The Crystal Caves of Bermuda Alexa Lafferty. I visited The Crystal Caves of Bermuda last summer. These amazing underground caves were very beautiful and.

Slides:



Advertisements
Similar presentations
Groundwater Chapter 9, Section 2.
Advertisements

Earth Processes: Part 2: Hydrosphere (water)
Caves By Akhil Chivukula.
Erosion - The process of moving sediment from one place to another Caused by wind, water, or ice (sediment moves away)
By: Katie Hudson. Mammoth Cave was established July 1941 to keep the cave system preserved and to protect natural areas. The Green and Nolin River is.
Presented by: Kristin McKeown Project 6 May 4, 2011 Click here to find out more about Bermuda!
A presentation. Key Question: How do rocks and landforms affect what we do? Rocks and landforms affect people Rocks and Landforms affect the shape of.
Left: Judy pauses before going into the second cave on our trip; this cave did not require helmet lighting. Below: our guide offered coffee, tea and cookies.
Caves and Cave Formation. Caves are created by Ground Water Water, when mixed with Carbon containing material, makes Carbonic Acid. Acids dissolve limestone.
Limestone Scenery Limestone scenery is mainly found in England, in areas such as the Yorkshire Dales and the Peak District. Limestone is a sedimentary.
Limestone Features Miss James Higher. Limestone scenery exposure of very extensive limestone pavements may be partly an example of the stripping of soil.
Carbonic Acid Most groundwater is slightly acidic due to carbonic acid. Carbonic acid forms when carbon dioxide gas dissolves in water and combines with.
Any comments????. Now how about this image??? CHAPTER 3 Weathering and Erosion FIRST YEAR GEOG MS CLIFFORD St Tiernans CS.
Groundwater Chapter 6.3.
Erosion and Deposition Changing Earth’s Surface
Water Erosion.
Chapter 3 Section 2 Pages 72-81
Erosion and Soil Depostion
Erosion and Deposition
HIGHER GEOGRAPHY LITHOSPHERE LIMESTONE SCENERY. LIMESTONE -UNDERGROUND FEATURES Caves and Caverns Tunnels, passages and sumps Potholes, sinkholes, swallow.
Do you know what’s going on in Timpanogos Caves? By: Diantha Smith, 2009 Cave Basics.
TEXT NO 1 Questions I to 10 refer to the following passage:
WEATHERING AND EROSION.  Groundwater dissolves rock  Groundwater is often mildly acidic  Contains weak carbonic acid  Forms when rainwater dissolves.
Erosion and Deposition
Stalactites Presented by Joseph, Kaden and Andre.
January 13, 2014 Agenda 1.Roll 2.Student Survey 3.PowerPoint titled: Water Underground 4.Possible Video “Wonder Beneath”
Ground water.
Groundwater What is Groundwater???? The water that has seeped into the soil and rock. The underground area is broken down into 4 areas… 1) Zone of Aeration.
Compiled by N. Boucher 10/09. What is a cave? A cave is: A hole or tunnel into the earth with an opening to the surface Caves are located underground.
Erosion Rapid Fire Picture Review. What is the geologic structure?
Water Erosion: How do processes involving water change Earth’s surface? Part 3 1.
MAIN IDEA: LANDFORMS CAUSED BY THE CHEMICAL WEATHERING OF LIMESTONE ARE CALLED KARST TOPOGRAPHY. Chp 10.2 Notes Groundwater Erosion & Deposition.
1 Environmental Science Unit 1: Geology Basics Earth’s Layers & Plate Tectonics.
The most beautiful places on Earth TOP 10 rating.
The Effects of Weathering by Water By Richard Horn.
Michal Čirip. Belianska cave  only one accessible to public in the Tatras  the cave entrance is at an altitude of 890 metres above sea level  cave.
Northern Karst. Northern Karts Rocky Region located between the interior mountain ranges and the northern coastal plain. Its is made up of limestone
Veronica McCauley, Alex Jensen, Nick Gibas, Tessa Buehner
Sedimentary Rocks are formed at or near the Earth’s surface No heat and pressure involved Strata – layers of rock Stratification – the process in which.
The Action of Groundwater Earth Science Grade 8. Groundwater The water that soaks into the ground and collects in pores is called groundwater. The water.
Famous caves of Ukraine. Caves of Ukraine ► “Optimistichna” ► “Atlantida” ► “Krishtaleva” ► “Ozerna” ► There are many caves in Ukraine. There are 3 main.
SEDIMENTARY ROCKS There are 2 ways sedimentary rocks are formed 1. Clastic are made from sediments glued together 2. Non-clastic : not glued together---include.
The Science of Caves.
LIMESTONE SCENERY.
SEDIMENTARY ROCKS SEDIMENTARY ROCKS WILL CONTAIN FOSSILS.
Assignment# 10 Sedimentary Rocks
6th grade Science Starter October 8th Changing Earth’s Surface:
Accounting Become Beautiful with QuickBooks24x
Caves.
Karst Topography Dissolved Carbonate Rock 80+ either:
Section 2: Groundwater and Chemical Weathering
What Shapes Can You See in this Picture?
Earth’s Changing Surface
Ground Water Chemical Weathering
Water Erosion Chapter 4.1 Pages
Take a minute to make an educated guess!
Groundwater Erosion & Deposition
10.2 Caves Chemical weathering of limestone by water causes characteristic topography of karst areas. AKA Water dissolves limestone leaving oddly shaped.
Ground water.
Stalagmites and Stalactites
(Discussion and Worksheet – Groundwater Part 3)
Continental Slope The descending slope which connects the sea floor to the continental shelf.
Take a minute to make an educated guess!
Week 13 - Mod 6 Foundations of Geology
Caves.
What is a Cave? Remember those aquifers? Well limestone erosion occurs in the aquifers that creates large empty pockets. These pockets are filled with.
BY: JOSEPHINE MANU & COLETTE ICKES
Pre-Historic Habitats in Malta (Ghar Dalam)
Chapter 3 Section 5 How are sedimentary rocks classified?
Groundwater Chapter 6.3.
Presentation transcript:

The Crystal Caves of Bermuda Alexa Lafferty

I visited The Crystal Caves of Bermuda last summer. These amazing underground caves were very beautiful and very interesting to see. The caves are made up of stalactites and stalagmites, and on the bottom lies a deep, clear, blue lake.

As you descend into the cave the first thing you notice is all the the crystals hanging from the ceiling. These are called stalactites and most commonly occur in limestone caves such as these.

These stalactites vary in size and shape depending on their age. These stalactites grow extremely slow(not even a quarter of an inch a year). You can also see the blue lake in this picture.

In this picture you can see just how clear the water on the bottom of the cave is. You can see straight through to the stalagmites growing up from the floor of the cave. Keep in mind the water is about 55 feet deep.

These stalagmites can even grow underwater and sometimes can rise up out of the water to meet a stalactite. Although, this takes many many years.

Photographed here are stalactites meeting stalagmites.

Overall, this was a very interesting trip and I would recommend visiting The Crystal Caves of Bermuda to anyone.