Saturday, April 11, 2020

How to Write a Sample Essay on Myself in French

How to Write a Sample Essay on Myself in FrenchHow to write a sample essay on myself in French is a question I get asked quite often. A lot of students who go through college get English as a second language and they want to go on to a degree program in the French language. They are especially interested in trying to get into prestigious colleges like NYU, Cambridge or Princeton where the chances of being accepted are higher than for anyone else.Since so many students would like to go to France to study their second language, one might think that the English-speaking students would naturally be at a distinct advantage. But this is far from the truth. The truth is that while you may be able to write better in French than your own mother tongue, the chances of you learning French are still better than for anyone else. It will just take more effort on your part.So how do you learn French? And why is it so difficult to learn this language?So how do you start learning French? The first th ing you need to do is make sure that you have all the tools you need to keep yourself well-informed about the culture and history of the place you will be living in, so that you will not be bored. What you will be doing is conversing in the French language, not simply speaking a bunch of words and phrases that you picked up in the English school.When you speak a lot of French, you will be translating a lot of words into English. Therefore, if you want to learn French quickly, the best way to do it is to take a foreign language class or take an immersion class. You can also decide to listen to tapes of recordings of native speakers that will enable you to keep your native tongue in your mind while you are learning French.Another problem with getting past the first two years of college, which is French, is that since the course is so new, there is not much of the French vocabulary to start with. This means that you have to work to expand your vocabulary, which is also very important. At the same time, it will help you develop fluency in your native language and your ability to think about everything in terms of a specific part of your vocabulary.So how to write a sample essay on myself in French is not so hard at all. Just remember to start off with something small and then you will be able to see the results quickly.

Thursday, April 2, 2020

The Geology of The Massif Montgris Essay Example For Students

The Geology of The Massif Montgris Essay Declaration This report entitled The Geology of The Massif Montgris Essay was composed by me and is based in my own work. Where the work of others has been used, it is fully acknowledged in the text and in captions to tables and illustrations. Signed . We will write a custom essay on The Geology of The Massif Montgris specifically for you for only $16.38 $13.9/page Order now Date .. Chapter 1.0 Abstract This is a study of the Massif Montgris, it is based on evidence gathered in the field over 21 days of field work. To supplement this data I have looked at papers and works by previous visitors to the Montgris. The units within the area are from the Upper Cretaceous the Tertiary and the Quaternary. I aim to give an overall guide to the geology on a smaller scale than has previously been accomplished. This study is mainly aimed at correctly dating the units of limestone using micropalaeontological data. The micropalaeontological data has also given light into the palaeoenvironment/geography during deposition. Chapter 2 Introduction 2.0.1 Introduction Between the 24th of June and the 24th of July 1995 Glen Burnham and I ventured to Catalunya. More precisely to Torroella de Montgris. Torroella is in the North East of Spain, just inland of the Mediterranean sea. This remarkable old town lies at the foot of the rather imposing Massif Montgris. Locally known as El Montgris (literally the grey Mountain) the massif rises up over the town and dominates the skyline. Torroella sits on quaternary conglomerate deposits. These are easily eroded, hence the valley between Pals (10Km to the south) and Torroella is extremely flat. The valley is bisected by the river El Ter, which flows at a leisurely pace from the foothills of the Pyrenees. The river flows to the south of Torroella and winds its way to its conclusion in the Playa de Pals (6Km east of Torroella). El Montgris has been known to humans since prehistoric times. It has some large caves on its slopes that served as a shelter to prehistoric man. The area was very popular with the Romans who cultivated the local area, built roads and towns (many of which still stand to this day) such as Peretelada to the south adjacent to Pals. Since the time of the Romans Torroella has grown into a thriving market town. It has always had close links with the Montgris which until recently still served a purpose as a shelter, not , however, against the elements but against Pirates and marauders from the sea. In fact, on top of the Muntanya Santa Catherina stands the remains of a thirteenth century castle (the last castle ever built in Spain). El Montgris has provided for the local commerce since it was first settled. The local people value the Mountains greatly and still use them today. The rock from which our dwelling was made was quarried from the mountain, the castle rock was quarried on the mountain. 2.0.2 Aims of Study. When I first considered the Montgris as a project area I realised that information would be sparse and that the project would be more complicated than a similar project in the U.K because the environment is so very different and resources would be a great deal more difficult to access (due to the language barrier). I also realised the project would probably be very different to the proposal. Before Glen and I left England we attempted to research the Massif Montgris through the usual channels in order to get an idea of what we would be facing. The research lead to a few vague leads, we new the rock was sedimentary and most likely limestone. Having visited the area previously I could recall a little about the rocks but was certain of their sedimentary nature. .udbb2c68fb78f3bb9dd1166fffc6e3f2a , .udbb2c68fb78f3bb9dd1166fffc6e3f2a .postImageUrl , .udbb2c68fb78f3bb9dd1166fffc6e3f2a .centered-text-area { min-height: 80px; position: relative; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a , .udbb2c68fb78f3bb9dd1166fffc6e3f2a:hover , .udbb2c68fb78f3bb9dd1166fffc6e3f2a:visited , .udbb2c68fb78f3bb9dd1166fffc6e3f2a:active { border:0!important; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a .clearfix:after { content: ""; display: table; clear: both; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a:active , .udbb2c68fb78f3bb9dd1166fffc6e3f2a:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a .centered-text-area { width: 100%; position: relative ; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a:hover .ctaButton { background-color: #34495E!important; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a .udbb2c68fb78f3bb9dd1166fffc6e3f2a-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .udbb2c68fb78f3bb9dd1166fffc6e3f2a:after { content: ""; display: block; clear: both; } READ: Dantes' Power and Limitations EssayOur first lead came from an unexpected source. My parents had vacationed in the area and upon my request had asked locally about any information pertaining to the Geology. The result was that they brought back a research map that dated the Massif as Cretaceous but suggested it was composed of 1 massive bed. We loosely agreed our study areas and arranged our projects accordingly. The local guide books and map had supplied us with information about the palaeontology (macro fossils) which suggested the rock was full of bivalves, brachiopods, corals and belemnites. Before leaving we were unable to unearth much more information BUT seemingly at the last minute we were able to make contact with Dr. David Brusi from the Universidad de Gerona(departament del geophysica) who reassured us that upon our arrival in Spain he would brief us on geology of El Montgris. Therefore, with very little in the way of . The Geology of The Massif Montgris Essay Example For Students The Geology of The Massif Montgris Essay The Geology of The Massif Montgris Essay Declaration This report entitled The Geology of the Massif Montgris was composed by me and is based in my own work. Where the work of others has been used, it is fully acknowledged in the text and in captions to tables and illustrations. We will write a custom essay on The Geology of The Massif Montgris specifically for you for only $16.38 $13.9/page Order now Signed . Date .. Chapter 1.0 Abstract This is a study of the Massif Montgris, it is based on evidence gathered in the field over 21 days of field work. To supplement this data I have looked at papers and works by previous visitors to the Montgris. The units within the area are from the Upper Cretaceous the Tertiary and the Quaternary. I aim to give an overall guide to the geology on a smaller scale than has previously been accomplished. This study is mainly aimed at correctly dating the units of limestone using micropalaeontological data. The micropalaeontological data has also given light into the palaeoenvironment/geography during deposition. Chapter 2 Introduction 2.0.1 Introduction Between the 24th of June and the 24th of July 1995 Glen Burnham and I ventured to Catalunya. More precisely to Torroella de Montgris. Torroella is in the North East of Spain, just inland of the Mediterranean sea. This remarkable old town lies at the foot of the rather imposing Massif Montgris. Locally known as El Montgris (literally the grey Mountain) the massif rises up over the town and dominates the skyline. Torroella sits on quaternary conglomerate deposits. These are easily eroded, hence the valley between Pals (10Km to the south) and Torroella is extremely flat. The valley is bisected by the river El Ter, which flows at a leisurely pace from the foothills of the Pyrenees. The river flows to the south of Torroella and winds its way to its conclusion in the Playa de Pals (6Km east of Torroella). El Montgris has been known to humans since prehistoric times. It has some large caves on its slopes that served as a shelter to prehistoric man. The area was very popular with the Romans who cultivated the local area, built roads and towns (many of which still stand to this day) such as Peretelada to the south adjacent to Pals. Since the time of the Romans Torroella has grown into a thriving market town. It has always had close links with the Montgris which until recently still served a purpose as a shelter, not , however, against the elements but against Pirates and marauders from the sea. In fact, on top of the Muntanya Santa Catherina stands the remains of a thirteenth century castle (the last castle ever built in Spain). El Montgris has provided for the local commerce since it was first settled. The local people value the Mountains greatly and still use them today. The rock from which our dwelling was made was quarried from the mountain, the castle rock was quarried on the mountain. 2.0.2 Aims of Study. When I first considered the Montgris as a project area I realised that information would be sparse and that the project would be more complicated than a similar project in the U.K because the environment is so very different and resources would be a great deal more difficult to access (due to the language barrier). I also realised the project would probably be very different to the proposal. Before Glen and I left England we attempted to research the Massif Montgris through the usual channels in order to get an idea of what we would be facing. The research lead to a few vague leads, we new the rock was sedimentary and most likely limestone. Having visited the area previously I could recall a little about the rocks but was certain of their sedimentary nature. .u2d51b0d7c9142b568ff0682a11fc18d7 , .u2d51b0d7c9142b568ff0682a11fc18d7 .postImageUrl , .u2d51b0d7c9142b568ff0682a11fc18d7 .centered-text-area { min-height: 80px; position: relative; } .u2d51b0d7c9142b568ff0682a11fc18d7 , .u2d51b0d7c9142b568ff0682a11fc18d7:hover , .u2d51b0d7c9142b568ff0682a11fc18d7:visited , .u2d51b0d7c9142b568ff0682a11fc18d7:active { border:0!important; } .u2d51b0d7c9142b568ff0682a11fc18d7 .clearfix:after { content: ""; display: table; clear: both; } .u2d51b0d7c9142b568ff0682a11fc18d7 { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .u2d51b0d7c9142b568ff0682a11fc18d7:active , .u2d51b0d7c9142b568ff0682a11fc18d7:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .u2d51b0d7c9142b568ff0682a11fc18d7 .centered-text-area { width: 100%; position: relative ; } .u2d51b0d7c9142b568ff0682a11fc18d7 .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .u2d51b0d7c9142b568ff0682a11fc18d7 .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .u2d51b0d7c9142b568ff0682a11fc18d7 .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .u2d51b0d7c9142b568ff0682a11fc18d7:hover .ctaButton { background-color: #34495E!important; } .u2d51b0d7c9142b568ff0682a11fc18d7 .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .u2d51b0d7c9142b568ff0682a11fc18d7 .u2d51b0d7c9142b568ff0682a11fc18d7-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .u2d51b0d7c9142b568ff0682a11fc18d7:after { content: ""; display: block; clear: both; } READ: History of the Conservative Movement EssayOur first lead came from an unexpected source. My parents had vacationed in the area and upon my request had asked locally about any information pertaining to the Geology. The result was that they brought back a research map that dated the Massif as Cretaceous but suggested it was composed of 1 massive bed. We loosely agreed our study areas and arranged our projects accordingly. The local guide books and map had supplied us with information about the palaeontology (macro fossils) which suggested the rock was full of bivalves, brachiopods, corals and belemnites. Before leaving we were unable to unearth much more information BUT seemingly at the last minute we were able to make contact with Dr. David Brusi from the Universidad de Gerona(departament del geophysica) who reassured us that upon our arrival in Spain he would brief us on geology of El Montgris. Therefore, with very . The Geology of The Massif Montgris Essay Example For Students The Geology of The Massif Montgris Essay The Geology of The Massif Montgris Essay Declaration This report entitled The Geology of the Massif Montgris was composed by me and is based in my own work. Where the work of others has been used, it is fully acknowledged in the text and in captions to tables and illustrations. We will write a custom essay on The Geology of The Massif Montgris specifically for you for only $16.38 $13.9/page Order now Signed . Date .. Chapter 1.0 Abstract This is a study of the Massif Montgris, it is based on evidence gathered in the field over 21 days of field work. To supplement this data I have looked at papers and works by previous visitors to the Montgris. The units within the area are from the Upper Cretaceous the Tertiary and the Quaternary. I aim to give an overall guide to the geology on a smaller scale than has previously been accomplished. This study is mainly aimed at correctly dating the units of limestone using micropalaeontological data. The micropalaeontological data has also given light into the palaeoenvironment/geography during deposition. Chapter 2 Introduction 2.0.1 Introduction Between the 24th of June and the 24th of July 1995 Glen Burnham and I ventured to Catalunya. More precisely to Torroella de Montgris. Torroella is in the North East of Spain, just inland of the Mediterranean sea. This remarkable old town lies at the foot of the rather imposing Massif Montgris. Locally known as El Montgris (literally the grey Mountain) the massif rises up over the town and dominates the skyline. Torroella sits on quaternary conglomerate deposits. These are easily eroded, hence the valley between Pals (10Km to the south) and Torroella is extremely flat. The valley is bisected by the river El Ter, which flows at a leisurely pace from the foothills of the Pyrenees. The river flows to the south of Torroella and winds its way to its conclusion in the Playa de Pals (6Km east of Torroella). El Montgris has been known to humans since prehistoric times. It has some large caves on its slopes that served as a shelter to prehistoric man. The area was very popular with the Romans who cultivated the local area, built roads and towns (many of which still stand to this day) such as Peretelada to the south adjacent to Pals. Since the time of the Romans Torroella has grown into a thriving market town. It has always had close links with the Montgris which until recently still served a purpose as a shelter, not , however, against the elements but against Pirates and marauders from the sea. In fact, on top of the Muntanya Santa Catherina stands the remains of a thirteenth century castle (the last castle ever built in Spain). El Montgris has provided for the local commerce since it was first settled. The local people value the Mountains greatly and still use them today. The rock from which our dwelling was made was quarried from the mountain, the castle rock was quarried on the mountain. 2.0.2 Aims of Study. When I first considered the Montgris as a project area I realised that information would be sparse and that the project would be more complicated than a similar project in the U.K because the environment is so very different and resources would be a great deal more difficult to access (due to the language barrier). I also realised the project would probably be very different to the proposal. Before Glen and I left England we attempted to research the Massif Montgris through the usual channels in order to get an idea of what we would be facing. The research lead to a few vague leads, we new the rock was sedimentary and most likely limestone. Having visited the area previously I could recall a little about the rocks but was certain of their sedimentary nature. .u343ce4ea66568b22f6964b04e1a8d78a , .u343ce4ea66568b22f6964b04e1a8d78a .postImageUrl , .u343ce4ea66568b22f6964b04e1a8d78a .centered-text-area { min-height: 80px; position: relative; } .u343ce4ea66568b22f6964b04e1a8d78a , .u343ce4ea66568b22f6964b04e1a8d78a:hover , .u343ce4ea66568b22f6964b04e1a8d78a:visited , .u343ce4ea66568b22f6964b04e1a8d78a:active { border:0!important; } .u343ce4ea66568b22f6964b04e1a8d78a .clearfix:after { content: ""; display: table; clear: both; } .u343ce4ea66568b22f6964b04e1a8d78a { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .u343ce4ea66568b22f6964b04e1a8d78a:active , .u343ce4ea66568b22f6964b04e1a8d78a:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .u343ce4ea66568b22f6964b04e1a8d78a .centered-text-area { width: 100%; position: relative ; } .u343ce4ea66568b22f6964b04e1a8d78a .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .u343ce4ea66568b22f6964b04e1a8d78a .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .u343ce4ea66568b22f6964b04e1a8d78a .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .u343ce4ea66568b22f6964b04e1a8d78a:hover .ctaButton { background-color: #34495E!important; } .u343ce4ea66568b22f6964b04e1a8d78a .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .u343ce4ea66568b22f6964b04e1a8d78a .u343ce4ea66568b22f6964b04e1a8d78a-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .u343ce4ea66568b22f6964b04e1a8d78a:after { content: ""; display: block; clear: both; } READ: J.P. Morgan Persuasive EssayOur first lead came from an unexpected source. My parents had vacationed in the area and upon my request had asked locally about any information pertaining to the Geology. The result was that they brought back a research map that dated the Massif as Cretaceous but suggested it was composed of 1 massive bed. We loosely agreed our study areas and arranged our projects accordingly. The local guide books and map had supplied us with information about the palaeontology (macro fossils) which suggested the rock was full of bivalves, brachiopods, corals and belemnites. Before leaving we were unable to unearth much more information BUT seemingly at the last minute we were able to make contact with Dr. David Brusi from the Universidad de Gerona(departament del geophysica) who reassured us that upon our arrival in Spain he would brief us on geology of El Montgris. Therefore, with very . The Geology Of The Massif Montgris Essay Example For Students The Geology Of The Massif Montgris Essay The Geology Of The Massif Montgris Essay Declaration This report entitled The Geology of the Massif Montgris was composed by me and is based in my own work. Where the work of others has been used, it is fully acknowledged in the text and in captions to tables and illustrations. We will write a custom essay on The Geology Of The Massif Montgris specifically for you for only $16.38 $13.9/page Order now Signed . Date .. Chapter 1.0 Abstract This is a study of the Massif Montgris, it is based on evidence gathered in the field over 21 days of field work. To supplement this data I have looked at papers and works by previous visitors to the Montgris. The units within the area are from the Upper Cretaceous the Tertiary and the Quaternary. I aim to give an overall guide to the geology on a smaller scale than has previously been accomplished. This study is mainly aimed at correctly dating the units of limestone using micropalaeontological data. The micropalaeontological data has also given light into the palaeoenvironment/geography during deposition. Chapter 2 Introduction 2.0.1 Introduction Between the 24th of June and the 24th of July 1995 Glen Burnham and I ventured to Catalunya. More precisely to Torroella de Montgris. Torroella is in the North East of Spain, just inland of the Mediterranean sea. This remarkable old town lies at the foot of the rather imposing Massif Montgris. Locally known as El Montgris (literally the grey Mountain) the massif rises up over the town and dominates the skyline. Torroella sits on quaternary conglomerate deposits. These are easily eroded, hence the valley between Pals (10Km to the south) and Torroella is extremely flat. The valley is bisected by the river El Ter, which flows at a leisurely pace from the foothills of the Pyrenees. The river flows to the south of Torroella and winds its way to its conclusion in the Playa de Pals (6Km east of Torroella). El Montgris has been known to humans since prehistoric times. It has some large caves on its slopes that served as a shelter to prehistoric man. The area was very popular with the Romans who cultivated the local area, built roads and towns (many of which still stand to this day) such as Peretelada to the south adjacent to Pals. Since the time of the Romans Torroella has grown into a thriving market town. It has always had close links with the Montgris which until recently still served a purpose as a shelter, not , however, against the elements but against Pirates and marauders from the sea. In fact, on top of the Muntanya Santa Catherina stands the remains of a thirteenth century castle (the last castle ever built in Spain). El Montgris has provided for the local commerce since it was first settled. The local people value the Mountains greatly and still use them today. The rock from which our dwelling was made was quarried from the mountain, the castle rock was quarried on the mountain. 2.0.2 Aims of Study. When I first considered the Montgris as a project area I realised that information would be sparse and that the project would be more complicated than a similar project in the U.K because the environment is so very different and resources would be a great deal more difficult to access (due to the language barrier). I also realised the project would probably be very different to the proposal. Before Glen and I left England we attempted to research the Massif Montgris through the usual channels in order to get an idea of what we would be facing. The research lead to a few vague leads, we new the rock was sedimentary and most likely limestone. Having visited the area previously I could recall a little about the rocks but was certain of their sedimentary nature. .u98b910d9a7b24df09fafea9c4657532e , .u98b910d9a7b24df09fafea9c4657532e .postImageUrl , .u98b910d9a7b24df09fafea9c4657532e .centered-text-area { min-height: 80px; position: relative; } .u98b910d9a7b24df09fafea9c4657532e , .u98b910d9a7b24df09fafea9c4657532e:hover , .u98b910d9a7b24df09fafea9c4657532e:visited , .u98b910d9a7b24df09fafea9c4657532e:active { border:0!important; } .u98b910d9a7b24df09fafea9c4657532e .clearfix:after { content: ""; display: table; clear: both; } .u98b910d9a7b24df09fafea9c4657532e { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .u98b910d9a7b24df09fafea9c4657532e:active , .u98b910d9a7b24df09fafea9c4657532e:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .u98b910d9a7b24df09fafea9c4657532e .centered-text-area { width: 100%; position: relative ; } .u98b910d9a7b24df09fafea9c4657532e .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .u98b910d9a7b24df09fafea9c4657532e .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .u98b910d9a7b24df09fafea9c4657532e .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .u98b910d9a7b24df09fafea9c4657532e:hover .ctaButton { background-color: #34495E!important; } .u98b910d9a7b24df09fafea9c4657532e .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .u98b910d9a7b24df09fafea9c4657532e .u98b910d9a7b24df09fafea9c4657532e-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .u98b910d9a7b24df09fafea9c4657532e:after { content: ""; display: block; clear: both; } READ: My Personality EssayOur first lead came from an unexpected source. My parents had vacationed in the area and upon my request had asked locally about any information pertaining to the Geology. The result was that they brought back a research map that dated the Massif as Cretaceous but suggested it was composed of 1 massive bed. We loosely agreed our study areas and arranged our projects accordingly. The local guide books and map had supplied us with information about the palaeontology (macro fossils) which suggested the rock was full of bivalves, brachiopods, corals and belemnites. Before leaving we were unable to unearth much more information BUT seemingly at the last minute we were able to make contact with Dr. David Brusi from the Universidad de Gerona(departament del geophysica) who reassured us that upon our arrival in Spain he would brief us on geology of El Montgris. Therefore, with very .