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Negit Island in Mono Lake is volcanic due to lava flows within the island. Former shore lines indicate dropping water levels in the lake. Tufa formations were created by freshwater springs entering the lake. Convict Lake was created by nearby glaciers' waterflow. Moraines are glacial deposits. Older rock formations are caused by mountain bunching.
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The document summarizes the 2004 Boscastle flood in Cornwall, England. It describes how heavy rainfall caused flash flooding in the town, with over 185mm of rain falling in just a few hours. The floodwaters rose rapidly, damaging homes and businesses and injuring some residents. While no lives were lost, the economic effects on the town's tourism-dependent economy were long-lasting as accommodations had to close for an extended period to recover. The document also discusses some of the factors that contributed to the flooding and measures taken to help prevent future floods.
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The document summarizes the 2004 Boscastle flood in Cornwall, England. It describes how heavy rainfall caused flash flooding in the town, with over 185mm of rain falling in just a few hours. The floodwaters rose rapidly, damaging homes and businesses and injuring some residents. While no lives were lost, the economic effects on the town's tourism-dependent economy were long-lasting as accommodations had to close for an extended period to recover. The document also discusses some of the factors that contributed to the flooding and measures taken to help prevent future floods.
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The numbers refer to:
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Heavy rainfall in August 2004 caused flash flooding in the village of Boscastle in Cornwall, damaging homes and businesses. The physical causes were intense rainfall over a short period which the small rivers could not cope with, exacerbated by steep slopes and saturated ground. Human factors included development in a narrow floodplain and an increased summer population. The effects included economic losses, property damage, infrastructure disruption and mental trauma for residents from the devastation. While Boscastle has always been at flood risk, some experts believe climate change may be increasing the potential for extreme storms.
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On August 16, 2004, the village of Boscastle in Cornwall, England suffered a devastating flash flood. Over 6cm of rain fell in just two hours, causing over 3 million liters of water to rush suddenly through the village, damaging buildings, cars, and infrastructure. The flood waters blocked bridges and overwhelmed the local river, causing extensive property damage estimated at over 2 million pounds. While no lives were lost, the tourism-dependent economy of Boscastle was severely impacted by the flood.
14307 Davis St , Blue Island, Illinois 60406
Great split Level home on a double lot. Home features 3 beds and 2 baths, separate living and dining room. Vaulted ceilings in the living room, dining room and
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The document discusses the Mississippi River. It states that the Mississippi River is the second longest river in North America at 2,320 miles long, running from Lake Itasca to the Gulf of Mexico. When combined with its tributaries, the Missouri and Jefferson Rivers, it forms the third longest river system in the world at approximately 3,900 miles long. The document also includes a poem about the Mississippi River called "Ol' Man River".
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South Carolina has a long history dating back to being one of the original 13 colonies. It played an important role in the Civil War, with the first shots being fired at Fort Sumter. The state capital is Columbia, and the state motto is "While I breathe, I hope." Major tourist attractions include Myrtle Beach, Fort Sumter, and the Riverbank Zoo. South Carolina has a diverse economy focused on agriculture, tourism, and other industries.
Boscastle 2004
The document summarizes the Boscastle floods that occurred on August 16, 2004 in Boscastle, North Cornwall. Heavy rainfall of 185mm in under 5 hours caused the Valency, Jordan and Paradise rivers to flood. The physical causes were the convergence of the three rivers in the small village, heavy rainfall from frontal weather systems, and steep, narrow valleys with thin soils that resulted in rapid runoff. Human causes included development on the narrow floodplain and increased population from tourism that doubled during the season. Effects included 58 flooded properties, four demolished homes, and over 100 vehicles lost in the floods or harbor.
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Storm 13
The river Sid experienced very rough weather and high waters on March 15, 2008 due to storms. The water level rose to three times higher than normal, flooding the surrounding banks that were half a foot deep. It took over a week for the river to recover from the three serious storms that pushed water levels almost to bursting. While the river did not overflow its banks, the storms left lots of debris in the muddy, murky water that obscured visibility of the river bottom.
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Flooding 4 Boscastle
The numbers refer to:
- 16 August 2004 - The date of the Boscastle floods
- 90 - The amount of rainfall in millimetres that fell in one hour
- 3 - The height of the flood wall of water in metres
- 4.5 million - The cost in pounds of the flood defence scheme
- 0 - The number of lives lost, thanks to the rescue operation
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The document summarizes information about the 2004 Boscastle flood in Cornwall, England. Heavy rainfall of 185mm in 5 hours caused the rivers Valency and Jordan to flood the village. The steep sides and lack of floodplains meant surface runoff rapidly increased. Over 440 million gallons of floodwater poured through Boscastle's main street, causing extensive property damage but no deaths. The flood highlighted the village's vulnerability from being built on a narrow floodplain.
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This document provides a brief tour of Victoria, BC including sights of ducks at Beacon Park pond, snow-capped mountains in the distance, large tulip flowers, beautiful neighborhoods, a climbing tree, and views of the harbor and downtown Victoria from the Marriott hotel where the author is staying.
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This document lists various geographic locations in Eastern Canada and New England, including provinces, islands, peninsulas, mountains, valleys, rivers, straits, bays, and cities. There are 26 items on the list, ranging from the Adirondack Mountains to White Mountains, and locations such as New Brunswick, Nova Scotia, Newfoundland, Labrador, and bodies of water including the St. Lawrence River and Bay of Fundy.
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Boscastle, a small village in north Cornwall, experienced catastrophic flooding on August 17, 2004 when over 3 million tons of water accumulated in the narrow valleys surrounding the village within just 5 hours. The heavy rainfall was caused by an extreme weather event that saturated the soils which limited the absorption of additional water, causing widespread surface runoff and flooding as the three converging rivers overflowed their banks. The narrow, steep valleys exacerbated the flooding in Boscastle by restricting water flow, while human development had removed vegetation and built on the flood plain, worsening the impacts.
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Geography 5 photo journal final
The document is a photo journal from a Geography 5 class containing photos and descriptions of various geographic locations in California, including:
- Cinder Hill, an inactive basaltic volcano last erupted 20,000 years ago near an area occupied by the Coso Indians.
- Fossil Falls, formed when lava flows met the waters of Owens Lake, altering the rock's texture.
- Evidence of the semi-nomadic Coso Indians like house rings, metate holes, and obsidian flakes used for arrowheads and knives.
- Features showing evidence of past rivers and lakes like stream beds, former shorelines, and remnants of the size the Owens River had before the Los Angeles aqu
Geography 5 photo journal
This document summarizes Jeanette Hernandez's geology field trips from October 6th and November 16-18th, 2012. It includes descriptions and images of Mormon Rocks, Cinder Hill Volcano, Fossil Falls, Mt. Whitney, the Inyo-White Mountains, an alluvial fan, Diaz Lake, the Lone Pine Fault, Manzanar, Mono Lake, Panum Crater, Convict Lake, Keoughs Hot Springs, the June Lake Loop, the Owens River, the Eastern California Museum, a solar power plant, Doppler radar tower, the Garlock Fault, desert vegetation including the Joshua tree and creosote, the California Aqueduct, and Owens Dry Lake.
Field Journal: Geography 5
This field journal summarizes Kiran Simmons' geology field trip on October 9, 2010 and November 5-7, 2010. The October trip covered Mormon Rocks, Cinder Hill, and Fossil Falls, where Simmons observed and photographed the unique rock formations, lava flows, stream beds, and other geographic features. The November trip included locations like Mt. Whitney, Mono Lake, Panum Crater, and Manzanar internment camp, allowing Simmons to study orographic effects, shorelines, volcanic craters, and historic sites. Simmons' detailed notes and images provide a record of the important geographic features and landscapes observed during the two educational trips.
Photographic Field Journal
The document summarizes Brandon Thrakulchavee's photographic field journal from trips to various locations in California's Eastern Sierra region. Some key locations visited included the Coso Volcanic Range, Fossil Falls, Mormon Rocks, Diaz Lake, Mt. Whitney Visitors' Center, Keough's Hot Springs, Mono Lake, Convict Lake, the Owens River, and the Eastern California Museum. The journal entries describe the unique volcanic, glacial, and geological features found at each site and include photographs taken by Brandon.
Presantation4
The document summarizes two field trips taken by a geography class. The first trip visited Cinder Hill volcano, Fossil Falls waterfall, and Mormon Rocks formation. Cinder Hill is a reddish cinder cone volcano between mountain ranges. Fossil Falls was created by an Owens River flowing through lava. Mormon Rocks shows evidence of the San Andreas Fault and contains sedimentary layers. The second trip visited Diaz Lake pond, Keoughs Hot Springs, Mt. Whitney, Mono Lake, Convict Lake, and the Manzanar internment camp. Diaz Lake was formed by an earthquake. Keoughs Hot Springs is heated by underground volcanic activity. Manzanar housed Japanese Americans during World War II.
Joanna Angeles Geography 5 Photo Journal 11/28/12
Mormon Rocks were formed by water carrying sediments along the San Andreas Fault. Their shape is a result of wind and precipitation acting on the uplifted sandstone formations. Cinder Hill is a cinder cone volcano made of basalt in the Coso Volcanic Field. Fossil Falls was formed by volcanic activity and melted water from glaciers creating a river that smoothed and rounded the basalt rocks. Native Americans who lived in the area created petroglyphs and house rings from local obsidian and basalt.
Geography 5 field trip
The document summarizes a geography field trip taken by Martha Aguayo and Lisa Schmidt. It describes several sites visited, including Mormon Rocks formed from erosion of sandstone with holes where larger rocks used to be; the San Andreas Rift Zone; Cinder Hill cinder cone volcano that last erupted 500 years ago; lava flows from Cinder Hill and other volcanoes; Fossil Falls stream bed smoothed by water with metate holes, obsidian flakes, petroglyphs, and house rings left by Native Americans; Mt. Whitney and the Sierra Nevada mountains' rain shadow effect; the Manzanar internment camp for Japanese Americans during WWII; beetle bark infestation in Mammoth; Mono
Photo journal
The document describes various geographic and geological features found around Fossil Falls State Park and the Coso Volcanic Field in California. It discusses how Fossil Falls was formed by meltwater from glaciers, and describes Native American artifacts and structures found in the area like metate holes, obsidian flakes, petroglyphs, and home rings. It also summarizes information about Mormon Rocks, the San Andreas Fault, and plant life commonly found in the Mojave Desert region.
Geography 5 Photo Journal - by: Juan Vasquez
This document contains photos and descriptions from Juan Vasquez of various geographic locations in California, including:
- Rock formations in the Cajon Pass created by the San Andreas Fault.
- Mormon Rocks showing layers of sandstone from periods of high and low rainfall.
- A stream bed and evidence of past water flow.
- Features around Mono Lake such as tufa towers, shorelines, and islands.
- Lakes and glacial formations around Mammoth Lakes and June Lake.
- The Japanese internment camp at Manzanar during WWII.
- Various other sites showcasing volcanic activity, faults, plants, and infrastructure like aqueducts and radar towers.
geography 5 photo journal
The photo journal documents trips to Mormon Rocks, Cinder Hill, Fossil Falls, Mono Lake, and other locations in Eastern California. Key points include:
- Mormon Rocks were formed by wind and water erosion over decades and consist of sandstone and other rocks.
- Cinder Hill is a composite volcano and cinder cone near the San Andreas rift zone, a strike slip fault.
- Fossil Falls was formed by volcanic activity and melt water from glaciers in the Sierra Nevada mountains.
- Mono Lake and Negit Island were affected when water was diverted from creeks to the Los Angeles Aqueduct, lowering lake levels.
- The Owens River and Owens Dry Lake show
Geography 5 Photo Journal
This document summarizes Steven Li's photo journal from two geography lab trips. On the first trip, photos were taken of Mormon Rocks formed by the San Andreas fault, Cinder Hill cinder cone volcano and lava flows, and Fossil Falls featuring metate holes, obsidian flakes, and Native American petroglyphs and house rings. The second trip featured photos of Diaz Lake formed by an earthquake, Mono Lake with islands and shorelines, Panum Crater, Convict Lake and its moraines, Keoughs Hot Springs, the June Lake Loop including Grant and Silver Lakes, and Mt. Whitney showing the orographic effect.
The Scenic Housatonic River Watershed
The Housatonic River winds through western Connecticut from Massachusetts to Long Island Sound, encompassing a scenic watershed. The river features rushing waterfalls, farms and wineries, historic covered bridges, and many spots for recreation like fishing, hiking, and camping. Arts and culture thrive throughout the communities in the watershed, and more adventurous activities like sections of the Appalachian Trail also exist alongside relaxed scenic walks. Several large lakes formed by dams are popular recreation areas on the Housatonic River.
Geog5 field trip journal & Field Questions
The document summarizes Adela Lopez's field trip journal from a geography class trip. The trip included visits to Mormon Rocks Formation near the San Andreas Fault, Fossil Falls which shows evidence of ancient lake flows, cinder hill from volcanic activity, and Convict Lake. Sites provided evidence of Native American habitation and included house rings, petroglyphs, and obsidian flakes. Stops also included Mono Lake to see tufa formations and former shorelines, and Owens River valley. The trip gave insights into geology, ecology and helped the student appreciate their environment.
Geography 5
The Mormon Rocks were formed by the tilted San Andreas fault where the North American and Pacific plates meet. The layers in the rocks show past rainfall amounts, with larger rock pieces indicating more rain. The San Andreas Rift Zone near Cajon Pass was created by an ancient stream bed during an 1857 earthquake. Fossil Falls was formed by water from melted glaciers that created lakes, including Owens Lake, and volcanic activity in nearby mountain ranges. Manzanar was one of the camps that incarcerated over 110,000 Japanese Americans during World War 2, located between Lone Pine and Independence in Owens Valley.
NWIFC Magazine Fall 2008
Inside:
Protecting Headwater Streams
Bacteria Threaten Shellfsh
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Pocket Estuaries Provide Refuge
Chinook Get Population Boost
Logjams Constructed for Salmon
Geography 5 digital photo journal
The document is a digital photo journal created by Rolie Mendoza from March 8 to April 6, 2014. It contains photos and descriptions from various locations in California, including Mormon Rocks, Cinder Hill, Fossil Falls, Mt. Whitney Visitors Center, Diaz Lake, Manzanar, Mammoth Area, Mono Lake, Keoughs Hot Springs, Convict Lake, June Lake Loop, and the Eastern California Museum. The photos document geological features such as volcanic formations, faults, lakes, and streams, as well as historical sites related to Native Americans and Japanese internment camps.
Geography 5
The document summarizes key geographic features observed during a field trip, including:
Cinder Hill, a cinder cone volcano formed from lava blobs; Fossil Falls, with basalt rocks carved by glacial flows; Mormon Rocks, a sedimentary formation showing layers from past rainfall; and Mono Lake, which contains tufa formations and has higher salinity due to water diversion. The field trip observed evidence of human habitation like obsidian flakes, petroglyphes, and the Manzanar internment camp.
Geog5 Photo J
Gabriel Heimberg documented photos from a geography field trip through California deserts and mountains. The photos showed various landforms like the California Aqueduct, Joshua trees in the desert, a solar power plant, and the SETI satellite dishes. Other photos documented Mormon Rocks by the San Andreas Fault, cinder cones at Cinder Hill, petroglyphs and house rings left by Native Americans, glaciated valleys, and Mono Lake with its receding shoreline and tufa formations. The photos were accompanied by explanations of the geographic features and processes that formed the landscapes.
Gabe'sGeog5photoj
Gabriel Heimberg documented photos from a geography field trip through California deserts and mountains. The photos showed various landforms like the California Aqueduct, Joshua trees in the desert, a solar power plant, and the SETI satellite dishes. Other photos documented Mormon Rocks by the San Andreas Fault, cinder cones at Cinder Hill, petroglyphs and house rings left by Native Americans, glaciated valleys, and Mono Lake with its receding shoreline and tufa formations. The photos were accompanied by explanations of the geographic features and processes that formed the landscapes.
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- 1. OF THE TWO ISLANDS IN MONO LAKE, NEGIT ISLAND IS A VOLCANIC ISLAND DUE TO THE LAVA FLOWS COMPOSED WITHIN THE ISLAND.
- 2. FORMER SHORE LINES INDICATE THE DROP OF WATER LEVELS IN THE LAKE.
- 3. TUFA FORMATIONS WERE CREATED BY THE FRESHWATER SPRINGS THAT ENTERED THE LAKE.
- 5. MT. WHITNEY DISPLAYS THE HIGHEST PEAK IN THE STATE OF CALIFORNIA, AN ASTONISHING 14,505 FEET.
- 10. JUNE LAKE LOOP
- 11. CONVICT LAKE WAS CREATED DUE TO THE WATERFLOW OF NEARBY GLACIERS.
- 12. THESE MORAINES ARE GLACIAL SETTLEMENTS.
- 13. THESE OLDER ROCK FORMATIONS ARE CAUSED BY THE BUNCHING OF MOUNTAINS.
- 14. THE STORY BEHIND CONVICT LAKE
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