Wondrous World (rp)

Nami: "It was voluntary, though some money would be fair for my struggle. I can see why you didn't deal with that mummy before. God, that thing was strong..."

 

"Of course."
I stretch out my hand to shake his.
If he shakes my hand then I will use Disconnection to pull out his soul.

OOC:
I told him the fight was gonna start after we shook hands.

 

Lucien goes to the library to read about rocks.

 

Ramus

Ken: "Sure. Enjoy yourself! I'll just walk around town exploring. Surprisingly I actually haven't seen it all yet."

A. Go into the woods
B. Do something else
C. Free Action

 

A.
"Aah, what a nice day."

 

Milikke

You manage to hit his arm, and after stopping a second to take in the pain, he picked it up with his other hand and is continuing to run at you. You also manage to blind the archers and shoot at 3 of them. As you fire though you relies that they also have armor. You manage to hit 2 in the armor (still hurts a little) and the other by the foot in an open spot in the armor, making him jolt his foot back, loss his balance, and fall over the side of the wall. You don't know if he's hurt enough to not get back up. The orcs below seem to be starting to damage the light shield.

A. Free Action

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ALSO RIP ME the Wi-Fi problems came back ;-; I cri (At another location so I can reply right now)

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(I'v got writers block 2 xD Maybe ask a question of how the church got destroyed or somethen?"

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Elzen

Soldier: "I don't know how it could have actually moved at all. We can try to look for it, but the sleeping orc might wake up.

A. Search for it (orc might wake up)
B. Continue to town
C. Free Action

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(Lol It's non-physical fist fight)

If he didn't get the "joke" then he won't be to thrilled that you started it with clever wording.

A. Do it anyway
B. Let him call in the fight for the people to watch
C. Free Action

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Nami

General: "Sure." He hands you 10 eb. "Thank you again for your service. We might have a need for a mercenary like you in the future if you'd care to join us." He does a little smile. "You may leave now, but tell the guard out front to come in while your leaving. I have a task for him."

~You gained liking in the Almuj military!

A. Free Action

 

Nami: "Thank you. I appreciate it. Now, I must return a couple of sound-proof earmuffs I borrowed."

I'll leave, tell the guard to go it, then head to a hotel to sleep.

Well, now I only have the small towns to wynn over before heading to Gavel after finding a plot convenient item that tells me about it... Do I even need to win the villages over?

 

Lucien

Rocks
They form within the Earth and make up a large part of our planet

View Images
Etna's Fireworks
Italy's Mount Etna provides a vivid image of one of the birthplaces of igneous rock during a night eruption. Igneous rock forms when magma cools and solidifies. (Lava is magma that has reached the Earth's surface.) Etna also shows off the etymology of igneous, from the Latin word for fire.

Photograph by Carsten Peter
Oozing Lava
Oozing lava acts as a seal over fractured ground in Hawaii Volcanoes National Park. Once the lava from Kilauea Crater cools, it becomes known as igneous rock, since it formed from molten material. Geologists would also call it extrusive rock because it solidified on the Earth's surface.

Photograph by Frans Lanting
Giant's Causeway
Stepping stones into the sea, these basaltic columns of the Giant's Causeway in Northern Ireland formed from volcanic activity some 50 million to 60 million years ago. Rock formed from molten matter is known as igneous, and geologists classify igneous rock by its texture. You would need a microscope to see the grains in the 40,000-some basalt columns that form the Giant's Causeway.

Photograph by Jim Richardson
Ripples of Pahoehoe
Cooled lava lies in icing-like ripples in Hawaii Volcanoes National Park. This image shows ropy pahoehoe, a type of basaltic lava that forms when solidifying lava meets an obstruction. Hot lava underneath the hardening crust continues to move it along, forming wrinkles in the process.

Photograph by Jeff Gnass
Devils Tower, Wyoming
Known as an igneous intrusion, the 1,267-foot-tall (386-meter-tall) Devils Tower in Wyoming formed when molten rock intruded into the existing rocks. At first the formation wasn't visible, but as wind and water began to erode the sedimentary rock surrounding the tower faster than the harder igneous rock, Devils Tower was born.

Photograph by John G. Wilbanks
Sedimentary Slope
Erosion's artistic side can be seen in sedimentary rock layers in Zion National Park, Utah. After mud, gravel, and sand sediments were deposited and formed rock layers over time, uplift raised the region. Erosion then began to carve the magnificent cliffs and canyons seen today.

Photograph by Peter Arnold, Inc./Alamy
Sedimentary Honeycomb
This section of eroded sedimentary rock on Elgol Beach on the Island of Skye, Scotland, mimics bone. Erosion shaped its honeycombed appearance.

Photograph by John McKenna/Alamy
Wittenoom Iron Formation
A small section of the Wittenoom Iron Formation in Western Australia highlights how sedimentary rocks are laid down in layers. The sediments in this photo curve near the ends of chert pods. Chert—a silica-based rock—occurs in limestone. Paleontologists know chert as a good place to look for fossils.

Photograph by Society for Sedimentary Geology
Limestone and Icicles
Climbing ice-encrusted limestone is careful work in Box Canyon in Ouray, Colorado. During the summer a 285-foot (87-meter) waterfall awes visitors, but in the winter ice and climbing enthusiasts take over.

Photograph by Bill Hatcher
Checkerboard Mesa
Horizontal furrows and vertical fractures in the bedrock give Checkerboard Mesa in Utah's Zion National Park its name. Erosion shaped the Navajo sandstone of the mesa on the edge of the Colorado Plateau, near the east entrance of the park.

Photograph by Larry Fellows
Chert Granules
A single pore between chert granules in a rock formation in Ontario Province, Canada, shows off its colors in this photomicrograph. This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

Photograph by Society of Economic Paleontologists and Mineralogists
White Rock
A river of white rock snakes within its darker surroundings, providing evidence that it had a greater viscosity than the darker rock. Geologists refer to this kind of formation as ptygmatic folding. A penny shows the scale of the size of this folding, which is highly irregular.

Photograph by Marli Miller, University of Oregon
Gneiss Lines
As if an avant-garde painting, younger white rock intrudes in a tapestry of gneiss. Since the white rock doesn't show the same evidence of folding as the surrounding gneiss, it offers proof that it is a younger intrusion. Gneiss, a metamorphic rock, can be commonly found in Precambrian areas. Note the penny for scale.

Photograph by Marli Miller, University of Oregon
Marble Quarry
Bulldozers work in a marble quarry in Thásos, Greece. The Earth's heat and pressure alter limestone into marble, which can range in color from black to white. The ancient Greeks recognized marble's durability, using it to build the Parthenon in Athens. Marble, a metamorphic rock, forms when limestone re-crystallizes.

Photograph by CuboImages srl/Alamy
Schist Rock Formations
The Colorado River has eroded these schist formations into fudge-like shapes and shades. Schist, a metamorphic rock, contains mineral crystals that can be seen by the naked eye.

Photograph by Peter Essick
Rocks are so common that most of us take them for granted—cursing when we hit them with the garden hoe or taking advantage of them to drive in tent pegs on summer camping trips.

What Is a Rock?
To geologists, a rock is a natural substance composed of solid crystals of different minerals that have been fused together into a solid lump.

The minerals may or may not have been formed at the same time. What matters is that natural processes glued them all together.

Types of Rocks
There are three basic types of rock: igneous, sedimentary, and metamorphic.


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Extremely common in the Earth's crust, igneous rocks are volcanic and form from molten material. They include not only lava spewed from volcanoes, but also rocks like granite, which are formed by magma that solidifies far underground.

Typically, granite makes up large parts of all the continents. The seafloor is formed of a dark lava called basalt, the most common volcanic rock. Basalt is also found in volcanic lava flows, such as those in Hawaii, Iceland, and large parts of the U.S. Northwest.

Granite rocks can be very old. Some granite, in Australia, is believed to be more than four billion years old, although when rocks get that old, they've been altered enough by geological forces that it's hard to classify them.

Sedimentary rocks are formed from eroded fragments of other rocks or even from the remains of plants or animals. The fragments accumulate in low-lying areas—lakes, oceans, and deserts—and then are compressed back into rock by the weight of overlying materials. Sandstone is formed from sand, mudstone from mud, and limestone from seashells, diatoms, or bonelike minerals precipitating out of calcium-rich water.

Fossils are most frequently found in sedimentary rock, which comes in layers, called strata.

Metamorphic rocks are sedimentary or igneous rocks that have been transformed by pressure, heat, or the intrusion of fluids. The heat may come from nearby magma or hot water intruding via hot springs. It can also come from subduction, when tectonic forces draw rocks deep beneath the Earth's surface.

Marble is metamorphosed limestone, quartzite is metamorphosed sandstone, and gneiss, another common metamorphic rock, sometimes begins as granite.





A. Free Action

(totally didn't copy off a random site and will get copywrite stricked)

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Ramus

The woods is beautiful. The leaves are even starting to change to colorful colors!

A. Free Action

(I don't think iv ever actually seen an RP change seasons.)

 

Thank god I'm not Lucien

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I start walking towards the Forest Guardian.

 

Can I just the orc over the head several times with the flat of my knife or a rock so that it stays unconscious? If so I'll do it, if not do the soldiers have rope to tie it up, if not we'll just continue on as the orc will probably die anyway and the other orcs probably won't take offence as they do tend to respect battles(in quest in wynncraft, the one that you need to get the orc mask for).

 

Nami

You go out and tell the guard to go in. He does.

A. Easdrop
B. Go to hotel (Sleep or TV?)

 

Hard choice... But Nami is too tired to make rational decisions, so she goes to the hotel.

 

Ramus

As you walking, you spot 1 orc sleeping sitting and leaning on a rock.

A. Kill it and move on
B. Free Action

 

B.
I just look at it and move on

 

Elzen

You can beat the orc over the head, but that might kill it, which the soldiers would prefer you to not do.

A. Beat it's head (Small chance of waking it up as well)
B. Take the risk of it waking up
C. Continue to camp
D. Free Action

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Nami

You go to the hotel

A. Sleep
B. TV (It's rly late but you still can)
C. Free Action

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Ramus

You look at it and then move on, making it to the guardian. He's asleep, as always.

A. Free Action

 

I flop down on the bed and fall asleep as soon as my head hits the pillow.

 

"Of course he's sleeping."
I walk into the forest a de return with a Volt Goat in my hands. I stab the Guardian with the horns.

 

Do the soldiers have any rope I could tie it up with?

 

Lucien closes the book before going outside to check to see how much time he killed.

 

Nami

You go into a deep sleep right as you hit the pillow. You wake up at about 11 the next morning after a good sleep. You kinda hungry cause you haven't eaten in a while.

A. Eat (where)
B. Wait a while
C. Free Action

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Ramus

He wakes up. Guardian: "Wh-wha, oh, hello Ramus. How have you been?"

A. Free Action