Earth Science | NYS Regents Aligned
Click a card to reveal its definition. Cards close automatically after 8 seconds.
Click a term on the left, then click the matching definition on the right.
Read the passage, complete the activities, and analyze the data.
Rivers are among Earth's most powerful forces of change. They begin high in mountains as small streams called tributaries, collecting water and growing larger as they flow downhill toward the sea. Along the way, rivers erode rock, transport sediment, and build new landforms like deltas and floodplains. The entire land area that drains water into a single river system is called a watershed or drainage basin.
In New York State, major watersheds include the Hudson River basin, the Delaware River basin, and the St. Lawrence–Great Lakes drainage system. Rainwater and snowmelt that falls within a watershed eventually finds its way to streams and rivers. In spring, melting snow causes discharge — the volume of water flowing past a point per unit of time — to peak dramatically, sometimes causing rivers to overflow onto their floodplains.
Dams are built to control flooding, generate hydroelectric power, and store water for drinking and irrigation. However, dams significantly change river ecosystems. Behind a dam, water slows in a reservoir. Below the dam, flows are reduced and controlled. Sediment that would normally travel downstream is trapped behind the dam, reducing the natural delivery of nutrients to coastal areas. In New York State, the Ashokan and Schoharie reservoirs in the Catskill Mountains are critical to New York City's water supply, yet their dams have permanently altered the ecology of Esopus Creek and Schoharie Creek.
Dams also affect aquifers — underground rock layers that store groundwater. When river discharge drops, less water percolates into the ground to recharge aquifers. In coastal areas like Long Island, reduced groundwater recharge combined with over-pumping can allow saltwater to intrude into the freshwater aquifer, making the water unfit for drinking or irrigation.
Click a word from the bank below, then click the blank to fill it in. (4 pts)
Click the words in the correct order to rebuild the sentence.
Click the words in the correct order to rebuild the sentence.
Add details to each bare sentence using the prompts provided.
The graph above compares sediment load (mg/L) measured at different distances downstream from a dam, both before and after dam construction.
Explore erosion and deposition on inside vs. outside river banks.
When water flows around a bend in a river, it does not move equally on both sides. Water on the outside of the curve moves faster because it travels a longer distance. This faster-moving water has more energy and carves into the bank, creating a steep, undercut cliff called a cut bank. The outside bank loses material through erosion.
On the inside of the curve, water moves more slowly. Slow water loses energy and drops its sediment load, building up a shallow, gently sloping deposit called a point bar. This is the process of deposition. Together, erosion on the outside and deposition on the inside cause the bend — called a meander — to grow wider and more exaggerated over time.
Eventually, a meander may loop so tightly that the river cuts through the narrow neck of land, abandoning the old curve entirely. This creates a crescent-shaped, isolated body of water called an oxbow lake.
Rivers in New York State provide dramatic examples of this process. The Genesee River at Letchworth State Park in western New York has carved through hundreds of feet of sedimentary rock, creating a spectacular gorge with walls of layered limestone and shale. These rock layers were deposited in warm, shallow Devonian seas some 350–400 million years ago. The rate of erosion depends on water speed, rock hardness, sediment load, and the presence of vegetation along the banks.
Click a word, then click the blank to place it.
Click the buttons to highlight erosion and deposition zones on a river meander.
Use what you have learned to complete the table below.
| Feature | Inner Bank | Outer Bank |
|---|---|---|
| Water Velocity | ||
| Primary Process | ||
| Landform Created | ||
| Bank Shape |
Study the photograph of Letchworth Gorge on the Genesee River. Two locations are labeled X and Y.
Students in a class are identifying a safe hiking route along the edge of the Genesee River gorge shown in the photo. A student makes the claim below:
"The safest route of the hiking trail should be near location ___ because at ___ there is a greater chance of weathering and erosion due to ___, which increases the risk of ___ along the trail."
Study the diagram and record your observations about ecological impacts.
Study every detail of the diagram above. You will use it to complete the data table and answer analysis questions below.
For each ecological effect shown in the diagram, write a description and classify the impact as Positive (P) or Negative (N).
| Ecological Effect | Description (what happens) | Impact: P or N? |
|---|---|---|
| River Flow | ||
| Fish Migration | ||
| Sediment Transport | ||
| Wetland Area | ||
| Water Table | ||
| Algal Blooms |
Investigate plastic pollution in rivers and innovative cleanup methods.
Plastic pollution is one of the most serious environmental threats facing Earth's waterways. Each year, millions of metric tons of plastic waste enter rivers and eventually reach the ocean. The Great Pacific Garbage Patch — a massive accumulation of floating plastic debris in the North Pacific Ocean — covers an area estimated to be twice the size of Texas.
The Ocean Cleanup Project has developed innovative methods to target plastic at its source — rivers — and to remove it from open ocean gyres. In rivers, V-shaped barriers funnel floating plastic into collection systems onshore. This strategy is effective because approximately 1,000 rivers worldwide contribute about 80% of all plastic that reaches the ocean.
In the open ocean, a giant C-shaped floating barrier moves with the plastic, driven by wind and waves. A sea anchor slows the barrier so that plastic accumulates in the retention zone while marine animals can escape beneath a 3-meter-deep skirt. Support vessels arrive every few weeks to collect the debris for recycling.
On Long Island, storm drains that empty into Great South Bay, Jamaica Bay, and the Atlantic Ocean carry plastic, motor oil, and fertilizer from streets, lawns, and parking lots. Students and local organizations monitor stream quality and organize beach cleanups to reduce the flow of pollutants into Long Island's estuaries and coastal waters.
Classify each pollution source as Point Source (identifiable pipe/location) or Nonpoint Source (scattered/diffuse origin). (1 pt each row)
| Pollution Source | Classification (Point or Nonpoint) | Brief Explanation |
|---|---|---|
| A factory draining wastewater through a pipe into a river | ||
| Fertilizer runoff from lawns after heavy rain | ||
| A sewage treatment plant releasing treated water |
Explore the rivers, watersheds, and bedrock geology of New York State.
New York State has three major drainage basins. The Hudson–Mohawk watershed drains much of central and eastern New York, with the Hudson River flowing south to New York Harbor. The Delaware River watershed covers the Catskill Mountains and drains southwest to the Atlantic Ocean. The St. Lawrence–Great Lakes watershed covers western New York, draining north toward Canada.
An estuary is a partially enclosed coastal body of water where fresh river water mixes with salt water from the ocean. Estuaries are among the most productive ecosystems on Earth, providing nursery habitat for fish, feeding grounds for shorebirds, and natural flood protection. The Hudson River Estuary extends approximately 150 miles from New York Harbor north to the Federal Dam at Troy. During high tides, salt water can push more than 60 miles upriver from the ocean.
Long Island is surrounded by important estuaries and bays including Jamaica Bay, Great South Bay, and Peconic Bay. The geology of Long Island — primarily glacial outwash sands and gravels deposited during the last ice age — means freshwater moves quickly underground through a series of aquifers rather than forming large surface rivers. The Upper Glacial Aquifer, Magothy Aquifer, and Lloyd Aquifer supply drinking water to millions of Long Islanders.
The bedrock geology of New York State reflects billions of years of Earth history. The Adirondack Mountains expose ancient metamorphic and igneous rocks over one billion years old. Central and western New York is underlain by Devonian-age limestones, shales, and sandstones deposited in warm shallow seas. Moving east toward the Hudson River, rock ages generally increase, and complex metamorphic terranes dominate. Long Island's surface is entirely covered by the youngest deposits in the state — Pleistocene glacial sediments.
Use the bedrock geology map and your knowledge to complete the following table.
| NYS Region | Major Watershed / Drainage Basin | Dominant Rock Type at Surface | Age of Rock |
|---|---|---|---|
| Long Island | |||
| Adirondacks | |||
| Central NY (Syracuse area) | |||
| Hudson Valley |
Click each river button to explore data and key facts. Use the information to answer the evidence and claim questions below.
Use the river data panels above to find EVIDENCE (specific data or facts) to support each CLAIM. Always cite the data (numbers, measurements, or named facts) in your answer.
5 questions selected from a bank of 20. You need 60% (3/5) to continue. Multiple attempts allowed.
Your complete score for Mr. Brown's Rivers & Watersheds Lab.
Tip: In the print dialog, choose "Save as PDF" to download your report.