Stalactite Formation Simulation

Slides:



Advertisements
Similar presentations
Groundwater Chapter 9, Section 2.
Advertisements


Erosion - The process of moving sediment from one place to another Caused by wind, water, or ice (sediment moves away)
Slow Changes to Earth’s Surface
Click here for an animation
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.
5th year Geography Ms Carr
Carbonic Acid Most groundwater is slightly acidic due to carbonic acid. Carbonic acid forms when carbon dioxide gas dissolves in water and combines with.
 Draw a meander and label these locations: erosion, deposition, faster water, and slower water. Warm – Up 2/6.
Chapter 15 & 16 Review. Question # 1 The rock and other material that a stream carries is known as its ….. Stream load.
Changing Earth’s Surface
Prentice Hall EARTH SCIENCE
Running Water and Groundwater
Objectives: 1. To review the terms ‘denudation,’ ‘erosion,’ and ‘weathering’ (freeze-thaw action & carbonation), along with surface landforms found in.
Water Erosion Chapter 9 Section 2.
Water Erosion Meander-bend in a river.
HIGHER GEOGRAPHY LITHOSPHERE LIMESTONE SCENERY. LIMESTONE -UNDERGROUND FEATURES Caves and Caverns Tunnels, passages and sumps Potholes, sinkholes, swallow.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 3 Earth’s Materials Reference: Chapters 2, 3, 6,
9 Karst Landscape The formation of karst landscapes
Fresh Water. Rivers What Is Erosion? Erosion is the process by which soil and sediment are transported from one location to another. Water and Erosion.
U Chemical sedimentary rocks v derived from material carried in solution to lakes/seas v evaporation and precipitation from solution to form “chemical.
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.
Chapter 16 section 2 Groundwater & Chemical Weathering The warmer the rock + long periods of contact with water will cause greater amounts of dissolved.
Fresh Water and Karst Topography. Hydrologic cycle On a global basis: Water from atmosphere to earth (Precipitation) Water from earth to atmosphere (Evaporation.
Stalactites Presented by Joseph, Kaden and Andre.
Unit 1 Lesson 3 Erosion and Deposition by Water
Ch Water Shapes the Land
January 13, 2014 Agenda 1.Roll 2.Student Survey 3.PowerPoint titled: Water Underground 4.Possible Video “Wonder Beneath”
Ground water.
Chapter 11 The Flow of Fresh Water.
Water Beneath the Surface
Cave Formations Be prepared to identify all these cave formations When we visit:
 Draw a meander and label these locations: erosion, deposition, faster water, and slower water. Warm – Up 2/6.
Water Erosion: How do processes involving water change Earth’s surface? Part 3 1.
Effects of Groundwater on Topography By Diana L. Duckworth Rustburg High School Campbell County, VA.
Unit 1 Lesson 3 Erosion and Deposition by Water
A COMMON TOPOGRAPHIC FEATURE EFFECT BY POROSITY AND PERMEABILITY IS…… Karst Topography  What is Karst topography?  topography developed in areas underlain.
Bats Cave Formation Cave Sections Types of Caves.
Carboniferous Limestone
Chapter 10 Groundwater!.
Erosion by Runoff Moving water is the major agent of erosion that has shaped Earth’s land surface. Runoff- water that moves over land that can carry soil.
Unit 1 Lesson 3 Erosion and Deposition by Water
T/F Wind, water, ice, and gravity continually shape Earth’s surface.
Section 2: Groundwater and Chemical Weathering
Water Beneath the Surface
Stream/River Erosion & Deposition
Chapter 6.1 Running Water.
Caverns, Sinkholes and Karst
8th Grade The Dynamic Earth (Module E)
Ground Water Chemical Weathering
10.2 Caves Chemical weathering of limestone by water causes characteristic topography of karst areas. AKA Water dissolves limestone leaving oddly shaped.
Water Erosion Chapter 9 Section 2.
Stream/River Erosion & Deposition
Ground water.
Stalagmites and Stalactites
Stream/River Erosion & Deposition
(Discussion and Worksheet – Groundwater Part 3)
Stream/River Erosion & Deposition
Cavern and Mineral Deposits: How Caverns Form
Unit 1 Lesson 3 Erosion and Deposition by Water
Groundwater Erosion and Deposition Nayiri, Eileen, Liz, Talin
Stream/River Erosion & Deposition
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
PROF. ROBINA KOUSER ASSISTANT PROFESSOR IN GEOGRAPHY
Chapter 9: Karst Landscape
Presentation transcript:

Stalactite Formation Simulation By Ruben Escolero

Formation of Stalactites Water carries calcium bicarbonate through the cracks of the roof of the cave As these drops come out the cracks travel along the roof of the cave, they will at some point evaporate and deposit calcite on the roof This eventually forms a stalactite on the ceiling Simulated these droplets using DLA by having one source of water from the center and water drops also coming from all sides Each drop would evaporate with a certain probability Also, the steeper the gradient of the surface, the higher the probability is that the drops would travel downward Probability = -10^-(g/10) + 1 where ‘g’ is the gradient

Stalactite Formation Simulation