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This document provides information about Lathkill Dale, including its location in Derbyshire, England. It describes the area's geological history from the Carboniferous period 340 million years ago to the Pleistocene period 2 million years ago. It then details 5 sites along the dale, noting their geological features such as limestone rock and fossils from the Carboniferous period, a mining hole from lead and iron mining since the 13th century, and Mandale Mine buildings made of limestone. Site 4 describes Bateman's House built of limestone and the nearby Lathkill mine shaft. Site 5 focuses on fossils such as brachiopods and crinoids imprinted in the limestone. The conclusion lists topics
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Lathkill dale
The document summarizes a geology fieldtrip to Lathkill Dale located 5km south of Bakewell in the Derbyshire Dales National Nature Reserve. It describes the landscape which was underwater during the early Carboniferous period approximately 340 million years ago. During the fieldtrip, participants observed limestone bridges with visible fossils, limestone rock with bedding planes dipping north, and an old mining hole used to drain mines for iron and lead since the Bronze Age. The document provides an introduction and overview to the sites visited during the geology presentation and fieldtrip to Lathkill Dale.
Lathkill dale latest
This document summarizes a field trip to Lathkill Dale, located 5km south of Bakewell in Derbyshire, England. It introduces the group members and their roles. The trip covers the geology, history, and landscape of Lathkill Dale. Key sites visited include the entrance with fossilized limestone, areas showing bedding planes and mining holes, and Jacobs Ladder with fossils of brachiopods, sea lilies, and other marine life from the Carboniferous period approximately 340 million years ago. Pictures were meant to be included to illustrate the different fossils, geological features, and historical sites discussed.
Lathkill dale latest
This document outlines the roles of group members and provides information about Lathkill Dale. It describes the location as being 5km south of Bakewell in the Derbyshire Dales National Nature Reserve. The document then discusses the history, landscape, and past and present of Lathkill Dale. Key points along a trail are summarized, including the entrance, three sites that describe the geology and mining history, and site four which details fossils found there like brachiopods and sea lilies. The conclusion recaps the areas covered in the document such as geology, geomorphology, impacts of tourism, industrial archaeology, and biogeography.
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The Twelve Apostles are a collection of limestone rock stacks off the coast of Port Campbell National Park in Australia that were formed when erosion of the limestone cliffs by the Southern Ocean created caves that eventually collapsed, leaving tall rock stacks isolated from the shore. Known originally as the Sow and Piglets and later renamed the Twelve Apostles for tourism despite never having more than nine stacks, the limestone formations were created over 10-20 million years by erosion of the mainland cliffs.
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Pikes Peak is composed of pink granite formed over 1 billion years ago from magma deep within the earth. It was formed in three stages: first, an early Rocky Mountain range was created and eroded; sediment was deposited and covered the area. As the land converged, it pushed the granite batholith upward, exposing it to erosion over millions of years, including glaciers, streams, and wind, carving it into the prominent peak seen today.
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This document provides a summary of the geology of the Burren region in County Clare, Ireland. It describes the various rock formations, from the sedimentary rocks and shale cliffs at Moher to the exposed limestone terraces further north. It explains how the unique karst landscape formed over millions of years and discusses how the geology influences the environment, flora, and fauna of the area. It also examines how human activities have shaped the region over time through practices like livestock grazing and fuel collection. The document aims to establish the geological framework of the Burren and explore the environmental impacts of the distribution of different rock types in the area.
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Lathkill dale
The document summarizes a geology fieldtrip to Lathkill Dale located 5km south of Bakewell in the Derbyshire Dales National Nature Reserve. It describes the landscape which was underwater during the early Carboniferous period approximately 340 million years ago. During the fieldtrip, participants observed limestone bridges with visible fossils, limestone rock with bedding planes dipping north, and an old mining hole used to drain mines for iron and lead since the Bronze Age. The document provides an introduction and overview to the sites visited during the geology presentation and fieldtrip to Lathkill Dale.
Lathkill dale latest
This document summarizes a field trip to Lathkill Dale, located 5km south of Bakewell in Derbyshire, England. It introduces the group members and their roles. The trip covers the geology, history, and landscape of Lathkill Dale. Key sites visited include the entrance with fossilized limestone, areas showing bedding planes and mining holes, and Jacobs Ladder with fossils of brachiopods, sea lilies, and other marine life from the Carboniferous period approximately 340 million years ago. Pictures were meant to be included to illustrate the different fossils, geological features, and historical sites discussed.
Lathkill dale latest
This document outlines the roles of group members and provides information about Lathkill Dale. It describes the location as being 5km south of Bakewell in the Derbyshire Dales National Nature Reserve. The document then discusses the history, landscape, and past and present of Lathkill Dale. Key points along a trail are summarized, including the entrance, three sites that describe the geology and mining history, and site four which details fossils found there like brachiopods and sea lilies. The conclusion recaps the areas covered in the document such as geology, geomorphology, impacts of tourism, industrial archaeology, and biogeography.
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The Twelve Apostles are a collection of limestone rock stacks off the coast of Port Campbell National Park in Australia that were formed when erosion of the limestone cliffs by the Southern Ocean created caves that eventually collapsed, leaving tall rock stacks isolated from the shore. Known originally as the Sow and Piglets and later renamed the Twelve Apostles for tourism despite never having more than nine stacks, the limestone formations were created over 10-20 million years by erosion of the mainland cliffs.
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Pikes Peak is composed of pink granite formed over 1 billion years ago from magma deep within the earth. It was formed in three stages: first, an early Rocky Mountain range was created and eroded; sediment was deposited and covered the area. As the land converged, it pushed the granite batholith upward, exposing it to erosion over millions of years, including glaciers, streams, and wind, carving it into the prominent peak seen today.
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Eskers provided early humans and animals with safe passage across boggy ground, and their elevated positions and sandy soils made them useful for settlements, roadways, grazing livestock, and burials. Geologists have also learned from eskers, as their locations and excavated materials have provided insights into Norfolk's geological history and past climate changes.
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The document is a photo journal from Eric Martinez's geography field trips. It summarizes locations visited and key geographic features photographed. Locations included Mormon Rocks formed by the San Andreas Fault, Cinder Hill volcano, Fossils Falls formed by lava flows diverting a river, and Native American house rings and petroglyphs over 10,000 years old. The second trip covered Mt. Whitney, the Inyo-White Mountains, Diaz Lake formed by an earthquake, the Manzanar internment camp, Mono Lake and islands, shorelines of a shrinking lake, tufa stone formations, Convict Lake of glacial origin, and the oldest local rock formation.
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This document provides a summary of the geology of the Burren region in County Clare, Ireland. It describes the various rock formations, from the sedimentary rocks and shale cliffs at Moher to the exposed limestone terraces further north. It explains how the unique karst landscape formed over millions of years and discusses how the geology influences the environment, flora, and fauna of the area. It also examines how human activities have shaped the region over time through practices like livestock grazing and fuel collection. The document aims to establish the geological framework of the Burren and explore the environmental impacts of the distribution of different rock types in the area.
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- The Jurassic Coast exposes geology spanning millions of years, including rocks from the Jurassic period 200-140 million years ago.
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The document summarizes field assignments completed by Robert Garcia for a geology course on the Bay Area and San Jose. Garcia visited Almaden Quicksilver County Park and Alum Rock Park to observe local geology. At Almaden, he saw cinnabar ore deposits from former mercury mines and learned about the area's mining history. He also observed granodiorite, basalt, and Coast Range fence lizards. At Alum Rock Park, he saw more granodiorite and California poppies, and saw tadpoles in a stream. The document discusses the geological formation of the Bay Area and evolution of local plant and animal species over time.
Abigail taylor 7053583398 - 10 mysterious geological wonders
This document summarizes 10 mysterious geological wonders from around the world, including The Wave in Arizona/Utah, Antelope Canyon in Arizona, the Great Blue Hole off the coast of Belize, the Crystal Cave of the Giants in Mexico, the Eye of the Sahara desert formation in Mauritania, the Blue Lake Cave in Brazil, the Giants Causeway volcanic formations in Ireland, Hell Gate, an underground gas fire that has been burning for 35 years in Uzbekistan, Wave Rock in Australia which is shaped like an ocean wave, and the Chocolate Hills cone-shaped limestone formations in the Philippines.
Boettcher Local Project
The document discusses Northern Dynasty Mine's proposed Pebble Mine Project in Alaska's Bristol Bay Region. It would be one of the largest open pit mines and underground mines in North America. Concerns include potential water contamination from tailings and acid mine drainage affecting the many salmon that spawn in the rivers. The mine would require huge infrastructure like dams and roads, bringing economic benefits but also environmental risks to the fish and wildlife in the area. There is an ongoing debate between potential jobs and money versus risks to the local subsistence lifestyle and world-class salmon fishery.
Allan Ponniah | 10 mysterious geological wonders
This document summarizes 10 mysterious geological wonders from around the world, including The Wave in Arizona/Utah known for its unique rock formations, Antelope Canyon's photogenic slot canyons, the deep blue hole in Belize, giant crystals found in a mine in Mexico, the circular Eye of the Sahara structure in Mauritania, the underground blue lake in Brazil's caves, Northern Ireland's Giants Causeway volcanic formations, a gas fire that has burned for decades in Uzbekistan called Hell Gate, Australia's Wave Rock shaped like an ocean wave, and the cone-shaped Chocolate Hills found in the Philippines.
A guide to central park
This document provides a guide to the geology of Central Park in New York City. It is divided into three sections. Section one describes the building stones used in park structures. Section two examines bedrock outcroppings, showing evidence of NYC's tectonic history over billions of years. Section three inspects evidence left behind by glaciers, including striations and erratic boulders deposited during the last ice age. Stops around the park are detailed, identifying rock types and geological features formed by metamorphism, intrusions, erosion and glaciation.
Crater Lake
Mount Mazama was a large volcano in Oregon that erupted violently 7,700 years ago, collapsing into itself and forming a large caldera that was later filled with water to create Crater Lake. The lake has extremely pure and deep blue water, being the deepest lake in the United States at nearly 2,000 feet deep. In the late 1800s, explorer William Steel advocated to have the area protected as a national park, the 6th in the US, to preserve the unique geology and beauty of Crater Lake.
Mesolithic and Neolithic Ireland
The Mesolithic settlers in Ireland arrived by boat and chose riverbanks, lakesides, and coastal locations for their settlements. They hunted wild pigs and birds and gathered nuts. Tools were made of stone, including flint and chert. The earliest settlements were probably covered by the sea. In the Neolithic period, people began farming and raising cattle, sheep, and goats. They cleared forests for fields and built permanent houses and monuments like court tombs, portal tombs, passage tombs, and wedge tombs for burials.
Waterfalls Of The Rivers Twiss + Doe
The document describes waterfalls located along the River Twiss and River Doe near Ingleton, North Yorkshire. It includes photos and questions about the geology and features of the waterfalls, such as the vegetation, relief, and erosion patterns visible. Differential erosion has created circular plunge pools below harder limestone bands. Over time, waterfalls will move upstream, leaving steep gorges as the erosion process continues.
Sarah Culver's Field Study
Sarah Culver documented various geological features around California's central coast for a field assignment. She observed Morro Rock, a volcanic plug near San Luis Obispo that formed 23 million years ago. She also studied sea otters in Morro Bay and how they evolved adaptations for both land and water over millions of years. Additionally, she identified and analyzed samples of oolitic limestone from Montaña De Oro State Park, pillow basalt from Port San Luis Harbor, and sedimentary rocks containing silica and sandstone. Culver demonstrated principles of relative dating by examining examples of the principle of inclusions near Highway 1 and an angular unconformity at Montaña De Oro.
Meso and neolithic nearpod slideshare
The document provides information on Mesolithic and Neolithic settlers in Ireland. It discusses:
- Mesolithic settlers arrived in Ireland around 7000 BC and settled along river banks and coasts, hunting and gathering food. Evidence from Mount Sandel shows they lived in huts and exploited salmon and other fish.
- In the Neolithic period, around 3500 BC, farming was introduced through clearing forests and domesticating animals. This allowed more permanent settlements and the development of monumental architecture like megalithic tombs, as well as pottery and polished stone tools like porcellanite axes.
Field assignment with revisions
Thunder Mountain is located in Kirkwood, CA between Silver Lake and Kirkwood. The hike begins at 7,600 feet and ends at 9,400 feet. 225 million years ago, the Farallon plate subducted under the Pacific plate causing heat and melting to form magma and granitic plutons. Volcanic activity then built up the mountain through ash, mud, and basaltic rock. Uplifting and tilting further shaped the region. Today, Thunder Mountain is composed primarily of volcanic tuff and ash deposits. Evidence at the site shows the effects of glaciation and erosion over time on the mountain's geology.
Dowth 1
Brú na Bóinne is one of the world's most important archaeological landscapes, containing passage tombs from 5,000 years ago that were designated a UNESCO World Heritage Site. Dowth is one of the three great passage tombs at Brú na Bóinne, surrounded by a kerb of 115 stones with two tombs facing west and smaller tombs to the east and south. Dowth North has an 8.2 meter passage leading to a cruciform chamber with side recesses and annexes, while Dowth South has a shorter passage opening to an almost circular chamber.
Part (3) Of Catfincut
The document describes the geology, archeology, and history of the Lower Catawba River Valley in South Carolina. It notes the presence of various types of rock jointing and mentions Native American artifacts that have been found, including projectile points and pottery pieces. It also discusses the area's more recent history, including a proposed but unsuccessful plan to establish a military academy at Mount Dearborn in 1816. Remnants of old dams, canals, and other industrial infrastructure from the early 1900s are also described.
art as land
This document discusses land art and site-specific artworks created in the late 1960s and 1970s. It features images and information on works by artists such as Nancy Holt, Christine Oatman, Michael Heizer, and Robert Smithson. These works were created in remote natural locations and often incorporated or responded to the landscape. The document examines how these land artworks aimed to reconsider relationships between art, land, and memory.
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Lathkill dale latest
- 2. Lathkill Dale Map Lathkill Dale grid reference = SK 187 658 Lathkill Dale
- 3. Group and Roles •Cheryl Bennett – Note Taker and Fossil researcher. •Deb Royle – Photographer, Presenter and Rock researcher. •Michelle Townsend - Photographer and History writer. •Katy Dixon – Note Taker and PowerPoint designer. •Kelly Marie Farnsworth – Photographer and Summary writer.
- 4. Introduction Location • Lies 5km South of Bakewell. • Part of the Derbyshire Dales National Nature Reserve. History • Traced back to early Carboniferous period. • Approximately 340 million years ago. Landscape • Originally would have been underwater, only peaks visible. • Changed again during Pleistocene period (2 million years ago)
- 6. Entrance •Limestone bridge over river. •Fossils (mainly bivalve molluscs) have been revealed due to the wear of visitors shoes on the now polished stone. •Area was once a limestone mill featuring a large water wheel.
- 7. Site One Limestone rock on side of path. Visible bedding planes dipping to the north. Saturated with water allowing plans and fauna to grow.
- 8. Site Two Mining hole – would have been mined for iron and lead. Mining in Lathkill Dale has taken place since the 13th century. The hole would have been a way of draining the mine for ore. This method was called sough.
- 9. Site Three •Mandale Mine: building is limestone as are the pillars used to carry water over the valley to power the water wheel. •There is a legal obligation to protect the area. •A popular potholing site.
- 10. Site Four • Bateman’s House - built in the 1840’s using primarily limestone. • Windowsills and doorways are made from sandstone as it is weaker /easier to dress. • Below is Lathkill mine, a recently renovated deep mineshaft. •This shaft is home to a water turbine, used to power drainage.
- 11. Site Five Jacobs Ladder fossil area included; Brachiopods also known as Gigantas procuctus (pictured top right) and sea lilies. Limestone was quarried by hammering in large pins, so as to split evenly (pictured bottom right).
- 12. Site Four Continued •Sea lilies, also known as “Derbyshire screw” consisted of a stalk and tentacles. When the lilies died they lay on the sea bed and were imprinted into the fossils we see today (pictured right and below).
Editor's Notes
- Magic – trail. Starting point. Blackboard.