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Pawtuckaway State Park

Pawtuckaway State Park is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Pawtuckaway State Park rather than just read about it. In short: Pawtuckaway State Park is a 5,000-acre (20 km2) preserve in New Hampshire, United States. It is one of the largest state parks in southeastern New Hampshire and is named for Pawtuckaway Lake and the Pawtuckaway Mountains.

Pawtuckaway State Park — main illustration
Pawtuckaway State Park — illustration

Key takeaways

  • Pawtuckaway State Park belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Pawtuckaway State Park to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Pawtuckaway State Park from memory before moving on to harder problems.

Reference excerpt

Pawtuckaway State Park is a 5,000-acre (20 km2) preserve in New Hampshire, United States. It is one of the largest state parks in southeastern New Hampshire and is named for Pawtuckaway Lake and the Pawtuckaway Mountains. The park extends from the west shore of the lake to the west side of the mountains.

Geology

The Pawtuckaway Mountains are a small, rocky, circular range that form the outline of an ancient volcanic ring dike dating from 130 to 110 million years ago (Cretaceous). The ring dike, first completely mapped in 1944, is a smaller and more accessible example of the same kind of geological process that formed the Ossipee Mountains to the north. The inner ring is roughly one mile in diameter, while the outer is measured at almost two miles. Earthquakes occurred in the vicinity of the ring dike in the summer and fall of 1845. Known as the Deerfield explosions, they were described as subterranean noises "often as loud as the report of a 12 pounder cannon when heard at a distance of half a mile" but without echoes. They were the subject of much speculation at the time.

Environment The park lies within the Northeastern coastal forests ecoregion.

Recreation

The park has 32 miles (51 km) of hiking trails. Trails lead to the approximately 900-foot (270 m) summits of North and South Pawtuckaway mountains and connect the ring dike area to the lake. Other hiking trails lead to ponds, boulder fields, and views of the lake. Some of the hiking trails are used in the winter as snowmobile routes. The Pawtuckaway ring dike includes a boulder field of interest to boulderers, along with roped climbing, and the park is a popular destination for geocaching. The lake is a 783-acre (317 ha) water body with numerous islands and coves and is a popular boating, fishing, and swimming destination. Since orienteering enthusiasts made an orienteering map of the park in 1992, the park has become a venue for major orienteering meets, including foot orienteering and canoe orienteering. The venue is shared by several orienteering clubs in New England, including Cambridge Sports Union, New England Orienteering Club, and Up North Orienteers. Park amenities include 5 cabins, 195 campsites, a boat launch, a swimming beach, camp store, ball field, playground, bathhouse, shelters, picnic tables, and canoe, paddleboard, and kayak rentals.

History The area was originally composed of many brooks which collected in low spots and formed small ponds, such as what was then known as Pawtuckaway Pond. Some of the brooks that ran through the area eventually ran into the Pawtuckaway River. Both the North River and the Pawtuckaway River then ran into the Lamprey River. The construction of two colonial sawmills marked the beginning of enlarging the small ponds. On the north end, in 1729 a sawmill enlarged Pawtuckaway Pond. On the south end, in 1732 another sawmill enlarged Dolloff Pond. Beginning in 1825 the Newmarket Manufacturing Company began to acquire land in the area for the construction of a reservoir to supply a consistent source of water power to its textile mill in nearby Newmarket, downstream from the lake. In 1836 two dams and several dikes were constructed that changed the features and character of the two ponds, causing their waters to merge except when the water levels were drawn down. Eventually, steam power replaced water power, and gradually less water was drained from the lake to generate power. As water levels rose over time, Dolloff Pond and Pawtuckaway Pond merged into a single body of water. When the Newmarket Manufacturing Company fell on hard times in the early 1920s, it closed its mill in Newmarket. Its interests in the lake eventually passed into the hands of the New Hampshire Electric Company, which outfitted the dams with generators for hydroelectric power. Ultimately, the production of electricity became unprofitable and in December 1955 NH Electric deeded the lake, its islands, its adjacent land, two dams, the dikes, and the water rights to the State of New Hampshire. In 1958 Dolloff Pond was officially considered merged into Pawtuckaway Pond, and the level of the pond is now managed for recreational and environmental uses.

References

External links Pawtuckaway State Park New Hampshire Division of Parks and Recreation Visiting New Hampshire's Biodiversity: Pawtuckaway State Park New Hampshire Division of Forests and Lands

Illustrations

Pawtuckaway State Park illustration
Pawtuckaway State Park: 1957 topographic map, showing lake and ring dike
1957 topographic map, showing lake and ring dike
Pawtuckaway State Park: Aerial map of Pawtuckaway Lake and part of Pawtuckaway State Park (green overlay); the southeast quarter of the ring dike is visible in the upper left corner
Aerial map of Pawtuckaway Lake and part of Pawtuckaway State Park (green overlay); the southeast quarter of the ring dike is visible in the upper left corner

Worked examples

Example 1 — a first encounter with Pawtuckaway State Park

Start with the simplest possible case. Write down what Pawtuckaway State Park claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Pawtuckaway State Park before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Pawtuckaway State Park ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Pawtuckaway State Park

In research
Pawtuckaway State Park appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Pawtuckaway State Park in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Pawtuckaway State Park is common in secondary-school and first-year university syllabi. It links to neighbouring topics Deerfield, New Hampshire, IUCN Category V, Landforms of Rockingham County, New Hampshire, so understanding it makes those chapters shorter.
In everyday life
Look for Pawtuckaway State Park outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Pawtuckaway State Park in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Pawtuckaway State Park means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Pawtuckaway State Park out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Pawtuckaway State Park in simple terms?

Pawtuckaway State Park is a 5,000-acre (20 km2) preserve in New Hampshire, United States. It is one of the largest state parks in southeastern New Hampshire and is named for Pawtuckaway Lake and the Pawtuckaway Mountains.

Why does Pawtuckaway State Park matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Pawtuckaway State Park?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Pawtuckaway State Park.

Tags

  • Deerfield, New Hampshire
  • IUCN Category V
  • Landforms of Rockingham County, New Hampshire
  • Nottingham, New Hampshire
  • Parks in Rockingham County, New Hampshire
  • Ring dikes
  • Rock formations of New Hampshire
  • State parks of New Hampshire
  • Volcanism of New Hampshire

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