarse silt particles (10–50 μm in diameter) make 40–70% of typical loess by weight. This size fraction of particles is characteristic of eolian dust deposits and commonly is called the “basic,” “loess” or “loessic” fraction. The percentage ...Examine the five words and/or phrases and determine the relationship among the majority of words/phrases. Choose the one option that does not fit the pattern. A. chalk B. coccolithophores C. diatoms D. limestone E. stromatolites. C. diatoms. Study Chapter 4 flashcards. Create flashcards for FREE and quiz yourself with an interactive flipper. Deserts with a pebble surface are called _____ . draas barchans regs ergs. Which of the …

The Great Lakes. The Great Lakes are a prominent geologic feature of the Midwest and include three of the five largest lakes in the world: Lake Superior, Lake Michigan, and Lake Huron. In fact, the Great Lakes contain 21% of the world’s fresh water. A mere 20,000 years ago, the Great Lakes did not exist.

Wind can carry small particles such as sand, silt, and clay. Wind erosion abrades surfaces and makes desert pavement, ventifacts, and desert varnish. Sand dunes are common wind deposits that come in different shapes, depending on winds and sand availability. Loess is a very fine grained, wind-borne deposit that can be important to soil formation.Loess is a geologic term that refers to deposits of silt (sediment with particles 2-64 microns in diameter) that have been laid down by wind action (aeolian activity to geologists). Extensive, thick loess deposits generally formed in areas bordering large, continental glaciers. Large volumes of meltwater flowed from the edges of these glaciers ...Terms in this set (84) Wind, glaciers, gravity, flowing water and waves. What are the types of weathering? False. Wind causes very little erosion. False. Wind can carry dust for just a few kilometers. true. Particles that the wind moves by traction stays on the ground.the sharp ends of a jagged ridge formed by glaciers. the end of an ice sheet that is floating in the sea. a pile of sediment deposited at the end of the glacier. the final time that two glaciers come together. A pile of sediment deposited at the end of the glacier. If waves approach the shore at an angle they: die out before they reach the shore. Deserts with a pebble surface are called _____ . draas barchans regs ergs. Which of the …Deposits of fine silt blown by wind is called as _____ (a) Loess (b) Barchans (c) Hamada (d) Ripples Answer: (a) Loess. Question 7. Stacks are formed by _____. ... Landforms formed by the glacial …... glacier was exposed and dried out. Winds blew the dust to surrounding areas where it slowly grew into thick silt deposits called loess. Vertical faces of ...Stones that have become polished and faceted due to abrasion by sand particles are called ventifacts (Figure below). As wind blows from different direction, ...Soils deposited by wind are known as aeolian deposits. Loess is a silt …

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Eolian processes pertain to the activity of the winds. Winds may erode, transport, and deposit materials, and are effective agents in regions with sparse vegetation and a large supply of unconsolidated sediments. Although water is much more powerful than wind, eolian processes are important in arid environments.Sandstone depositional environments. The depositional environments are very important and determine the reservoir quality. They sandstone beds range from terrestrial to deep marine, including: Fluvial (alluvial fans, river sediments); Deltaic (levees, distributary deposits ,mouth bars and other sediments formed where river meets a lake …This sediment group is the relatively coarsest sediment group that occurs within the aeolian loess sediments. The grain size is generally in the coarse-grained silt or fine sand range (c. 75 μm), but it does not show one particular modal size.This sediment is always derived from a nearby, rather sandy source region as a river terrace, outcropping …The unconsolidated sand and gravel aquifers shown in figure 4 can be grouped into the following three categories: basin-fill aquifers, referred to as valley-fill aquifers in many reports; blanket sand and gravel aquifers; and glacial-deposit aquifers. A fourth type, called stream-valley aquifers, is located beneath channels, floodplains, and ...d. yardang. e. b, c and d. Yardangs are formed when wind: a. removes all fine particles and exposes the flat bedrock. b. deposits sand in the form of a ridge. c. leaves a pavement of flat pebbles on the ground surface. d. cuts troughs into soft bedrock leaving a ridge of that rock. Sand grains are deposited on the ________ producing crossbeds ...Locally Weighted Regression. loess could be considered as a generalization of the k -nearest neighbor method ( Mitchell et al., 1997 ). It was firstly introduced by Cleveland (1979) and the following analysis is based on Cleveland and Devlin (1988). Loess yi = g ( xi) + ϵi, where i = 1, …, n index of observations, g is the regression ...Sequences of wind-blown dust called loess have been deposited over 10s of millions of years and cover 10% of the continents, while dust is also incorporated into other sediments on land, in the sea and in ice.A loess (US: / ˈ l ɛ s, ˈ l ʌ s, ˈ l oʊ. ə s /, UK: / ˈ l oʊ. ə s, ˈ l ɜː s /; from German: Löss) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loesses or similar deposits.Loess deposits and wind-blown dust. Wind-blown atmospheric dust is a major driver of global climate change. Dust impacts incoming solar radiation, changes cloud formation and drives changes in oceanic productivity. Sequences of wind-blown dust called loess have been deposited over 10s of millions of years and cover 10% of the continents, …The landforms which are created by erosional and depositional activities of wind are called as ... It is defined as a desert area that contains more than 125 ...Etymology and related terms. The word glacier is a loanword from French and goes back, via Franco-Provençal, to the Vulgar Latin glaciārium, derived from the Late Latin glacia, and ultimately Latin glaciēs, meaning "ice". The processes and features caused by or related to glaciers are referred to as glacial. The process of glacier establishment, growth and flow … ….

Sediments are formed from the weathering and erosion of Earth materials. Sediments can be organic, but most are inorganic; their source being a body of rock.from metamorphic rockerosion ...Study with Quizlet and memorize flashcards containing terms like A glacially-carved, deep valley filled with water is called a(n) fjord. moraine. drumlin. esker., A glacier can have only one of which of the following types of moraines? Lateral End Medial Terminal, According to Milankovitch, which of the following is a contributing causative factor to the short-term glacial and interglacial ... For example, wind-blown sands are typically extremely well sorted, while glacial deposits are typically poorly sorted. These characteristics help identify the type of erosion process that occurred. Coarse-grained sediment and poorly sorted rocks are usually found nearer to the source of sediment , while fine sediments are carried farther away. Lake systems and deposits, called lacustrine, form via processes somewhat similar to marine deposits, but on a much smaller scale. Lacustrine deposits are found in lakes in a wide variety of locations. ... Compacted layers of wind-blown sediment are known as loess. Loess commonly starts as finely ground-up rock flour created by glaciers ...Oct 19, 2023 · This layer of fine, mineral-rich material is called loess. Loess is mostly created by wind, but can also be formed by glaciers. When glaciers grind rocks to a fine powder, loess can form. Streams carry the powder to the end of the glacier. This sediment becomes loess. Loess ranges in thickness from a few centimeters to more than 91 meters (300 ... ArticleVocabulary In some parts of the world, windblowndustand siltblanketthe land. This layer of fine, mineral-rich …Terms in this set (84) Wind, glaciers, gravity, flowing water and waves. What are the types of weathering? False. Wind causes very little erosion. False. Wind can carry dust for just a few kilometers. true. Particles that the wind moves by traction stays on the ground.A pile of wind-deposited sand. Mass Wasting. The downslope movement of soil, regolith and rock due directly to gravity. Gravity. Force that pulls objects toward the center of the Earth. Lateral Moraine. Glacial till deposited in a pile or ridge along the sides of a glacier. Deflation. Lifting and movement of loose sand, silt or dust by the wind. Wind-blown glacial deposits are called, This is due to a compilation of the angularity of the sediment particles and also the weak cementation. Loess covers much of the Great Plains of the United States and much of mid latitude Europe where it was blown from glacial outwash deposits, and we'll study the glacial period in an upcoming lesson., Compacted layers of wind-blown sediment are known as loess. Loess commonly starts as finely ground-up rock flour created by glaciers. Such deposits cover thousands of square miles in the Midwestern United States. Loess may also form in desert regions (see Chapter 13). Silt for the Loess Plateau in China came from the Gobi Desert in China and ... , Typical loess (so called “primary loess”) usually has a yellow or pale yellow color. Coarse silt particles (10–50 μm in diameter) make 40–70% of typical loess by weight. This size fraction of particles is characteristic of eolian dust deposits and commonly is called the “basic,” “loess” or “loessic” fraction. The percentage ... , The term dates from pre-Agassiz studies of glacial deposits, when geologists thought that the sediment had “drifted” into place during an immense flood. Specifically, glacial drift includes the following: Sedimentation processes and products associated with glaciation. Glacial sediment is distinctive. Till: Sediment transported by …, Sand piles up in drifts called DUNES. SUSPENDED LOAD - silt is carried away by the wind, sometimes thousands of miles. ... TYPES OF SEDIMENTARY DEPOSITS IN ARID REGIONS 1) Wind blown deposits: ... blankets of silt LOESS (from glacial outwash blowouts) 2) Water deposits: ALLUVIAL FANS (sand and gravel) PLAYAS (ephemeral …, Glacial Moraines: The material carried by the glacier, such as rocks big and small, sand and silt, gets deposited and forms glacial moraines. Work of wind. Wind: In the desert, an active agent of erosion and deposition is wind. Mushroom Rocks: In deserts, rocks can be shaped like a mushroom, commonly called mushroom rocks. Sand Dunes: When the ..., A loess (US: / ˈ l ɛ s, ˈ l ʌ s, ˈ l oʊ. ə s /, UK: / ˈ l oʊ. ə s, ˈ l ɜː s /; from German: Löss) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loesses or similar deposits., 2. Deposition : where agents (causes) of erosion deposit or lay down sediment. Changes the shape of land. B. Geologic Cycle : weathering, erosion and deposition act together in a cycle that wears down and builds up Earth’s surface. – Has continued for billions of years. C. Causes of erosion (agents): 1., This sediment group is the relatively coarsest sediment group that occurs within the aeolian loess sediments. The grain size is generally in the coarse-grained silt or fine sand range (c. 75 μm), but it does not show one particular modal size.This sediment is always derived from a nearby, rather sandy source region as a river terrace, outcropping …, ... glacier, or by wind that blows off of glaciers and redistriubtes fine sediments. Collectively, these sediments are called glacial drift. Till--Till is an ..., A. deflation and sheet wash remove fine-sized materials leaving coarse, weathered, rock fragments concentrated at the surface. Loess deposits in the central United States ____. B. originated as rock flour in Pleistocene glacial streams and rivers. A ____ is a crescent-shaped dune whose tips point downwind., Blown sand Glacial and glaciofluvial features and the distribution of tills in the Elgin district. P915371. Deposits of wind-blown sand occur in many coastal localities. They are most commonly found next to sandy beaches, from where most of the sand has blown, but sandy glaciofluvial deposits have been a source locally., For example, wind-blown sands are typically extremely well sorted, while glacial deposits are typically poorly sorted. These characteristics help identify the type of erosion process that occurred. Coarse-grained sediment and poorly sorted rocks are usually found nearer to the source of sediment , while fine sediments are carried farther away., Glacial deposits are called till. Wind deposits are referred to as aeolian deposits and include loess, dunes, and hills. What are the most common wind deposits?, true or false: most sand carried by the wind moves by saltation. true. true or false: the steeper the slope of a sand dune is on the windward side, the side protected but the wind. false. true or false: wind erosion tends to occur in areas of heavy vegetation cover. false., Deserts with a pebble surface are called _____ . draas barchans regs ergs. Which of the …, This secondary process of transport and deposition creates additional glacial landforms. Unlike till, these structures are generally sorted by grain size because the main agent of transport is flowing water. Water flowing along the base of the glacier carries and deposits sediment in a manner similar to a river., Erosion is the opposite of deposition, the geological process in which earthen materials are deposited, or built up, on a landform. Most erosion is performed by liquid water, wind, or ice (usually in the form of a glacier ). If the wind is dusty, or water or glacial ice is muddy, erosion is taking place. The brown color indicates that bits of ..., Eolian processes pertain to the activity of the winds. Winds may erode, transport, and deposit materials, and are effective agents in regions with sparse vegetation and a large supply of unconsolidated sediments. Although water is much more powerful than wind, eolian processes are important in arid environments., Glacial Moraines: The material carried by the glacier, such as rocks big and small, sand and silt, gets deposited and forms glacial moraines. Work of wind. Wind: In the desert, an active agent of erosion and deposition is wind. Mushroom Rocks: In deserts, rocks can be shaped like a mushroom, commonly called mushroom rocks. Sand Dunes: When the ..., D. in areas where more snow falls than melts. 7. The loosening and lifting of blocks of rock by glaciers is called ____. A. plucking. 8. Material deposited directly by a glacier is called ____. C. till. 9. Icebergs are produced when large pieces of ice break off from the front of a glacier during a process called ____., This often happens when the wind has to move over, or around, an obstacle. A rock or tree may cause wind to slow down. As the wind slows, it deposits the largest particles first. Different types of deposits form depending on the size of the particles deposited. Deposition of Sand. When the wind deposits sand, it forms small hills of sand., These so called ... Figure 7: A thick loess deposit dating from the last glacial period in central Nebraska, U.S.A.. The wind-blown silt particles that form this ..., Study with Quizlet and memorize flashcards containing terms like True or False: Running water is an important erosional agent in many arid lands despite infrequent rainfalls., True or false: Moraines are the only glacial deposits composed of till, Which of the following did not exist prior to the Quaternary Ice ages? a) the Mississippi River b) the Great Lakes c) …, Aug 11, 2023 · Loess is the term given to silt that accumulates due to windblown dust. It is usually highly porous. Windblown deposits of mineral-rich dust and silt is called loess. The term comes from the ... , • marine deposits (glaciomarine) • loess (wind-blown silt) • sand dunes (usually reworked outwash) Glaciofluvial deposits (these are also called glacial outwash) • Mainly sand and gravel; fine material (silt and clay) is either carried farther downstream into areas not recognizably glacial, or blown away by the wind, Dec 1, 2022 · Introduction Aeolian landforms are shaped by the wind (named for the Greek God of wind, Aeolus). Aeolian processes create a number of distinct features, through both erosion and deposition of sediment, including: Sand dunes Loess Deposits Ventifact Yardangs Deflation Hollow or Blowout Desert Pavement , Study with Quizlet and memorize flashcards containing terms like A glacially-carved, deep valley filled with water is called a(n) fjord. moraine. drumlin. esker., A glacier can have only one of which of the following types of moraines? Lateral End Medial Terminal, According to Milankovitch, which of the following is a contributing causative factor to the short-term glacial and interglacial ..., Erosion is the opposite of deposition, the geological process in which earthen materials are deposited, or built up, on a landform. Most erosion is performed by liquid water, wind, or ice (usually in the form of a glacier ). If the wind is dusty, or water or glacial ice is muddy, erosion is taking place. The brown color indicates that bits of ..., Study with Quizlet and memorize flashcards containing terms like A glacially-carved, deep valley filled with water is called a(n) fjord. moraine. drumlin. esker., A glacier can have only one of which of the following types of moraines? Lateral End Medial Terminal, According to Milankovitch, which of the following is a contributing causative factor to the short-term glacial and interglacial ... , Wind-blown deposits and ___ lakes are features of desert environments. ... Drift deposited by fluvial processes issuing from melting glaciers is called ___. Upgrade ... , Study with Quizlet and memorize flashcards containing terms like 01) Sediment that begins as rocks on continents or islands is called ________. A) biogenous sediment B) hydrogenous sediment C) cosmogenous sediment D) lithogenous (terrigenous) sediment, 02) High-energy environments are most likely to deposit which one of the following? A) Cosmogenous sediments B) Silt-sized particles C ..., A. Develop hillsides with roads so they become stable. B. Allow septic systems to run unmaintained so that they provide a source of nutrients for the soil. C. Build homes in steep terrain in order to stabilize the slope. D. Avoid construction and structures on vulnerable slopes. Verified answer.